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  • 1
    Publication Date: 2022-07-15
    Description: In Niedermendig / Osteifel (Rheinland-Pfalz/Bundesrepublik Deutschland) ist vor etwa 200000 Jahren ein basaltischer Lavastrom ausgeflossen. Nach den chemisch-petrographischen Analysen handelt es sich um einen Tephrit. Der meist 15 m bis 25 m mächtige Lavastrom wird zumindest seit dem Mittelalter als mineralischer Rohstoff genutzt. Wesentliche Merkmale des Basaltes von Niedermendig sind die Porosität von ca. 15 bis 29 Vol.-Prozent und die zum Teil sehr großen Trennflächenabstände (Säulendicke). Diese und weitere geotechnische Eigenschaften der Basaltlava sind für die Nutzung als Mühlstein ideal. Mühlsteine aus Niedermendig und Mayen wurden bis in das 20. Jahrhundert hinein weltweit vertrieben. Aufgrund des meist 10m bis 20m mächtigen Deckgebirges wurde der Abbau bis vor wenigen Jahrzehnten unter tägig vorgenommen. Ein amtliches Grubenbild aus dem 19. Jahrhundert wurde mit einem Geoinformationssystem ausgewertet, so dass einerseits die zeitliche Entwicklung des damaligen Bergbaues nachvollzogen werden kann und andererseits die Lage der untertägigen Hohlräume in Bezug zur heutigen Topographie gezeigt wird. Zusammen mit den Ergebnissen der ingenieurgeologischen Kartierung nach 1988 wird die Lage von 240 verschiedenen Schächten nachgewiesen. Berichte von Zeitzeugen dokumentieren dieUmstände des Bergbaues im 19. Jahrhundert. Aktuell existieren noch 17 Basaltlava-Tagebaue unter der Aufsicht der Bergbehörde, wobei im Jahr 2002 nur in sechs Betrieben tatsächlich abgebaut wurde. Gegenwärtig werden aus der Basaltlava von Niedermendig sowohl Werksteine als auch Korngemische/Schüttgüter hergestellt.
    Description: About 200 000 years b.p. a basaltic lava flow formed near Niedermendig in the Eifel Mountains (Rhineland-Palatinate/Germany). According to the Chemical and petrographical data the basalt is classified as tephrite. The mining of the mostly 15m to 25m thick basaltic lava flow started at least in the Middle Ages. Essential features of the Niedermendig basalt are a porosity of about 15-29 Vol.-% and the widely spaced columnar jointing. These features and additional geotechnical properties are responsible for the ideal qualification of the basalt to grind grain and other materials. Mill stones from Niedermendig and Mayen have been distributed world-wide until the beginning of the 20th Century. Due to the 10 m to 20 m thick overburden the basalt has been exploitcd by Underground mining for centuries. Surface-mining just started several decades ago. A 19th Century mine map was anaiysed using GIS Software. The results reveal the rate of advance of the former Underground mining and the spatial distribution of the cavities referring to the current Settlement. In addition to the data of the engineering geology mapping which was started in 1988, this article presents the location of 240 different mining shafts. Historie reports from the 19th Century provide Information about the details of the former Underground mining. At present, 17 open-pit mines in Niedermendig are under supervision of the Department of Mines. Only 6 mines were in production in 2002. Currently the basaltic lava is mined for products like building stones and solid bulk materials
    Description: research
    Keywords: ddc:622.35 ; ddc:553.5
    Language: German
    Type: doc-type:article , publishedVersion
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  • 2
    Publication Date: 2022-07-15
    Description: Investigations on the systematic position of the foraminifer generally refered to as Hastigerina demens known from the Aquitanian of the Mayence basin have shown, that a new classification has to be made. Based on the shown protoforamina the species has to be considered as belonging to the family Polystomellidae EIMER & FICKERT, 1899. The aberrant test of the species which above all appears in the evolute arrangement of the chambers, has induced the author to place the species in a new genus Nonionoides n. gen. For N. demens a benthonic way of life has to be assumed. Therefore no autochthon planctonic living foraminifers are known from the Hydrobia beds and Corbicula beds of the Mainz basin.
    Description: research
    Keywords: ddc:562
    Language: German
    Type: doc-type:article , publishedVersion
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  • 3
    Publication Date: 2022-07-15
    Description: Auf der Basis von Mikrofaunen-Untersuchungen wurden die Corbicula- Schichten des Mainzer Beckens s. str. feinstratigraphisch-paläoökologisch bearbeitet. Die Untersuchungen stützten sich auf detaillierte Geländeprofile vom Sommerberg, südwestlich Alzey und aus den Steinbrüchen bei Göllheim, Oppenheim/Nierstein und Rüssingen. Für den stratigraphischen Bereich vom höchsten Teil der Oberen Cerithien-Schichten bis in basale Lagen der Hydrobien-Schichten werden 4 Profilabschnitte nachgewiesen, in denen ein verstärktes Auftreten von Foraminiferen und brackischen Ostrakoden auf eine Erhöhung der Salinität im ehemaligen Ablagerungs- und Lebensraum schließen läßt. Ökologische Faktoren können jedoch unterschiedliche Mikrofaunen- Assoziationen an den verschiedenen Untersuchungspunkten eines gleichen stratigraphischen Niveaus bedingen. Das Einsetzen des Ostrakoden Hemicyprideis lienenklausi Marz in mittleren Lagen der Corbicula-Schichten ermöglicht eine Zweiteilung in Untere und Obere Corbicula-Schichten. Als mikrofaunistisches Abgrenzungskriterium Obere Cerithien-Schichten/Corbicula- Schichten wird das Erlöschen von Hemicyprideis rhenana (LienenkLaus) herangezogen. Gleichzeitig ist an der Wende Obere Cerithien-Schichten/Corbicula-Schichten ein scharfer ökologischer Wechsel von brackischen zu limnischen Verhältnissen zu beobachten. Die Grenze Corbicula-Schichten/Hydrobien-Schichten ist mikropaläontologisch nicht exakt faßbar. Sicherstes Abgrenzungskriterium bleibt daher das Erlöschen von Hydrobia inflata (Liu). Die Foraminifere Nonionoides demens (BıXx) und der Ostrakode Cypridopsis (Obliquopsis) obliqua Maız setzen in höheren Lagen der Corbicula-Schichten sehr vereinzelt ein. Individuenreiche Populationen dieser Arten können als sicherer Hinweis auf Hydrobien- Schichten angesehen werden. Im Kapitel Mikropaläontologie werden die stratigraphisch wichtigen Hemicyprideis- Arten (Östracoda) beschrieben und abgebildet. Die Foraminiferen-Gattungen Neobulimina CusHMANn & Wickenpen und Glabratella Dorreen werden erstmalig für das Mainzer Becken nachgewiesen.
    Description: Abstract: Based on investigations of microfaunas the Corbicula beds of the Mainz basin s. str. are researched biostratigraphically and paleoecologically. The investigations rely on sections from a road cut near Alzey and at the quarries of Göllheim, Oppenheim/ Nierstein and Rüssingen. Four stratigraphical sections can be proved which are characterized by increased appearance of foraminifers and brackish ostracods from the uppermost part of the Upper Cerithium beds up to the basal layers of the Hydrobia beds. These sections indicate increases of salinity in the paleoenvironment. Other ecological factors can imply different microfauna associations at several points of investigation within the same stratigraphical horizon. A subdivision into Lower Corbicula beds and Upper Corbicula beds is possible by the first appearance of the ostracod Hemicyprideis lienenklausi Maız in the middle layers of the Corbicula beds. The micropaleontological delimitation Upper Cerithium beds/Corbicula beds is defined by the extinction of Hemicyprideis rhenana (Lienenktaus). The boundary Upper Cerithium beds/Corbicula beds is also characterized by a sharp ecological change from brackish to fresh-water conditions in the paleoenvironment. An exact micropaleontological criterion to define the boundary Corbicula beds/Hydrobia beds was not found. The extinction of Hydrobia inflata (Lıuı) is considered as the best biostratigraphical datum to limit the Corbicula beds from the Hydrobia beds. The ostracod Cypridopsis (Obliquopsis) obligqua Maız and the foraminifer Nonionoides demens (Bıx) appear at the first time in the upper parts of the Corbicula beds and populations rich in these species can be taken as a sure hint to Hydrobia beds. The stratigraphical important species of the genus Hemicyprideis (Ostracoda) are figured and described. For the first time the foraminifer genera Neobulimina CusumAan & WICKENDEN and Glabratella Dorrzen are evidenced at the Mainz basin.
    Description: research
    Keywords: ddc:562
    Language: German
    Type: doc-type:article , publishedVersion
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  • 4
    Publication Date: 2022-09-12
    Description: In bisher als fluviatil angesehenen tertiären Sedimenten im Durchbruchstal des Guldenbaches durch den Taunusquarzit-Härtlingszug des Soonwaldes kann aufgrund sedimentpetrographischer und mikrofaunistischer Analysen eine Verzahnung von fluviatilen mit marin-brackischen Ablagerungen des oberen Rupels (= Schleichsand) belegt werden. Das Schleichsandmeer des Mainzer Beckens und seines Ausläufers, der „Stromberger Bucht”, benutzte das prämitteloligozäne Guldenbachtal als schmalen Korridor in den Ost-Hunsrück. Weitere Vorkommen von mehr oder weniger tonigen Quarzkiesen im Ost-Hunsrück werden beschrieben. Eine Diskussion ihrer Bildungsbedingungen sowie Foraminiferenfunde führen zur Annahme litoraler Ablagerung zur Zeit des Schleichsandmeeres oder im tieferen Chatt. Die angenommene Küstenlinie erlaubt als tektonischer Bezugshorizont die Feststellung einer nach SW unbedeutender werdenden Flexur am Hunsrücksüdrand sowie einer Kippung des Ost-Hunsrück - mit Ausnahme der Moselmulde - nach Süden um ca. 50 m. Weiterhin spricht einiges für eine zusätzliche Kippung vor allem der südlichen Teile nach Osten.
    Description: Abstract: Tertiary sediments in the narrow gap of the stream Guldenbach in the monadnocks of the Taunusquarzit of the Soonwald mountain ranges were up to now thought to be of a fluvial origin. Investigations of the sedimentary petrography and microfauna prove that fluvial sediments dovetail with marine or brackish ones of upper Rupelian age (Schleichsand). The sea, which transgraded from the Mainz basin into the Stromberg embayment at that time, used the preexisting valley of the stream Guldenbach as a narrow corridor into the Eastern Hunsrück. Furthermore some relics of more or less clayey quartz gravels, some of which contain Foraminiferae, are described. The discussion of their sedimentary environment leads to the hypothesis of a litoral sedimentation of the upper Rupelian or Chattian sea. The supposed shoreline as a tectonic reference level shows a flexure at the southern boundary of the Hunsrück with decreasing amounts of uplift towards Southwest. The Hunsrück itself - except the Moselle syncline in the northernmost parts - was tilted southwards with a maximum uplift of about 50 m, and perhaps eastwards, too, especially in the southern parts.
    Description: research
    Keywords: ddc:554.3
    Language: German
    Type: doc-type:article , publishedVersion
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  • 5
    Publication Date: 2022-09-14
    Description: Der Baugraben einer Treibstoff-Pipeline bei Odenbach erschloss kurzfristig ein ca. 200 m mächtiges Profil, das große Teile der Lauterecken-Formation umfasst. Ein neuer Leithorizont wird aufgestellt, drei weitere detailliert beschrieben. Die Abfolge wird mit anderen Aufschlüssen bei Odenbach verglichen.
    Description: Abstract: In 1998 the restoration of the Trans European NATO Pipeline (TENP) in northern Palatinate (Southwest Germany) opened a two hundred meter long exposure yielding big parts of the Lauterecken formation (Lower Permian). The lithology and palaeontology of the outcrop is described, focusing arthropod and fish remains. A new lake horizon called Roetherhof bed is erected. Together with the formerly known Odenbach bed and Medard bed it is described in detail. The whole section is compared with other localities in the vicinity of Odenbach.
    Description: research
    Keywords: ddc:554.3
    Language: German
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  • 6
    Publication Date: 2022-09-14
    Description: Die vorliegende Aufstellung umfaßt 60 Arten, die überwiegend aus dem Unteren Meeressand stammen. Darunter sind 18 Arten, die im Mainzer Becken erstmals nachgewiesen werden. Die ökologische Differenzierung der mitteloligozänen Otolithenfaunen, die als überwiegend autochthon angesehen werden, wird in knapper Form diskutiert. Biogeographisch werden provisorisch drei Gruppen unterschieden.
    Description: Abstract: A list of 60 species is given. Most of the species are from the Unterer Meeressand and 18 species are new for the Mainz basin. The Middle Oligocene otolith associations seem to be mainly autochthonous. Their biostratigraphical, paleoecological and paleobiographical implications are discussed.
    Description: research
    Keywords: ddc:567
    Language: German
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  • 7
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    ARGE GMIT, Bonn
    In:  ARGE GMIT
    Publication Date: 2022-08-31
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2001 enthält die Themenblöcke: Berufsstand: Der Höhepunkt der Welterdölproduktion - ein Wendepunkt für die Menschheit?, Rohstoffe: Erfolgreiche Erdöl-Erdgas-Bohrungen im deutschen Nordsee-Sektor, Forschung: Neue Sonderforschungsbereiche, Geothermie: Neues Projekt in Hannover, Geokalender: Alle Termine und Adressen auf einen Blick
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 8
    Publication Date: 2022-08-31
    Description: Die dauerhafte Sanierung von aktiven Rutschungen ist meist mit erheblichem finanziellen und technischen Aufwand verbunden. In Fällen, in denen weder wichtige Verkehrswege noch zahlreiche Bauwerke betroffen sind, stehen keine großen Geldmittel für eine Sanierung zur Verfügung. Somit ist schnell die Grenze der wirtschaftlichen Verträglichkeit der Maßnahme erreicht. Durch eine Kombination von Zugpfählen, einer Pfahlbock-Stützkonstruktion und gezielten Entwässerungsbohrungen können Rutschungen im Locker- und verwitterten Festgestein dagegen mit relativ geringem Aufwand saniert werden. Die Vorteile dieser Methode liegen in der Flexibilität während der Bauausführung, der Möglichkeit, auch aktive Rutschungen sanieren zu können sowie im geringen Eingriff in den Untergrund. Am Beispiel einer Rutschungssanierung im Rotliegend des Saar-Nahe-Beckens soll dieses konstruktive Verfahren vorgestellt werden, das sowohl in wirtschaftlicher als auch bautechnischer Hinsicht eine interessante Alternative zu konstruktiven Lösungen mit massiven Stützelementen darstellen kann.
    Description: Abstract: The permanent remediation of active landslides most often requires substantial technical and financial investment. In cases where neither important roads nor numerous buildings are impacted, available funds for remediation are limited. Therefore, the economic requirements of intervention quickly surpass available funds. The combination of tension piles and drainage drills is an alternative construction method to stabilize landslides in loose rocks and is associated with a relatively limited amount of investment. This method’s advantages lies in its flexibility during the construction phase, its potential to remediate active landslides, and its limited involvement in the underlying soilirock. The remediation of a landslide in Rheinland-Pfalz provides an overview of this remediation method, which can be a cost effective and technically superior alternative to construction with massive piles.
    Description: research
    Keywords: ddc:620
    Language: German
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  • 9
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    ARGE GMIT, Bonn
    In:  ARGE GMIT
    Publication Date: 2022-08-31
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2001 enthält die Themenblöcke: Berufsleben: Die Paläontologische Bodendenkmalpflege in Deutschland, Geologische Landesdienste: Zehn Jahre Geologisches Landesamt Sachsen-Anhalt, Ausbildung: Bessere Studienbedingungen oder Bildungskatastrophe?, Hochschulen: Neue Studiengänge, Öffentlichkeitsarbeit: Geowissen, Tourismus, Ökonomie und nachhaltige Entwicklung:European Geoparks
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 10
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    ARGE GMIT, Bonn
    In:  ARGE GMIT
    Publication Date: 2022-08-31
    Description: Die zweite Ausgabe der Geowissenschaftlichen Mitteilungen vom 4. Quartal 2000 enthält die Themenblöcke: GEOaktiv (Praxis und Beruf), Geonova (Wissenschaft und Forschung), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport, Geokalender, Anschriften.
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 11
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    ARGE GMIT, Bonn
    In:  ARGE GMIT
    Publication Date: 2022-08-31
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2002 enthält die Themenblöcke: GEO 2002: Planet Erde: Vergangenheit, Entwicklung und Zukunft, Öffentlichkeit: Das Jahr der Geowissenschaften in vollem Gange, Bundesregierung: Paläoklimaforschung unentbehrlich, Berufsleben: Aktivitäten der IAEA, Gesellschaft: Stand der Bildung einer deutschen Dachgesellschaft geowissenschaftlicher Organisationen, Politk: Parlamentarischer Abend in Hannover
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 12
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-08-31
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Juni 2002 enthält die Themenblöcke: Geoaktiv- Praxis und Beruf, Genova - Wissenschaft und Forschung, Geolobby - Gesellschaften, Verbände, Institutionen, Georeport, Geokalender
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 13
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    ARGE GMIT, Bonn
    In:  ARGE GMIT
    Publication Date: 2022-08-31
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Dezember 2001 enthält die Themenblöcke: Berufsleben: Der Geologische Landesdienst in Hessen, Chance: Das Jahr der Geowissenschaften 2002, Forschung: Größte deutsche Forschungsorganisation gegründet, Ausbildung: Neue Studiengäge in Oldenburg und Freiberg, Öffentlichkeitsarbeit: Die Situation der Naturwissenschaftlichen Sammlungen des Museums Wiesbaden
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German , English
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  • 14
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    ARGE GMIT, Bonn
    In:  ARGE GMIT
    Publication Date: 2022-08-31
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Juni 2001 enthält die Themenblöcke: Berufsstand: Weltenergierat warnt vor Problemen in der Energieversorgung, Rohstoffe: 1. Rohstaofftag Baden-Württemberg, Geologische Landesdienste: Verlagerung der Aufgaben des Geologischen Dienstes in Mecklenburg-Vorpommern, Forschung: Geotechnologien - ein geowissenschaftliches Forschungsprogramm gewinnt an Kontur, Berufsbild: Industrielle Beschäftigung eines Geologien- Ein Beispiel aus der NE-Metallindustrie
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 15
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2002 enthält die Themenblöcke: Geoaktiv- Praxis und Beruf, Genova - Wissenschaft und Forschung, Geolobby - Gesellschaften, Verbände, Institutionen, Georeport, Geokalender
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 16
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Dezember 2002 enthält die Themenblöcke: Geoaktiv- Praxis und Beruf, Genova - Wissenschaft und Forschung, Geolobby - Gesellschaften, Verbände, Institutionen, Georeport, Geokalender
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 17
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2002 enthält die Themenblöcke: Geoaktiv- Praxis und Beruf, Genova - Wissenschaft und Forschung, Geolobby - Gesellschaften, Verbände, Institutionen, Georeport, Geokalender
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 18
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Juni 2003 enthält die Themenblöcke: Geoaktiv- Praxis und Beruf, Genova - Wissenschaft und Forschung, Geolobby - Gesellschaften, Verbände, Institutionen, Georeport, Geokalender
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 19
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Dezember 2003 enthält die Themenblöcke: Geoaktiv- Praxis und Beruf, Genova - Wissenschaft und Forschung, Geolobby - Gesellschaften, Verbände, Institutionen, Georeport, Geokalender
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
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  • 20
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2003 enthält die Themenblöcke: Geoaktiv- Praxis und Beruf, Genova - Wissenschaft und Forschung, Geolobby - Gesellschaften, Verbände, Institutionen, Georeport, Geokalender
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
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  • 21
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom März 2004 enthält die Themenblöcke: Geofokus: Impaktkrater auf der Erde - Spuren des kosmischen Bombardements, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 22
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2004 enthält die Themenblöcke: Geofokus: Die frühe Geschichte der Erde, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 23
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    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Juni 2004 enthält die Themenblöcke: Geofokus: Energie für unsere Welt-heute,morgen,übermorgen, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
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  • 24
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-09-01
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom Dezember 2004 enthält die Themenblöcke: Geofokus: Kaltwasser-Karbonate und Tiefwasser-Riffe - eube geobiologische Herausforderung, Geoaktiv (Wirtschaft, Beruf, Forschung und Lehre), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport
    Description: DFG, SUB Göttingen
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
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  • 25
    Publication Date: 2022-10-28
    Description: In der Meisenheim-Formation (Glan-Gruppe) des karbonisch-permischen Saar-Nahe-Beckens treten weitverbreitet vulkanische Aschentuffe auf, die hervorragende Leithorizonte innerhalb der fluvio-lakustrinen Abfolge darstellen. Die laterale Verbreitung sowie die stratigraphische Position und Bedeutung der wichtigsten tephrostratigraphischen Horizonte im nordöstlichen Beckenbereich werden hier dokumentiert. Die Erhaltung der distalen pyroklastischen Fallablagerungen wurde durch das Ablagerungsmilieu und die synsedimentäre Tektonik gesteuert, was sich in einer unterschiedlichen Faziesausbildung der Tuffe widerspiegelt. Die Hauptleithorizonte sind meist aus mehreren aufeinanderfolgenden Tuff- und Tuffitlagen zusammengesetzt. Daneben weisen zahlreiche geringmächtige, lokal begrenzt auftretende Tuffhorizonte auf häufige Vulkanausbrüche bzw. Aschenfallereignisse hin. Innerhalb laminierter bituminöser Tonsteinabfolgen konnten Eruptionspausen von weniger als 200 Jahren bestimmt werden. Die Eruptionszentren lagen südlich des Saar-Nahe-Beckens, sehr wahrscheinlich im Schwarzwald und den Vogesen, möglicherweise auch im Bereich der heutigen Zentralalpen. Eine Aschenherkunft von Vulkanen innerhalb des Beckens wird ausgeschlossen. Zwei primäre Tufflagen im Kappeln- und St. Alban-Leithorizont deuten DRE (dense rock equivalent)-Volumen von mindestens 1,6 bzw. 1,1 km3 an, womit sie deutlich größere Eruptionsereignisse repräsentieren als der Ausbruch des Mount St. Helens 1980. Dabei gehört die Fallablagerung im Kappeln-Tuff zu den bedeutendsten Aschenfallereignissen im Saar-Nahe-Becken vor Beginn des beckeninternen Vulkanismus in der Nahe-Gruppe. Das Alter des Pappelberg-Tuffs von 297,0 + 3,2 Ma zeigt die stratigraphische Position der Meisenheim-Formation im Grenzbereich Karbon/Perm an.
    Description: Abstract: In the Meisenheim-Formation (Glan-Group) of the Carboniferous-Permian Saar-Nahe Basin widespread volcanic ash tuffs occur representing excellent marker horizons within the fluvio-lacustrine sequence. The lateral distribution and Stratigraphie Position and significance of the main tephrostratigraphic horizons in the northeastern part of the basin are documented here. The preservation of the distal pyroclastic fallout deposits was controlled by the depositional environment and the synsedimentary tectonic activity which is reflected by a different facies character of the tuffs. The main marker horizons are offen composed of several successive tuff and tuffaceous layers. In addition, many thin and locally restricted tuff horizons indicate frequent eruptions and ash fall events, respectively. Within laminated bituminous mudstone successions, intereruptive periods of less than 200 years have been determined. The volcanic centres were located south of the Saar-Nahe Basin, most probable in the Black Forest and Vosges but possibly also in the area of the Central Alps. An ash origin from volcanoes within the basin is unlikely. Two primary tuff layers in the Kappeln and St. Alban marker horizon indicate DRE (dense rock equivalent) volumes of at least 1.6 and 1.1 km32, respectively, thus representing distinctly greater eruption events than the Mount St. Helens eruption in 1980. Hence, the fallout deposit in the Kappeln-Tuff belongs to the most important ash fall events in the Saar-Nahe Basin prior to the beginning of the basininternal volcanism of the Nahe-Group. The age of the Pappelberg-Tuff of 297.0 ± 3.2 Ma indicates a Stratigraphie position of the Meisenheim-Formation in the ränge of the Carboniferous/ Permian boundary.
    Description: research
    Keywords: ddc:554.3
    Language: German
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  • 26
    Publication Date: 2022-10-21
    Description: In einer Sandgrube bei Steinhardt wurde im Verzahnungsbereich oligozäner, fluviatiler Kiese des „Proto-Ellerbachs” mit Meeressanden eine horizontbeständige Schwermineralseife gefunden. Sie enthält eine Klinopyroxen-Epidot-Biotit- Assoziation und unterscheidet sich somit deutlich von der Turmalin-Muskovit-Zirkon- Assoziation der Meeressande. Als Muttergesteine für die Turmalin-Muskovit-Zirkon- Assoziation werden tiefgründig verwitterte, devonische Gesteine und die Rotliegend- Sedimente angenommen. Die Klinopyroxene werden auf Rotliegend-Vulkanite zurückgeführt, der Biotit ebenfalls auf die Vulkanite aber auch aufrhyolithische Tuffite und der Epidot auf die Gesteine der metamorphen Hunsrücksüdrandzone.
    Description: Abstract: A concordant Rupelian heavy mineral placer was found in a sand pit at Steinhardt near Bad Sobernheim. It was formed near the mouth of the „Proto-Ellerbach”- creek in an area of interlocking fluvial gravels with marine sands of the Mainz Basin. The placer clearly differs by its clinopyroxene-epidote-biotite-assemblage from the marine sands’ tourmaline-muscovite-zircon-assemblage. Deeply weathered Devonian sediments and the Rotliegend sediments are supposed to be the bedrocks of the latter heavy mineral-assemblage. The clinopyroxenes were derived from volcanic rocks of the Rotliegend, the biotite from the volcanic rocks and rhyolitic tuffites and the epidote from the metamorphic rocks of the South-Hunsrück-zone.
    Description: research
    Keywords: ddc:549.943
    Language: German
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  • 27
    Publication Date: 2022-10-18
    Description: Mit den Tiefbauarbeiten im Rahmen der Neuverlegung einer Gasfernleitung wurde in den Frühjahrs- und Sommermonaten 1999 ein ausgedehntes Profil im variskischen Sockel des zentralen und südlichen Rheinischen Schiefergebirges der geologischen Betrachtung zugänglich. In der ca. 3 m tiefen, über rund 80 km Länge weitgehend quer zum Generalstreichen verlaufenden Grabentrasse wurden die variskisch deformierten Sedimentgesteine des unterdevonischen Grundgebirges hinsichtlich ihrer stratigraphischen und tektonischen Eigenheiten aufgenommen und zur Konstruktion eines geologischen Profilschnittes ausgewertet. Von Nordwesten nach Südosten konnten die im Bereich der Westeifel, der Moselmulde und des Hunsrücks erschlossenen Gesteinsverbände als drei Profilabschnitte den faziell und tektonisch typisch geprägten Baueinheiten des Rheinischen Schiefergebirges zugeordnet werden. In der stratigraphischen Abfolge überwiegen Schichten der Unter- und Oberems- Stufe. Untergeordnet treten Gesteine der Siegen-Stufe im Kernbereich des Manderscheid- An tiklinoriums und an der Nordflanke der Moselmulde zu Tage, vom paläogeographischen Muster bestimmt in jeweils unterschiedlicher Lithofazies. Die gesamte Abfolge unterdevonischer Schichtverbände ist charakterisiert durch intensiven Faltenbau und mehr oder weniger starke Störungstektonik, von Norden nach Süden insgesamt gekennzeichnet durch zunehmende Komplexität und stratigraphische Bedeutung.
    Description: Abstract: By the excavations for the installation of a new gas-pipeline in spring and summer 1999 a large profile across the central and Southern parts of the Rhenish Massif became available. In the trench line, about 3 m deep, trending perpendicular to the general strike direction, sedimentary rocks of mainly Lower Devonian age have been investigated between Dorsel/Eifel Hills and the Hunsrück area with regard to Stratigraphie and tectonic elements. The data have been evaluated to build up a geologic profile of approximately 80 km an length. From NW to SE the rock sequences of the Eifel Hills, the Mosel-syncline and the Hunsrück area can be correlated with facies and tectonic units of the Rhenish Massif. The Stratigraphie sequence is dominated by lower and upper Emsian beds. Older rocks of Siegenian age and of variable lithologic facies are rare. They locally occurr in the core of the Manderscheid Anticline and the northern flank of the Mosel-Syncline, depending on their paleographic position in the rhenish basin. The whole sequence of Lower Devonian rocks is characterised by intensive folding and fault tectonics which incrase from North to South in complexity and Stratigraphie relevance.
    Description: 1. Einleitung 2. Regionale Abgrenzung und geologischer Rahmen 3. Die stratigraphische Abfolge 3.1. Abschnitt Nord (Westeifel) 3.1.1. Obere Siegen-Stufe (Herdorf-Unterstufe) — Saxler-Schichten 3.1.2. Unterems-Stufe 3.1.2.1. Ulmen-Unterstufe — Eckfeld-Schichten — Reudelsterz-Schichten 3.1.2.2. Singhofen- bis Vallendar-Unterstufe — Stadtfeld Schichten — Klerf-Schichten 3.1.3. Oberems- bis untere Eifel-Stufe 3.2. Abschnitt Mitte (Moselmulde) 3.2.1. Siegen- bis Unterems-Stufe (Ulmen-Unterstufe) — Hunsrückschiefer (sensu lato) 3.2.2. Unterems-Stufe (ohne Ulmen-Unterstufe) 3.2.2.1. Singhofen-Unterstufe — Co ehern-Schichten 3.2.2.2. Vallendar-Unterstufe — Gladbach-Schichten — Klerf-Schichten 3.2.3. Oberems-Stufe 3.2.3.1. Lahnstein-Unterstufe — Emsquarzit — Flussbach-Schichten 3.2.3.2. Laubach-Unterstufe — Höllenthal-Schichten 3.2.3.3. Kondel-Unterstufe — Flaserschiefer — Kieselgallenschiefer 3.3. Abschnitt Süd (Hunsrück) 3.3.1. Siegen-Stufe 3.3.1.1. Herdorf-Unterstufe — Taunusquarzit, Dhrontal-Schichten 3.3.2. Unterems (Ulmen- bis Singhofen-Unterstufe in Hunsrückschiefer-Fazies) 3.3.2.1. Ulmen-Unterstufe (Hunsrückschiefer sensu stricto) — Zerf-Schichten / Zerfer Fazies — Kaub-Schichten / Kaub er Fazies 4. Tektonik 4.1. Vorbemerkungen 4.2. Faltenbau, Schieferung und Vergenzverhältnisse 4.2.1. Abschnitt Nord (Westeifel) 4.2.2. Abschnitt Mitte (Moselmulde) 4.4.3. Abschnitt Süd (Hunsrück) 4.3. Störungen 4.3.1. Abschnitt Nord (Westeifel) 4.3.2. Abschnitt Mitte (Moselmulde) 4.3.3. Abschnitt Süd (Hunsrück) 5. Fossilien 6. Bilanz und Ausblick 7. Geologische Profile Schriften
    Description: research
    Keywords: ddc:554.3
    Language: German
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  • 28
    Publication Date: 2022-08-04
    Description: Zur Charakterisierung der Anteile von Lössen und Verwitterungsprodukten der liegenden Keuper- und Liasgesteine innerhalb kolluvialer Mischsedimente und holozäner Terrassenkörper erweisen sich in Oberfranken neben Korngrößenverteilungen insbesondere Quarz-Feldspat- und Albit-Mikroklin-Quotienten als geeignete Indizes. Danach sind an den untersuchten bodenerosiv überprägten Flachhängen bevorzugte Abtragung von Löß und Liegendmaterial an den Oberhängen, vorherrschender Durchtransport an den Mittelhängen und Ablagerung von Mischsedimenten an den Unterhängen zu erkennen. In den holozänen Sedimenten der Vorfluter sind Lößderivate demgegenüber nur gering vertreten, woraus auf vorherrschenden Durchtransport dieses Materials in den untersuchten Talstrecken und — im Vergleich mit niedersächsischen Beispielen entsprechender Größenordnung — auf eine regionale Differenzierung der holozänen fluvialen Dynamik geschlossen wird, die möglicherweise auf Unterschiede des Regionalklimas zurückzuführen ist.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 29
    Publication Date: 2022-08-04
    Description: In dem Hügelgebiet um den Falken-Berg zwischen Fallingbostel und Bergen Kr. Celle zeichnen sich 3 Endmoränenbögen ab, der Örbker, der Becklinger und der wenig deutlich ausgeprägte Kl. Bockeler Endmoränenbögen. Örbker und Kl. Bockeler Endmoränenbögen verdanken ihre Entstehung Gletscherloben, die von NW heranrückten; der Becklinger Endmoränenbögen geht auf einen von NE heranrückenden Lobus zurück. Keine dieser Endmoränen ist vom nordischen Inlandeis überfahren worden. Ein nahe den Endmoränenbögen wurzelnder Fächer aus Schmelzwasser-Ablagerungen läßt sich bis nahe an die Aller-Niederung heran verfolgen. Er überlagert die drenthestadiale Hauptmoräne, ist also jünger als diese. Die Endmoränen zwischen Fallingbostel und Bergen sind in einer späten Phase des Drenthe-Stadiums der Saale-Eiszeit entstanden.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 30
    Publication Date: 2022-08-04
    Description: Am nördlichen Harzrand zwischen Benzingerode und Heimburg (Sachsen-Anhalt) konnten bei archäologischen Ausgrabungen mehrere bis zu 100 m lange Aufschlüsse in pleistozänen und holozänen Sedimenten des Hellbach-Schwemmfächers bearbeitet werden. Über pleistozänen Sedimenten eines ca. 2 km breiten Schwemmfächers mit Eiskeilpseudomorphosen, Kryoturbationserscheinungen sowie zentimetermächtigen Lösslagen, sind verschiedene holozäne Kolluvien, Auesedimente und Bodenbildungen auf einem kleineren, ca. 200 m breiten Schwemmfächer abgelagert worden bzw. entstanden. Stellenweise vorhandene Schwarzerdereste sowie mit schwarzem Bodenmaterial gefüllte Pfosten- und Vorratsgruben unterschiedlicher vorgeschichtlicher Epochen deuten auf eine relativ weite Verbreitung von spätpleistozänen und frühholozänen Schwarzerden in der Region hin. Im Auenbereich finden sich an der Basis der holozänen Kolluvien Reste von schwarzen, humosen, stark tonigen Horizonten mit einem lössähnlichen Sediment im Liegenden. Ob es sich hierbei um in situ gebildete Schwarzerden bzw. Schwarze Auenböden oder um anthropogene, durch Brandwirtschaftsweisen geschaffene, schwarze Horizonte handelt, ist noch unklar. Holzkohle aus dem schwarzen Horizont konnte auf rund 5.500 v. Chr. datiert werden. Das lössähnliche Sediment im Liegenden ergab OSL-Alter von ca. 5.910 v. Chr. (7,9 ± 0,5 ka). Nach Ende dieser Stabilitätsphase kam es zu einer oder mehreren größeren Überflutungen des damaligen Auenbereichs. In dieser Aktivitätsphase wurde der schwarze Horizont gekappt und zunächst mit Grobmaterial, später von einer meist 10-20 cm mächtigen feinmaterialreichen, dunkelbraunen Sedimentschicht überlagert. Diese Schicht bildete für längere Zeit die Oberfläche, enthält kaiserzeitliche Funde in situ und wird im Hangenden von gröberen Sedimenten und mächtigen, zweiphasigen mittelalterlichen Auelehmen abgedeckt. Rinnen im jüngsten Auelehm enthalten ziegel- und kalksteinreichen Schotter und repräsentieren vermutlich den letzten Lauf des Hellbachs vor seiner Begradigung in der Mitte des 19. Jahrhunderts. Nach den vorliegenden Befunden ist ein Zusammenhang zwischen den einzelnen fluvialen Aktivitätsphasen und der Besiedlung und Wirtschaftsweise im Einzugsgebiet des Hellbaches sehr wahrscheinlich, kann jedoch nicht zweifelsfrei nachgewiesen werden.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 31
    Publication Date: 2022-07-27
    Description: Die Zusammenstellung der Foraminiferen (535 Taxa) und Ostrakoden (147 Taxa) beruht auf der Verarbeitung der verfügbaren Literatur. Da spezielle taxonomische Arbeiten in diesem Zusammenhang nicht möglich waren, finden sich in den Tabellen auch noch die alten Namen. Es werden kurze Angaben über stratigraphisch wichtige Formen und zur Ökologie gemacht.
    Description: Abstract: The synopsis of the foraminifers (535 taxa) and ostracods (147 taxa) from the “Pre-aquitanian’’ of the Mainz basin is based on a critical review of the available literature. As in this context special taxonomic studies were not intended the earlier taxonomic names are stillto be found. Brief data are given on biostratigraphically important taxa and to the ecology.
    Description: research
    Keywords: ddc:562
    Language: German
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  • 32
    Publication Date: 2022-07-27
    Description: research
    Keywords: ddc:562
    Language: German
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  • 33
    Publication Date: 2022-08-02
    Description: Im östlichen Niedersachsen und westlichen Sachsen-Anhalt wurden in den letzten Jahrzehnten in zwei großen Untersuchungskampagnen mächtige quartäre Ablagerungen beobachtet und dokumentiert. Die Elster-zeitlichen Anteile dieser Ablagerungen sind Gegenstand dieser Veröffentlichung. Ablagerungen der ältesten Vereisung aus diesem Gebiet wurden schon vor über 100 Jahren beschrieben. Im Helmstedter Braunkohlerevier waren über lange Zeit über mächtigen Vorschütt-Schmelzwassersanden zwei Elster-Grundmoränen aufgeschlossen. Stillwasserbildungen verschiedenster Ausbildung waren Zeugen des periglaziären Geschehens in diesem Raum. Am Ende des Pleniglazials kamen in kleinen Seen limnische Sedimente zur Ablagerung, die Hinweise auf mehrere Spätelster-Interstadiale lieferten. Im Zuge einer sehr umfangreichen ingenieurgeologischen Erkundung im nur wenige Kilometer entfernten Allertal bei Morsleben wurden dort einige Jahre später zahlreiche Kernbohrungen niedergebracht und intensiv geologisch dokumentiert und beprobt. Die erbohrten Ablagerungen ähneln den Elster-zeitlichen Sedimenten aus dem Tagebau Schöningen, sind jedoch durch zahlreiche Subrosionssenken noch mächtiger. Hierdurch lassen sich auch mehrere kleine Oszillationen zu Beginn der Überfahrung durch das Elster-Inlandeis nachweisen. An einer Stelle im Allertal ist zudem relativ sicher eine jüngste dritte Elster-Grundmoräne nachweisbar. Die periglazären Bildungen kamen hier in einem eher fluviatil geprägten Milieu zur Ablagerung, das auch die Erhaltung sicher zuordnenbarer Spätelster-Interstadiale behinderte. Eine Korrelation der beobachteten Ablagerungen mit denen anderer Räume ist bisher nur regional, nicht jedoch überregional möglich.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 34
    facet.materialart.
    Unknown
    Geozon Science Media
    Publication Date: 2022-08-02
    Description: Die Küsten des nördlichen Hokkaidos gehören zu den äquatornächsten Bereichen, die in saisonalem Wechsel einer wellen- und strömungsdominierten Sommerformung (8—10 Monate) und einer packeis- und frostinduzierten Winterformung (2—4 Monate) unterliegen. Es werden für diesen Raum die typischen Prozesse der Sommer- und Wintermonate beschrieben. Im Sommer werden die Küsten wesentlich stärker geformt als im Winter und die durch Eispressung entstandenen Formen an den Stränden und Dünen überdauern nur in Relikten. Dennoch kann die Zone der saisonal vereisten Küsten klimageomorphologisch von den Küsten wärmerer Breiten abgegrenzt werden, da nur hier ein derart großer Kontrast zwischen Sommer- und Winterformung existiert. Diese Grenze ist allerdings ein breiter Saum und kein schmaler Übergang, wie es für solche physisch geographischen Grenzen die Regel ist.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 35
    Publication Date: 2022-08-05
    Description: In den Lössdeckschichten des Steinbruchs Mainz-Weisenau (Heidelberger Zement AG) sind im Hangenden des letztinterglazialen Bodens drei Altwürmhumuszonen aufgeschlossen (Mosbacher Humuszonen). Auf der Grundlage einer detaillierten Profilbeschreibung erfolgte eine lückenlose Entnahme von Sedimentproben zur Untersuchung der Molluskenfaunen. Die Aussage des Fossilberichts wird durch die Anwesenheit von verlagerten Sedimenten unter und zwischen den Humuszonen und die Möglichkeit einer sekundären Einmischung von Schalenmaterial beeinträchtigt. Dennoch lässt der Fossilbericht nach dem letzten Interglazial drei Wärmeschwankungen erkennen, die mit den Humuszonen korrelierbar sind. In den Sedimenten zwischen Eemboden und unterer Humuszone sowie zwischen mittlerer und oberer Humuszone wurden Reste kaltzeitlicher Faunen festgestellt, die auf Kälteperioden hinweisen. Der Bereich der unteren und, in geringerem Maße, der Bereich der mittleren Humuszone zeichnen sich durch die Anwesenheit von warmzeitlichen Faunenelementen aus (darunter ausgesprochene Waldarten), was auf einen mehr oder weniger hohen Grad an Wiederbewaldung schließen lässt. Es handelt sich dabei ausnahmslos um Waldarten, die sowohl in Laub- als auch in Nadelwaldbeständen auftreten können. Der Abschnitt zwischen unterer und mittlerer Humuszone und die obere Humuszone führen lediglich Steppen- und Waldsteppengesellschaften, die eng miteinander verzahnt sind. Der vorliegende Fossilbericht lässt sich gut mit den allgemein akzeptierten Vorstellungen über die Klimaentwicklung im frühen Würm vereinbaren, die sich aus Tiefsee- und Eisisotopenkurven ergeben haben. Zum gegenwärtigen Zeitpunkt wird eine Parallelisierung der unteren und mittleren Humuszone von Mainz-Weisenau mit den beiden bewaldeten norddeutschen Interstadialen Amersfoort/ Brörup und Odderade sowie den beiden St-Germain-Interstadialen in Ostfrankreich für wahrscheinlich gehalten. Für die Korrelation der oberen Humuszone werden verschiedene Möglichkeiten diskutiert.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 36
    Publication Date: 2022-08-05
    Description: Vorgestellt werden Untersuchungen zur holozänen Landschaftsentwicklung im Gebiet der Müritz, des größten Sees der Norddeutschen Tiefebene. Geomorphologische Untersuchungen zeigen für das Holozän bis zum Mittelalter eine im Wesentlichen aufwärts gerichtete Tendenz des Seespiegels (9500 BP: 57 m NN, 5400 BP: 61 m NN, AD 1100: 61 m NN, AD 1280: 62-63 m NN, nach AD 1300: 65 m NN, AD 1788: 63,5 m NN, heute: 62 m NN). Östlich des Sees wurden unter Wald große Flächen mit jungen anthropogenen Erosionsspuren nachgewiesen. Vier Pollendiagramme geben einen Überblick zur Vegetationsentwicklung auf verschiedenen Standorten und bei unterschiedlich starkem menschlichen Einfluß. Die bislang im Gebiet nachgewiesenen 401 archäologischen Fundplätze datieren überwiegend in das Neolithikum, die Bronzezeit und die Slawenzeit. Die Auswirkungen des Menschen auf den See und sein Umland sowie die Qualität der Befunde stehen im Mittelpunkt der Diskussion.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 37
    Publication Date: 2022-08-05
    Description: Glaziale Sedimente und Formen der tropischen Anden enthalten Paläoklima-Archive. Für die Jüngere Dryaszeit (Younger Dryas = YD) besteht eine kontroverse Diskussion bezüglich der Gletschervorstöße. Im Gebiet des Papallacta-Passes (Ostkordilleren in Ecuador) wird ein Gletschervorstoß durch Till und Moränen dokumentiert. Die glazialen Sedimente werden unter- und überlagert von Tephrahorizonten, Torf und anderen Sedimenten, die reich an organischem Material sind. Radiokarbon-Altersbestimmungen werden somit möglich. 29 14C-Alter zu diesem Gletschervorstoß publizierten Clapperton et al. (1997); weitere 29 14C-Alter werden hier vorgestellt. Die Daten belegen sowohl feuchte (=Gletschervorstoß) als auch trockene (= Gletscherabschmelzen) Klimabedingungen während der Jüngeren Dryaszeit. Unter Berücksichtigung der kalibrierten 14C-Alter ergibt sich ein Gletschervorstoß in der zweiten Hälfte der Jüngeren Dryaszeit und zu Beginn des Holozäns. An dem Beispiel wird belegt, daß die Interpretation der 14C-datierten Jüngere Dryaszeitlichen Gletschervorstöße mit größter Sorgfalt vorgenommen werden muß.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 38
    Publication Date: 2022-08-05
    Description: Nach Vorarbeiten 1977 und 1979 wurden im Bereich der paläolithischen Fundstelle Şehremuz im Jahre 1982 zwei Grabungskampagnen von je zwei Monaten durchgeführt. Es konnten zwei archäologische Komplexe in unterschiedlicher geologischer Lagerung festgestellt werden: a) Silexabschläge und Faustkeile im obersten aufgeschlossenen Schotter des Keluşk-Baches, eines Euphratzuflusses. Dieser Seitentalschotter ist korrelierbar mit einem etwa 60 m über der heutigen Talaue liegenden Euphratschotter. b) „Mittelpaläolithische" Inventare in einem über den Keluşk-Schottern liegenen Glacis, weitgehend nur aus Oberflächenfunden bekannt. Sie sind aufgrund ihrer Einlagerung jünger als der "Faustkeilkomplex". Die Inventare mit Faustkeilen sind einem entwickelten faustkeilführenden Paläolithikum zuzurechnen. Auf sie ist die vorliegende Untersuchung konzentriert. Die durch die Silexartefakte belegten zahlreichen Begehungen des alten Keluşk-Bettes durch den paläolithischen Menschen haben ihre Ursache u.a. in einem hohen natürlichen Anteil von Silex im Schotter. Neben vollständigen Knollen liegt zahlreicher Naturbruch vor, der gegen die Stücke mit anthropogenen Bearbeitungsspuren abgegrenzt werden muß. Dabei kommt der Konfiguration der Einzelmerkmale — Dimensionen; Abbaufläche und Schlagmerkmale — die größte Bedeutung zu. Die Bearbeitung der Steinartefakte unter funktionalen Gesichtspunkten ist ein wichtiger Teil der Untersuchungen: Die Methoden werden beschrieben. Form und Zurichtung der Faustkeile lassen makroskopisch mögliche Funktionsflächen zum tiefen Einschneiden etwa in Fleisch und mögliche Funktionskanten zum Ritzen oder flach Einschneiden erkennen. Im mikroskopischen Bereich werden an Artefakten punktuell Gebrauchsspuren faßbar, die z.B. die Benutzung eines Faustkeils sowohl zum Einschneiden in Fleisch wie auch zum Zertrümmern von Knochen belegen.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 39
    Publication Date: 2022-08-05
    Description: Dreizehn Travertinproben von den Lokalitäten Tata, Vértesszöllös, Dunaalmás und Buda werden mit Hilfe zweier neuerer Absolutdatierungsverfahren untersucht, der Th-230/U-234- und der ESR-Methode. Für acht der untersuchten Proben ergibt sich eine gute Übereinstimmung zwischen den Th/U- und den ESR-Altern, zwei Proben waren aufgrund extrem hoher Mangan-Gehalte nicht ESR-datierbar und in drei Fällen ergaben sich deutliche Diskrepanzen. Travertine aus dem Riß/Würm Interglazial haben ein Alter von ca. 100.000 a, die des vorletzten Interglazial zeigen ein Alter von 200.000 a und etwas darüber die des drittletzten Interglazials weisen ein Alter von über 300.000 a auf.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 40
    Publication Date: 2022-08-05
    Description: Im unteren und mittleren Werratal läßt sich eine 5—8 m ü. Talaue gelegene Terrasse ausgliedern, die an mehreren Lokalitäten eine weite Verbreitung hat und aufgrund ihres Aufbaus und ihrer Deckschichten (z.T. Löß) als hochwürmzeitliche Niederterrasse eingestuft wird. Sie wurde schon im Spätglazial durch 0,5—1,0 m tiefen Rinnen zerschnitten, die von wahrscheinlich umgelagerten Niederterrassenschottern oder feinkörnigeren Sedimenten wieder aufgefüllt wurden. Die spätglaziale und frühholozäne Flußgeschichte läßt sich dank zeitweilig günstiger Aufschlußverhältnisse bei Eschwege recht gut rekonstruieren (Abb. 6 und 7). Dies gelingt hier besser als im Werraabschnitt auf dem Gebiet der DDR, der von Ellenberg (1967 bis 1975) sehr genau untersucht worden ist. „Ried"ablagerungen in ehemaligen Werrarinnen können präallerödzeitlichen und jungtundrenzeitlichen bis borealen Alters sein. Wie im Leinetal finden sich im Werratal zwei verschieden alte Auelehme, von denen der ältere stellenweise eine wahrscheinlich dem postglazialen Klimaoptimum zuzuordnende Auen-Schwarzerde trägt. In den „Ried"ablagerungen konnten 12 Flußmuschel- bzw. -Schneckenarten gefunden und bestimmt werden.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 41
    Publication Date: 2022-08-05
    Description: Aus dem nördlichen Galizien (NW-Spanien) werden von zwei Lokalitäten (Playa de Barañán, westl. La Coruña, und Cangas de Foz, westl. Ribadeo) jungpleistozäne Sediment-Boden-Folgen beschrieben, die auf einem 3—5 m ü. M. gelegenen Felssockel bzw. auf einer ca. 25 m ü. M. gelegenen Küstenterrasse auflagern. Mehrere 14C-Daten sowie Vergleiche mit früher aufgenommenen Sediment-Boden-Folgen in der näheren und weiteren Umgebung lassen den Schluß zu, daß in beiden Fällen eine nahezu vollständige würmzeitliche Schichtenfolge entwickelt ist, die von fossilen Braunerden bzw. kräftigen fossilen Ah-Horizonten gegliedert ist. Zwischen die fossilen Böden bzw. Bodensedimente sind möglicherweise äolisch entstandene Schlurfe bzw. Sande und Solifluktionsschuttdecken eingeschaltet. Die wahrscheinlich altwürmzeitlichen Profilteile zeichnen sich durch viel Holzkohle aus und weisen auf eine holzreiche Vegetation hin.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 42
    Publication Date: 2022-08-05
    Description: Beim Vorstoß sowie Rückzug des Eises werden Sandersedimente abgelagert. Sie setzen sich aus gröberen Vorschütt- und feineren Nachschüttsanden zusammen, die (meistens) durch eine Grundmoräne voneinander getrennt sind. Vorschüttsand, Grundmoräne und Nachschüttsand bilden einen glaziären Zyklus. Fehlt die Grundmoräne, so ist eine genetische Gliederung der Sedimente in eine Vorstoß- und Rückzugsphase erschwert. Bei der Sedimentuntersuchung zeigte sich, daß einzelne Korngrößenfraktionen für eine Gliederung des Sanders kaum von Bedeutung sind. Die Zusammenfassung von Korngrößenfraktionen zu Korngrößengruppen (Tab. 1) ermöglichte eine exakte Gliederung der Sandersedimente und damit die genetische Ansprache der Gletscherablagerungen am unteren Niederrhein. Aufgrund der Einlagerung von Grundmoränenmaterial in den Sandersedimenten konnten für das Drenthe-Stadial im Raum Louisendorf-Moyland drei Eisvorstöße nachgewiesen werden.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 43
    facet.materialart.
    Unknown
    Geozon Science Media
    Publication Date: 2022-08-05
    Description: Der Rodderberg bei Bonn ist der nördlichste Teil des Osteifel-Vulkanfeldes aus dem Pleistozän. Seine mehrphasige Entstehungsgeschichte ist verzahnt mit den fluviatilen Sedimenten des Rheins und den äolischen Sedimenten aus den Eiszeiten. Die dort aufgeschlossenen Gesteine Basalt, Löß und vulkanthermisch beeinflusster Löß erlauben den Vergleich von Magnetisierungen von Materialien etwa gleichen Alters, aber unterschiedlicher Zusammensetzung und Geschichte. Die von der lokalen Erdmagnetfeld-Richtung deutlich abweichende flache Magnetisierungsrichtung der Basaltproben ist durch Blitzschlag verursacht worden und stellte sich als Beispiel von Blitzschlag-Magnetisierung heraus. Aus der Verteilung der Deklination der Magnetisierung konnte die Einschlagstelle der Blitze in etwa 5 m vom Probenprofil ermittelt werden. Eine aeromagnetische Vermessung des Rodderberges hat neue Hinweise zu seiner Struktur ergeben: Die Anomalie erstreckt sich von NNW nach SSE, der magnetisch wirksame Teil der Vulkanstruktur beschränkt sich auf den Bereich innerhalb des topographisch erkennbaren Kraters. Der umlaufende Schlacke-Aschewall ist magnetisch nicht erkennbar. Unterschiede der Anomalieform aus Messungen am Boden und in 35 m Höhe (Aeromagnetik) legen den Schluss nahe, dass die magnetisch wirksame Kraterstruktur einen flachgründigen Körper aus pyroklastischem Material anzeigt. Mit einigem Abstand darunter ist weiterer Basalt zu erwarten. Mit dem Rodderberg scheint uns die Natur einen Vulkan zu liefern, der am Beginn von phreatomagmatischen Erscheinungen geprägt war, dessen zweite Hälfte seiner lang währenden Genese aber die eines mehr klassischen Vulkans war.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 44
    Publication Date: 2022-08-05
    Description: Geowissenschaftliche Untersuchungen bei Kallmünz in der südöstlichen Fränkischen Alb (Bayern) erbrachten paläobotanische Proben für Pollen- und Holzkohleanalyse. Die Auswertung gibt Hinweise auf die Vegetationszusammensetzung zu verschiedenen Zeiten des Holozäns. Intensive Landschaftsnutzung setzt spätestens in der Bronzezeit ein. In der römischen Periode und im Mittelalter können ausgeprägtere und großflächigere Eingriffe belegt werden. Für paläoökologische Forschung in Karstgebieten ist die Anwendung der Holzkohleanalyse von besonderem Nutzen, da palynologische Methoden aufgrund der Moorarmut nur begrenzt anwendbar sind.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 45
    Publication Date: 2022-09-29
    Description: Die Taxonomie einiger Brackwasser-Mollusken der höchsten Cerithienschichten und der Inflaten-Schichten (wahrscheinlich Miozän, Mainzer Becken) wird revidiert und folgende Namensänderungen werden vorgeschlagen: Vitta subangularis (Sandberger, 1860) ex Clithon (Vittoclithon) subangularis, Hydrobia inflata (Lill, 1830) ex Hydrobia inflata „(Faujas, 1806)" nom inval, Granulolabium plicatum (Bruguiere, 1792) ex Pirenella plicata, Tympanotonos margaritaceus (Brocchi, 1814) s. lat. ex Tympanotonos submargaritaceus (Braun, 1851) (non Orbigny, 1850), Perna (Perna) faujasi (Brongniart, 1822) ex Mytilus faujasi, Polymesoda (Pseudocyrena) donacina (Sandberger, 1861), bisher nur synonym mit Corbicula faujasi (Deshayes, 1830) gehalten. Außer dem Oberen Corbicula faujasi-Horizont in den Inflaten-Schichten und dem Unteren Corbicula fauj asi-Horizont in den höchsten Cerithienschichten existiert noch ein Polymesoda donacina-Horizont, wahrscheinlich unterhalb des Unteren Corbicula faujasi-Horizontes.
    Description: Abstract: The taxonomy of several brackish-water mollusks of the highest Cerithienschichten and of the Inflaten-Schichten (Cerithium Formation, Inflata Formation) (probably Miocene, Mainz Basin, West Germany) is reviewed and the following name alterations are proposed: Vitta subangularis (Sandberger, 1860) ex Clithon (Vittoclithon) subangularis, Hydrobia inflata (Lill, 1830) ex Hydrobia inflata „(Faujas, 1806)" nom. inval., Granulolabium plicatum (Bruguiere, 1792) ex Pirenella plicata, Tympanotonos margaritaceus (Brocchi, 1814) s. lat. ex Tympanotonos submargaritaceus (A. Braun, 1851) (non Orbigny, 1850), Perna (Perna) faujasi (Brongniart, 1822) ex Mytilus faujasi, Polymesoda (Pseudocyrena) donacina (Sandberger, 1861), removed from synonymy with Corbicula faujasi (Deshayes, 1830). The Stratigraphie significance of Polymesoda (Pseudocyrena) donacina and of Corbicula faujasi is discussed.
    Description: research
    Keywords: ddc:562
    Language: German
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  • 46
    Publication Date: 2022-09-29
    Description: Die traditionell als „Obere Cerithien-Schichten, oberer Teil“ und „Inflata-Schichten” bezeichneten stratigraphischen Einheiten im Untermiozän des Mainzer und Hanauer Beckens werden als lithostratigraphische Formationen neu definiert. Als neue Namen werden die den Internationalen Richtlinien für Stratigraphische Nomenklatur angepassten Begriffe Oberrad-Formation [für Obere Cerithien-Schichten, oberer Teill und Rüssingen-Formation [für Inflata-Schichten] eingeführt. Die Formationen werden beschrieben und Typusprofile, einschließlich Grenzstratotypus- Profilen, vorgeschlagen. Da eine geologisch aussagefähige Untergliederung der tertiären Schichtenfolge im Mainzer und Hanauer Becken allein aufgrund von Gesteinsmerkmalen wegen rascher lateraler und vertikaler Wechsel im Allgemeinen nicht möglich ist, werden paläontologische Definitions- und Abgrenzungskriterien beibehalten. Die beckenweit beobachtbaren Abfolgen von Faunenassoziationen (Mollusken, Ostrakoden, Foraminiferen) werden dabei als ein Lithofazies-Element gewertet.
    Description: Abstract: The stratigraphical units traditionally known as „Obere Cerithien-Schichten, oberer Teil“ and „Inflata-Schichten“ (Early Miocene, Mainz and Hanau Basins) are redefined as lithostratigraphical units. To conform with the International Guidelines for Stratigraphical Nomenclature, they are renamed as Oberrad-Formation (for Obere Cerithien- Schichten, oberer Teil) and Rüssingen-Formation (for Inflata-Schichten). The formations are described, and type sections including boundary type sections are proposed. As a geologically meaningful subdivision of Tertiary sediment packages in the study area is usually impossible from lithological characters alone due to rapid vertical and lateral lithofacies variations, palaeontological criteria for formation definition and delimitation are maintained. The basinwide succession of faunal associations (mollusks, ostracods, foraminifers) is thereby considered as a lithofacies element of the formations.
    Description: research
    Keywords: ddc:554.3 ; ddc:562
    Language: German
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  • 47
    Publication Date: 2022-08-17
    Description: In einigen Teilen der Bitburger Triasmulde konnten die Abfolge und die Lagerung der Schichten bei Baugrunduntersuchungen im Bereich der Nordumgehung von Trier zwischen Kyll- und Sauertal und nördlich von Bitburg näher geklärt werden. Einerseits konnten dadurch Erd- und Grundbaumaßnahmen sicherer beurteilt und andererseits lithostratigraphische und tektonische Vergleiche gezogen werden.
    Description: research
    Keywords: ddc:554.3
    Language: German
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  • 48
    Publication Date: 2022-08-17
    Description: In der Umgebung von Homburg/Saar werden die Tektonik und die Schichtenfolge des Buntsandstein der Nordwestflanke der Pfälzer Mulde beschrieben. Aufgrund der Auswertung aller bekannten Brunnenbohrungen und einer geologischen Kartierung können die Lage und die Ausbildung der Kluftgrundwasserleiter in den verschiedenen tektonischen Schollen näher charakterisiert und in Schnitten dargestellt werden. Sie bilden großräumig zusammenhängende Grundwasserstockwerke im höheren Buntsandstein (Voltziensandstein, Felsbänke in den Zwischenschichten, Obere Felszone), in den Karlstal-Schichten (Karlstal-Felszone) und im tieferen Buntsandstein (Rehberg- und Trifels-Schichten). Der für die Wasserversorgung wichtige tiefere Buntsandstein- Grundwasserleiter hat im peripheren Nordwestteil der Mulde (Westpfälzische Moorniederung) generell höhere Transmissivitäten, als in deren innerem Teil (Sickinger Höhe), wo er jedoch durch die auflagernden Karlstal-Schichten besser geschützt ist.
    Description: Abstract: The tectonics and strata sequence of the Bunter of the northwest flank of the Palatinate syncline in the Homburg/Saar area are described. Based on the evaluation of all known well boreholes and geological mapping, the location and development of the fissured aquifers in the various tectonic blocks can be characterized and illustrated in profiles. They form connected aquifer tables over large areas in the higher Bunter (Voltziensandstein, Zwischenschichten, Obere Felszone), in the Karlstal beds (Karlstal-Felszone) and in the deeper Bunter (Rehberg- and Trifels-Schichten). The deeper Bunter aquifer, being important for trinking water supply, has generally higher transmissivities in the peripheric northwestern part of the syncline (Westpfälzische Moorniederung) than in the interior part (Sickinger Höhe). In the interior part however this aquifer is better protected by the superposed Karlstal beds.
    Description: 1 Einleitung \ 2. Geographisch-morphologischer Überblick 3. Tektonik 4. Paläogeographie, Faziesentwicklung 5. Schichtenfolge und Charakterisierung der Grundwasserleiter 5.1. Stauf-Schichten (sSt bzw. zSt) 5.2. Trifels-Schichten (sT) 5.3. Rehberg-Schichten (sR) 54. Karlstal-Schichten (sK) 5.5. Höherer Buntsandstein 5.5.1. Obere Felszone (sOF) und Zwischenschichten (soZ) 5.5.2. Voltziensandstein (soV) 5.6. Unterer Muschelkalk (mu) 5.6.1. Muschelsandstein und Mergelige Schichten ( mul) 5.6.2. Terebratelzone mit basaler Hauptterebratelbank (zusammen als mu 1 T dargestellt) Schriften Anhang
    Description: research
    Keywords: ddc:554.3 ; ddc:551.49
    Language: German
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  • 49
    Publication Date: 2022-08-17
    Description: Die Funktion der im Teil 1 (Herrez£ 2001) beschriebenen Grundwasserleiter wird im Teil 2 zusammen mit ihren Grundwässern näher erläutert. Je nach Höhenlage und tektonischen Gegebenheiten gelangen die unterirdischen Abflüsse zu verschiedenen Vorflutern. Es kann gezeigt werden, dass der unterirdische Abfluss der tiefen Grundwasserleiter des Arbeitsgebietes (Rehberg-, Trifels- und Stauf-Schichten) größtenteils zu den Vorflutern in der Saarpfälzischen Moorniederung gelangt. Beim Brunnenbau sollen je nach Standort die Ausführungen gewählt werden, die dem Abflussgeschehen in den Grundwasserleitern optimal angepasst sind, so dass bei der Förderung nur Grundwässer mit ähnlichen Druckhöhen und Lösungsinhalten genutzt werden.
    Description: Abstract: The function of the aquifers, that has been described in part 1 (Herreıe 2001), are explained together with their groundwaters in part 2. According to the altitude and the tectonical circumstances the subsurface runoffs feed different receiving channels. It can be shown, that the subsurface runoffs of the deeper aquifers of the area (Rehberg-, Trifels-, Stauf-layers) mostly feed the receiving channels at the „Saarpfälzische Moorniederung”. The well-constructions design should be choosed according to the hydrogeological position. The constructions should be suited to the runoff of the aquifers, so only groundwaters with similar pressure heights and solution contents are used at the production. The groundwater mining in the different subsurface catchment areas should be limited according to the groundwater recharge in the deep aquifers of 5 I/(s - km?) in the NW-part and 6 li(s - km?) in the SE-part of the area.
    Description: 1. Einleitung 2, Klima 3. Oberirdische Gewässer 4. Grundwasser 4.1. Grundwasserstockwerke und ihre Quellen 4.2. Lösungsinhalte der Grundwässer, Grundwassertemperaturen 4.3. Vergleich der Niedrigwasserabflüsse am 05.08.1999, Hinweise zum unterirdischen Abflussgeschehen und zur Grundwasserneubildung 4.4. Spezifische Brunnenergiebigkeiten, Neigungen der Grundwasseroberflächen und -druckflächen, Hinweise zu den unterirdischen Wasserscheiden g, Wasserversorgungsanlagen, Hinweise zum Brunnenbau Schriften
    Description: research
    Keywords: ddc:551.49
    Language: German
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  • 50
    Publication Date: 2022-08-30
    Description: An zwei Kernbohrungen wurden der Sandgehalt und die Mikrofauna von Sedimenten im Übergangsbereich Oberer Rupelton [= Rosenberg-Subformation]/ Schleichsand“ [= Stadecken-Formation] untersucht. Als Abgrenzungskriterium zwischen den beiden stratigraphischen Einheiten kann im Ablagerungsraum Mainzer Becken neben dem schubweisen Einsetzen von glimmerführenden, feinsandigen Mergeln auch das erstmalige Auftreten von allochthonen kretazischen bis paläogenen Foraminiferen herangezogen werden. Etwa gleichzeitig, oder nur wenig zeitversetzt, erscheinen die brackisch-marinen bis brackischen Östracoden-Taxa Hemicyprideis helvetica (LIENENKLAUS 1895), Cytheridea sandbergeri KAMMERER 1989 und Cytheromorpha zinndorfi (LIENENKLAUS 1905), die im Oberen Rupelton [= Rosenberg- Subformation] fehlen.
    Description: Abstract: Core samples of two drillings penetrating the boundary Upper Rupelian Clay [= Rosenberg-Subformation]/„Schleichsand” [= Stadecken-Formation] were investigated for their content of sand and their microfauna. Criteria to define the boundary between both stratigraphical units in the Mainz Basin (Tertiary) are intermittently commencing supplies of micaceous, fine-sandy marls and first findings of allochthonous foraminifera of cretaceous and paleogene age. Nearly at the same time the brackish-marine to brackish ostracods Hemicyprideis helvetica (LIENENKLAUS 1895), Cytheridea sandbergeri KAMMERER 1989 and Cytheromorpha zinndorfi (LIENENKLAUS 1905) appear, which are absent in the underlying Upper Rupelian Clay [= Rosenberg-Subformation].
    Description: research
    Keywords: ddc:562
    Language: German
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  • 51
    Publication Date: 2022-09-16
    Description: Der erste bestimmbare Tetrapode des Oberrotliegenden ein kleinwüchsiger Dissorophide (Labyrinthodontia, Amphibia) wird mit seinem Schädeldach und disartikulierten Elementen des Gliedmaßenskelettes beschrieben. Abweichend von den bekannten Dissorophidae besitzt er ein wahrscheinlich unverknöchertes Quadratum und eine kräftige, teilweise radiale Schädelskulptur. Auch die Existenz eines aus kleinen Partikeln bestehenden Knochenmosaiks oberhalb des Auges (,,‚Sklerotikalpflaster‘‘), die mediale Begrenzung des Ohrschlitzes und die Form des Ilium sind ungewöhnlich für die Dissorophidae. Von den verschiedenen, bei Dissorophiden vorkommenden Merkmalen sind hervorzuheben: die abgeflachten und breit zugerundeten Zahnspitzen und die Existenz eines ‚‚nasal flange‘ auf Nasale und Praefrontale.
    Description: Abstract: The first determinable tetrapod from the upper Rotliegendes, a small dissorophid (Amphibia, Labyrinthodontia), is described. Only the skull roof and disarticulated limb bones are preserved. Several features distinguish this species from known dissorophids. The quadrate appears to be unossified and the sculpturing of the skull roof is more pronounced and has a partially radial pattern. Unusual for dissorophids are a mosaic of small bony particles in the eye lid, the pattern of the medial rim of the otic notch and the shape of the ilium. Among the common characteristics of dissorophids are the laterally compressed monocuspid tooth crowns and a nasal flange projecting from undersurface of nasal and prefrontal.
    Description: research
    Keywords: ddc:567
    Language: German
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  • 52
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    In:  SUB Göttingen
    Publication Date: 2022-06-17
    Description: Die erste Ausgabe der Geowissenschaftlichen Mitteilungen vom 1. Quartal 2000 enthält die Themenblöcke: GEOaktiv (Praxis und Beruf), Geonova (Wissenschaft und Forschung), Geolobby (Gesellschaften, Verbände, Institutionen), Georeport, Geokalender.
    Description: journal
    Description: DFG, SUB Göttingen
    Keywords: ddc:550
    Language: German
    Type: doc-type:book
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  • 53
    Publication Date: 2022-07-22
    Description: Der Buntsandstein der Pfälzer Mulde stellt einen der bedeutenden Trinkwassergewinnungsräume in Rheinland-Pfalz dar. Das Grundwasser wurde in den letzten Jahrzehnten in zunehmend größeren Tiefen erschlossen. Die Brunnenbauwerke erreichen Tiefen bis ca. 350 m. Die in den Tiefbrunnen durchgeführten Pumpversuche dienten zunächst der Ermittlung von Brunnen-spezifischen Ergiebigkeiten. Ergebnisse von Beobachtungen an flachen Grundwassermessstellen wurden auch hinsichtlich der vertikalen geohydraulischen Gliederung der Schichtenfolgen interpretiert. Es werden zwei Standorte vorgestellt, an denen Grundwasser des Buntsandstein durch Tiefbrunnen erschlossen wird. Die Beobachtungen und Ergebnisse durchgeführter Pumpversuche werden kurz dargelegt. Anhand eines Konzeptmodells, das hinsichtlich Geometrie und hydraulischer Randbedingungen als stark vereinfachter, aber realitätsnaher Beispielbereich für den Buntsandstein der Pfälzer Mulde angesehen werden kann, wurden die in flachen Grundwassermessstellen theoretisch zu erwartenden Reaktionen bei Pumpversuchen in Tiefbrunnen modellgestützt berechnet. Die Umsetzung erfolgte mit einem finite- Differenzen-Modell. In verschiedenen Rechenläufen wurden die Kenngrößen Durchlässigkeit und Speicherkoeffizient systematisch verändert. Aus den Ergebnissen lassen sich Mindestanforderungen an die Dauer und die Förderraten ableiten, um Informationen über das hydraulische System zu gewinnen. Die Modellergebnisse weisen ferner darauf hin, dass die Beobachtungsergebnisse bei den üblicherweise eingesetzten einfachen Messstellenkonfigurationen nicht geeignet sind, Rückschlüsse auf die vertikale Strukturierung des erschlossenen Grundwasserleitersystems zu ziehen.
    Description: Abstract: The Bunter of the Palatinate syncline is one of the important groundwater reservoiresin Rheinland-Pfalz. In the last decades the groundwater has been exploited in increasingly greater depth. Wells reach to about 350 m below surface. Pumping tests in deep wells have been primary realised to derive from productivity parameters. But test results have also been interpreted in terms of the vertical hydraulic structure of the Bunter succession. Two locations characteristic of deep wells will be presented. A short summary is given of the observations und the results of the performed pumping tests. A conceptual model has been created which is thought to be representative of parts of the Palatine Bunter in terms of hydrogeology and geohydraulics. On this base a three-dimensional finite-difference groundwater model was used to calculate the theoretically expected reaction of pumping tests for well-neighboured shallow observation wells. Several runs with systematically variations of conductivity and storage coefficient were done. The results give an idea about the minimum duration and necessary pumping rates to get informations about the hydraulic system. AdditionalIy the model results point out that the examinated observation configuration is not qualified to allow interpretations of the vertical aquifer structure.
    Description: 1. Einleitung 2. Zielsetzung und Vorgehensweise 3. Fallbeispiele 4. Konzeptmodell 4.1. Geohydraulische Kenngrößen 4.2. Modellanwendung 4.3. Ergebnisse 5. Diskussion Schriften
    Description: research
    Keywords: ddc:551.49
    Language: German
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  • 54
    Publication Date: 2022-07-25
    Description: research
    Keywords: ddc:562
    Language: German
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  • 55
    Publication Date: 2022-07-25
    Description: research
    Keywords: ddc:554.3
    Language: German
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  • 56
    Publication Date: 2022-12-22
    Description: Die oberrotliegenden rhyolithischen Tuffe der Prims-Mulde werden als Ignimbrite interpretiert. Sie sind maximal 110 m mächtig, gliedern sich durch wenige air-fall-Tuffe in mehrere Einheiten und können auf beiden Flanken der Prims-Mulde bis zu ca. 13 km weit verfolgt werden. Abgeplattete Bimse, Phänokristalle und zahlreiche Xenolithe treten in einer rötlichen, gering verschweißten Matrix auf. Die nicht dem Rotliegenden entstammenden Xenolithe, ihre Verteilung und die Ausrichtung von Bimslängsachsen weisen auf ein Liefergebiet für die pyroklastischen Ströme im Hunsrück hin. Gleichartig ausgebildete pyroklastische Ströme treten im Rotliegenden des Wittlicher Troges auf. Beide Vorkommen werden auf den im Hunsrück gelegenen, in devonische Gesteine eingebetteten Veldenzer Rhyolithschlot bezogen, der eine initiale Ignimbrit- Phase aufwies und wahrscheinlich den Förderort für die Vorkommen in den beiden Rotliegendtrögen darstellt.
    Description: Abstract: Rhyolithic tuffs within the Prims syncline of the Permocarboniferous late Hercynian intermontane Saar-Nahe trough, SW Germany, are interpreted as pyroclastic flow deposits. They are highly altered, weakly welded, and separated by thin air-fall tuffs. Their regional extent, petrography and xenolith content is described. The Devonian provenance of the xenoliths, their distribution, and the Orientation of the flattened pumice fragments all point to the Hunsrück north of the Saar-Nahe trough as the area the pyroclastic flows came from. The pyroclastic flows and similar flows in the next trough to the northwest, the Wittlich trough, are related to the Veldenz rhyolite in the Hunsrück which contains an initial ignimbrite phase and is considered to represent the feeder for these pyroclastic flows.
    Description: 1. Einleitung 2. Geologische Situation 3. Die Ignimbritfolge 3.1. Verbreitung, Volumen, Paläogeographie 3.2. Ausbildung der Ignimbrite 3.3. Abfolge der Ignimbrite 3.4. Beschreibung der Profile 3.5. Petrographie und Chemie 3.5.1. Ignimbrit-Typ Eisen 3.5.2. Ignimbrit-Typ Lauxwald 4. Die Xenolithe der Ignimbritfolge 4.1. Grünliche, grobkörnige Sandsteine 4.2. Feinsandsteine, Silt- und Tonsteine 4.3. Quarzite 4.4. Phyllite . 4.5. Chloritschiefer 5. Gesteine aus dem Rotliegenden und Unterdevon 6. Die Herkunft der Ignimbrite Schriften
    Description: research
    Keywords: ddc:554.3 ; Saar-Nahe-Becken ; Rotliegend ; Ignimbrite
    Language: German
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  • 57
    Publication Date: 2023-01-05
    Description: Nachdem sich Herzog Georg von Sachsen mit den Problemen des Bergbaus auf dem Aldenberg und Geising auseinandergesetzt hatte, erlies er am 11. November 1489 eine Ordnung für die dortigen Bergwerke. In den acht Artikeln dieser Ordnung wurden die Entlohnung der Bergleute sowie die Pflichten der Hutleute, Mühlmeister, Schmelzer und die Strafen bei Zuwiderhandlung festgelegt. Weiterhin wurde eine Vereidigung der Hutleute, Mühlenmeister und Schmelzer befohlen.
    Description: source
    Keywords: Herzog Georg von Sachsen ; Herzog Albrecht von Sachsen ; Hans von Bärenstein zu Ottendorf ; Altenberg ; Geising ; Zinnbergbau ; Sachsen ; Bergordnung
    Language: German
    Type: doc-type:book , updatedVersion
    Format: 6
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  • 58
    Publication Date: 2023-01-02
    Description: Diese Bergordnung wurde am 26. Juli 1449 für die Bergwerke in Schwaz von Herzog Siegmund von Österreich, Steiermark und Kärnten sowie Herr zu Krain und Pfirt, Graf zu Tirol und Kyburg, Landgraf zu Elsaß und Markgraf zu Burgau erlassen. Grundlage war ein 38 Paragrafen umfassendes Gutachten das von Herzog Siegmund mit einer zwölf Paragrafen umfassenden Bestätigung als Bergordnung in Kraft gesetzt wurde. Erklärt wurden das Gerichtswesen, die Holzrechte, die Entlohnung und Versorgung der im Bergbau Beschäftigten sowie die Rechte und Pflichten der Markscheider.
    Description: source
    Keywords: Herzog Siegmund von Österreich ; Österreich ; Steiermark ; Kärnten ; Tirol ; Elsaß ; Gossensaß ; Meran ; Schwaz ; Freundsberg, Burg ; Arlberg ; Brenner ; Silberbergbau ; Bergordnung
    Language: German
    Type: doc-type:book , updatedVersion
    Format: 13
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  • 59
    Publication Date: 2023-01-12
    Description: Transient magnetic reconnection plays an important role in energetic particle acceleration in planetary magnetospheres. Jupiter's magnetosphere provides a unique natural laboratory to study processes of energy transport and transformation. Strong electric fields in spatially confined structures such as plasmoids can be responsible for ion acceleration to high energies. In this study we focus on the effectiveness of ion energization and acceleration in plasmoids. Therefore, we present a statistical study of plasmoid structures in the predawn magnetotail, which were identified in the magnetometer data of the Juno spacecraft from 2016 to 2018. We additionally use the energetic particle observations from the Jupiter Energetic Particle Detector Instrument which discriminates between different ion species. We are particularly interested in the analysis of the acceleration and energization of oxygen, sulfur, helium, and hydrogen ions. We investigate how the event properties, such as the radial distance and the local time of the observed plasmoids in the magnetotail, affect the ion intensities close to the current sheet center. Furthermore, we analyze if ion acceleration is influenced by magnetic field turbulence inside the plasmoids. We find significant heavy ion acceleration in plasmoids close to the current sheet center which is in line with the previous statistical results based on Galileo observations conducted by Kronberg et al. (2019, https://doi.org/10.1029/2019JA026553). The observed effectiveness of the acceleration is dependent on the position of Juno in the magnetotail during the plasmoid event observation. Our results show no correlation between magnetic field turbulence and nonadiabatic acceleration for heavy ions during plasmoids.
    Description: Key Points: Intensity of heavy ions is strongly increased during plasmoids close to the current sheet center. Significant increase of heavy ion intensities is observed in plasmoids with larger wave power. Acceleration of heavy and light ions in plasmoids due to resonant interaction with the magnetic field fluctuations could not be observed.
    Description: Volkswagen Foundation (VolkswagenStiftung) http://dx.doi.org/10.13039/501100001663
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: NASA
    Description: https://pds-ppi.igpp.ucla.edu/
    Keywords: ddc:523 ; plasmoids ; Juno ; JEDI ; ion acceleration
    Language: English
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  • 60
    Publication Date: 2023-01-12
    Description: Hydrological extreme events are generated by different sequences of hydrometeorological drivers, the importance of which may vary within the sample of drought events. Here, we investigate how the importance of different hydrometeorological driver sequences varies by event magnitude using a large sample of catchments in Europe. To do so, we develop an automated classification scheme for streamflow drought events. The classification scheme standardizes a previous qualitative drought typology and assigns events to one of eight drought event types—each characterized by a set of single or compounding drivers—using information about seasonality, precipitation deficits, and snow availability. The objective event classification reveals how drought drivers vary not just in space and by season, but also with event magnitude. Specifically, we show that (a) rainfall deficit droughts and cold snow season droughts are the dominant drought event type in Western Europe and Eastern and Northern Europe, respectively; (b) rainfall deficit and cold snow season droughts are important from autumn to spring while snowmelt and wet‐to‐dry season droughts are important in summer; and (c) moderate droughts are mainly driven by rainfall deficits while severe events are mainly driven by snowmelt deficits in colder climates and by streamflow deficits transitioning from the wet to the dry season in warmer climates. These differences in sequences of drought generation mechanisms for severe and moderate events suggest that future changes in hydrometeorological drivers may affect moderate and severe events differently.
    Description: Key Points: We develop a standardized and objective classification scheme for streamflow droughts using hydroclimatic information. The most severe drought events are governed by other processes than moderate events. Moderate droughts are dominated by rainfall deficits and severe droughts by snowmelt deficits or prolonged rainfall deficit droughts.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: EC/H2020/PRIORITY 'Excellent science'/H2020 European Research Council http://dx.doi.org/10.13039/100010663
    Description: https://www.bafg.de/GRDC/EN/02_srvcs/21_tmsrs/riverdischarge_node.html
    Description: https://doi.pangaea.de/10.1594/PANGAEA.887470
    Description: https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-era5-land?tab=overview
    Description: http://www.hydroshare.org/resource/77114d4dfdfd4dd39e0e1d99165f27b3
    Keywords: ddc:551.6 ; drought types ; drought generation ; extremes ; typology ; classification ; streamflow
    Language: English
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  • 61
    Publication Date: 2023-01-12
    Description: Harmonic Earth tide components in well water levels have been used to estimate hydraulic and geomechanical subsurface properties. However, the robustness of various methods based on analytical solutions has not been established. First, we review the theory and examine the latest analytical solution used to relate well water levels to Earth tides. Second, we develop and verify a novel numerical model coupling hydraulics and geomechanics to Earth tide strains. Third, we assess subsurface conditions over depth for a range of realistic properties. Fourth, we simulate the well water level response to Earth tide strains within a 2D poroelastic layered aquifer system confined by a 100 m thick aquitard. We find that the non‐linear inversion of analytical solutions to match two observations (amplitudes and phases) to multiple unknown parameters is sensible to the initial guess. We reveal that undrained, confined conditions are necessary for the analytical solution to be valid. This occurs for the dominant M2 frequency at depths 〉50 m and requires specific storage at constant strain of Sϵ ≥ 10−6 m−1, hydraulic conductivity of the aquitard of kl ≤ 5 ⋅ 10−5 ms−1 and aquifer of ka ≥ 10−4 ms−1. We further illustrate that the analytical solution is valid in unconsolidated systems, whereas consolidated systems require additional consideration of the Biot modulus. Overall, a priori knowledge of the subsurface system supports interpretation of the groundwater response. Our results improve understanding of the effect of Earth tides on groundwater systems and its interpretation for subsurface properties.
    Description: Plain Language Summary: Earth tide induced strains in the subsurface lead to well water level fluctuations in groundwater monitoring wells. This groundwater response has been interpreted with analytical solutions to estimate aquifer properties. However, analytical solutions are based on simplified assumptions whose accuracy have not yet been tested. We develop a new approach to simulate the influence of Earth tides on groundwater based on fundamental physical principles. We simulate realistic conditions and compare our results to those from analytical solution to determine the hydraulic and subsurface conditions under which simplified interpretations are valid. Our results improve understanding of the effects of Earth tides on groundwater systems and interpretation of subsurface properties from well water levels.
    Description: Key Points: We develop and verify a numerical model for the well water level response to Earth tides. Subsurface property estimation requires undrained and confined conditions occurring at depths 〉50 m. Amplitudes and phases from numerical and analytical solutions systematically diverge reflecting theory simplifications.
    Description: German Research Council
    Description: https://doi.org/10.5281/zenodo.6950492
    Keywords: ddc:551 ; tidal subsurface analysis ; numerical modeling ; Earth tides
    Language: English
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  • 62
    facet.materialart.
    Unknown
    ARGE GMIT, Bonn
    Publication Date: 2023-01-09
    Description: Die Ausgabe der Geowissenschaftlichen Mitteilungen vom September 2022 enthält die Themenblöcke: GEOfokus: Klimagerechte Geowissenschaften Glaubwürdigkeit und Vorbild, GEOaktiv (Wirtschaft, Beruf, Forschung und Lehre), GEOlobby (Gesellschaften, Verbände, Institutionen), GEOreport (Geowissenschaftliche Öffentlichkeitsarbeit, Tagungsberichte, Ausstellungen, Exkursionen, Publikationen), GEOszene (Würdigungen, Nachrufe).
    Description: DFG, SUB Göttingen
    Description: journal
    Keywords: ddc:550 ; GMIT
    Language: German
    Type: doc-type:book , publishedVersion
    Format: 132
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  • 63
    Publication Date: 2023-01-10
    Description: manual
    Keywords: ddc:631.4 ; Rheinland-Pfalz ; Hessen ; Bodenschutz ; Raumplanung
    Language: German
    Type: doc-type:book , publishedVersion
    Format: 68
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  • 64
    Publication Date: 2023-01-15
    Description: A Guinier camera equipped with an imaging plate is used to investigate and eliminate the sources of instrumental errors affecting the quality of the obtained scanned Guinier data. A program with a graphical user interface is presented which converts the data of the scanned images into different standard file formats for powder X‐ray patterns containing intensities, their standard deviations and the diffraction angles. The program also allows for manual and automatic correction of the 2gθ scale against a known reference material. It is shown using LaB6 that the exported X‐ray diffraction patterns provide a 2gθ scale reproducible enough to allow for averaging diffractograms obtained from different exposures of the imaging plate for the same sample. As shown on a mixture of NaCl and sodalite, the quality of the produced data is sufficient for Rietveld refinement. The software including source code is made available under a free software license.
    Description: A program for the digitization of Guinier powder diffraction images is described, which works with images from both optical and laser scanners. Thus, processing of data from storage‐phosphor‐based imaging plates and Ag‐based photographic films is possible.
    Keywords: ddc:548 ; IPreader software ; Guinier cameras ; imaging plates (IPs) ; diffraction pattern conversion into data columns ; powder X‐ray diffraction ; data processing ; Guinier method
    Language: English
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  • 65
    Publication Date: 2023-01-15
    Description: Key knowledge about planetary composition can be recovered from the study of thermal infrared spectral range datasets. This range has a huge diagnostic potential because it contains diagnostic absorptions from a planetary surface and atmosphere. The main goal of this study is to process and interpret the dataset from the Thermal Infrared channel (TIRVIM) which is part of the Atmospheric Chemistry Suite of the ExoMars2016 Trace Gas Orbiter mission to find and characterize dust and water ice clouds in the atmosphere. The method employed here is based on the application of principal component analysis and target transformation techniques to extract the independent variable components present in the analyzed dataset. Spectral shapes of both atmospheric dust and water ice aerosols have been recovered from the analysis of TIRVIM data. The comparison between our results with those previously obtained on Thermal Emission Spectrometer (TES) data and with previous analysis on TIRVIM data, validates the methodology here applied, showing that it allows to correctly recover the atmospheric spectral endmembers present in the TIRVIM data. Moreover, comparison with atmospheric retrievals on PFS, TES and IRIS data, allowed us to assess the temporal stability and homogeneity of dust and water ice components in the Martian atmosphere over a time period of almost 50 years.
    Description: Plain Language Summary: The analysis of thermal infrared datasets from planetary bodies is of key importance for the understanding of a planet's climate evolution and history: it contains valuable information about composition, temperature and state of the atmosphere. Moreover, surface properties and the surface‐atmosphere interaction can be studied. Here we investigated new thermal infrared data from the Thermal Infrared channel instrument of the ExoMars Trace Gas Orbiter with the main goal of carefully identifying Martian atmospheric dust and water ice clouds components. A methodology based on principal component and target transformation factor analysis techniques has been applied. Based on our results, this methodology can correctly recover both atmospheric dust and water ice aerosols spectral shapes and their abundances in the Martian atmosphere.
    Description: Key Points: First successful application of principal components and target transformation techniques to high‐resolution Thermal Infrared channel (TIRVIM) data. Spectral shapes of both atmospheric dust and water ice clouds are recognized and recovered. TIRVIM data are successfully modeled through a linear combination of the recovered water ice and dust end‐members.
    Description: Roscosmos and ESA
    Description: https://doi.org/10.5281/zenodo.7032738
    Keywords: ddc:523 ; Martian atmosphere ; TIRVIM data
    Language: English
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  • 66
    Publication Date: 2023-01-15
    Description: A limited number of gauging stations, especially for nested catchments, hampers a process understanding of the interaction between streamflow, groundwater and water usage during drought. Non‐commercial measurement devices can help overcome this lack of monitoring, but they need to be thoroughly tested. The Dreisam River in the South‐West of Germany was affected by several hydrological drought events from 2015 to 2020 during which parts of the main stream and tributaries fell dry. Therefore it provided a useful case study area for a flexible longitudinal water quality and quantity monitoring network. Among other measurements the setup employs an image‐based method with QR codes as fiducial marker. In order to assess under which conditions the QR‐code based water level loggers (WLL) deliver data according to scientific standards, we compared its performance to conventional capacitive based WLL. The results from 20 monitoring stations reveal that the riverbed was dry for 〉50% at several locations and even for 〉70% at most severely affected locations during July and August 2020, with the north western parts of the catchment being especially concerned. Highly variable longitudinal drying patterns of the stream reaches emerged from the monitoring. The image‐based method was found valuable for identification and validation of zero level occurrences. Nevertheless, a simple image processing approach (based on an automatic thresholding algorithm) did not compensate for errors due to natural conditions and technical setup. Our findings highlight that the complexity of measurement environments is a major challenge when working with image‐based methods.
    Description: We monitored zero water levels in a meso‐scale catchment with temperate climate by means of image‐based and conventional water level logging techniques. A detailed analysis of the longitudinal drying patterns enables a discussion about hydrological connectivity and the processes influencing the drying.
    Description: Badenova Fund For Innovation
    Description: https://doi.org/10.6094/UNIFR/228702
    Keywords: ddc:551.48 ; hydrological drought ; innovative sensors ; longitudinal connectivity ; stream reaches ; streamflow intermittency ; zero flow
    Language: English
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  • 67
    Publication Date: 2023-01-15
    Description: The dynamics of the Alps and surrounding regions is still not completely understood, partly because of a non‐unique interpretation of its upper‐mantle architecture. In particular, it is unclear if interpreted slabs are consistent with the observed surface deformation and topography. We derive three end‐member scenarios of lithospheric thickness and slab geometries by clustering available shear‐wave tomography models into a statistical ensemble. We use these scenarios as input for geodynamic simulations and compare modeled topography, surface velocities and mantle flow to observations. We found that a slab detached beneath the Alps, but attached beneath the Northern Apennines captures first‐order patterns in topography and vertical surface velocities and can provide a causative explanation for the observed seismicity.
    Description: Plain Language Summary: Present‐day surface deformation, including earthquakes, plate motion, and mass (re)distribution, results from processes operating at the surface and in the interior of the Earth. Understanding these processes and their coupling is of utmost importance in light of the hazard they pose to society. The Alps provide an excellent natural laboratory to understand such coupling. Here, we use seismic tomography models to constrain its upper‐mantle architecture. We further use these models to quantify forces originating from the resolved architecture and their effects on the present‐day surface deformation. The models can reproduce first‐order patterns in the observed topography and vertical surface motions. We found a causative correlation between the presence of a shallow slab attached to the overlying lithosphere in the Northern Apennines and the seismicity in the region. Our results allow us to better understand the transfer of internal forces to the surface, thereby helping to quantify the present‐day mechanical setup of the area.
    Description: Key Points: Statistical ensemble of S‐wave tomography models is used to infer the Lithosphere‐Asthenosphere Boundary configuration and slab geometries in the Alps. The 3‐D upper‐mantle architecture from the statistics reproduce first‐order patterns in observed topography and Global Navigation Satellite Systems vertical velocities. A shallow/attached slab in the Northern Apennines is consistent with the mantle depth seismicity observed in this region.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5880/GFZ.4.5.2019.004
    Description: https://gfzpublic.gfz-potsdam.de/pubman/item/item_238001
    Description: http://ds.iris.edu/ds/products/emc-earthmodels/
    Description: https://doi.org/10.5281/zenodo.7071571
    Description: https://doi.org/10.5281/zenodo.6538257
    Keywords: ddc:551.1 ; Alps ; Apennines ; lithospheric architecture ; slabs ; seismicity
    Language: English
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  • 68
    Publication Date: 2023-01-15
    Description: Physiological sensitivity of cold‐water corals to ocean change is far less understood than of tropical corals and very little is known about the impacts of ocean acidification and warming on degradative processes of dead coral framework. In a 13‐month laboratory experiment, we examined the interactive effects of gradually increasing temperature and pCO2 levels on survival, growth, and respiration of two prominent color morphotypes (colormorphs) of the framework‐forming cold‐water coral Lophelia pertusa, as well as bioerosion and dissolution of dead framework. Calcification rates tended to increase with warming, showing temperature optima at ~ 14°C (white colormorph) and 10–12°C (orange colormorph) and decreased with increasing pCO2. Net dissolution occurred at aragonite undersaturation (ΩAr 〈 1) at ~ 1000 μatm pCO2. Under combined warming and acidification, the negative effects of acidification on growth were initially mitigated, but at ~ 1600 μatm dissolution prevailed. Respiration rates increased with warming, more strongly in orange corals, while acidification slightly suppressed respiration. Calcification and respiration rates as well as polyp mortality were consistently higher in orange corals. Mortality increased considerably at 14–15°C in both colormorphs. Bioerosion/dissolution of dead framework was not affected by warming alone but was significantly enhanced by acidification. While live corals may cope with intermediate levels of elevated pCO2 and temperature, long‐term impacts beyond levels projected for the end of this century will likely lead to skeletal dissolution and increased mortality. Our findings further suggest that acidification causes accelerated degradation of dead framework even at aragonite saturated conditions, which will eventually compromise the structural integrity of cold‐water coral reefs.
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Marine Research in Ireland
    Description: French National Research Agency http://dx.doi.org/10.13039/501100001665
    Keywords: ddc:577.7 ; cold-water corals ; ocean change ; laboratory experiments ; framwork dissolution ; bioerosion
    Language: English
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  • 69
    facet.materialart.
    Unknown
    Publication Date: 2023-01-16
    Description: Die Rehbergschichten treten im linksrheinischen Buntsandstein zwischen Trifels- und Karlstalschichten auf. Es ist ein Wechsel von Felsbänken und Dünnschichten, wobei die Felsbänke die petrographischen Merkmale der Trifelsschichten, die Dünnschichten die sedimentologischen Merkmale der Unteren Karlstalschichten enthalten. Die Untergrenze der Rehbergschichten bildet die tiefste Lage von Dünnschichten (Scheidter Niveau). Die Obergrenze der Rehbergschichten bildet die stratigraphisch höchste Felsbank mit den petrographischen Merkmalen der Trifelsschichten oder des smi. Stratigraphisch markante Felsbänke bestehen innerhalb der Rehbergschichten nicht, eine stratigraphische und kartographische Unterteilung der Rehbergschichten ist nicht möglich. Genetisch werden die Rehbergschichten als Wechsel zwischen äolisch und fluviatil sedimentierten Schichten verstanden. Die Rehbergschichten tragen in der Landschaft weite Verebnungsflächen, wobei Verebnungen und Hangverflachungen in verschiedenen Niveaus übereinander vorkommen.
    Description: Abstract: The Rehberg sandstone is found in the Southwest German and Alsatian Buntsandstein between Trifels and Karlstal sandstones. Banquettes and lamelliform layers relieve one another, the banquettes containing the petrographic characteristics of the Tifels sandstone and the fine bedded layers the sedimentological characteristics of the lower Karlstal layers. The lower boundary of the Rehberg sandstone forms the lowest deposit of the fine bedded layers (Scheidter Niveau). The upper boundary of the Rehberg sandstone forms the stratigraphically highest banquette with the petrographic characteristics of the Trifels sandstone or the sny. Within the Rehberg sandstone stratigraphically noticeable banquettes do not exist. A Stratigraphie and cartographic division of the Rehberg sandstone is not possible. As far as genesis is concerned, the Rehberg sandstone are regarded as an alternation of eolian and fluviatile sedimented layers. The morphological structure of the landscape formed by the Rehberg sandstone shows wide peneplanations which occur at different levels.
    Description: research
    Keywords: ddc:554.3 ; Buntsandstein ; Pfalz ; Stratigraphie
    Language: German
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  • 70
    Publication Date: 2023-01-17
    Description: In this study, a spectral model for convective transport is coupled to a thermal population model on a two‐dimensional horizontal “microgrid,” covering the typical gridbox size of general circulation models. The goal is to explore new ways of representing impacts of spatial organization in cumulus cloud fields. The thermals are considered the smallest building block of convection, with thermal life cycle and movement represented through binomial functions. Thermals interact through two simple rules, reflecting pulsating growth and environmental deformation. Long‐lived thermal clusters thus form on the microgrid, exhibiting scale growth and spacing that represent simple forms of spatial organization and memory. Size distributions of cluster number are diagnosed from the microgrid through an online clustering algorithm, and provided as input to a spectral multiplume eddy‐diffusivity mass flux scheme. This yields a decentralized transport system, in that the thermal clusters acting as independent but interacting nodes that carry information about spatial structure. The main objectives of this study are (a) to seek proof of concept of this approach, and (b) to gain insight into impacts of spatial organization on convective transport. Single‐column model experiments demonstrate satisfactory skill in reproducing two observed cases of continental shallow convection. Metrics expressing self‐organization and spatial organization match well with large‐eddy simulation results. We find that in this coupled system, spatial organization impacts convective transport primarily through the scale break in the size distribution of cluster number. The rooting of saturated plumes in the subcloud mixed layer plays a key role in this process.
    Description: Plain Language Summary: Recent studies have emphasized the importance of the spatial structure of convective cloud fields in Earth's climate, yet this phenomenon is not yet represented well in Earth System Models (ESMs). This study explores a new way to achieve this goal, by considering spatial organization at the scale of small bubbles of rising air called thermals that together make up convective clouds. Populations of interacting thermals are modeled in a computationally efficient way on a small two‐dimensional grid. This microgrid is then coupled to a convection scheme, which stands for the set of equations used to statistically represent the impact of convective transport at scales that remain unresolved in ESMs. The coupling makes the scheme decentralized, in that the transport becomes dependent on a population of longer‐lived convective structures that slowly develop and evolve on the microgrid. The new scheme is tested for observed conditions at a meteorological site in the Southern Great Plains area of the United States, making use of a combination of high‐resolution simulations and measurements to evaluate performance. Apart from proof of concept for the new modeling approach, the results provide new insights into how the spatial structure of convective cloud populations can affect its vertical transport.
    Description: Key Points: A multiplume spectral convection scheme is coupled to a binomial thermal population model on a horizontal microgrid. Observed diurnal cycles of continental shallow convection are reproduced, including good agreement on scale growth and spatial organization. Spatial organization impacts convective transport through the scale break in the cluster number density, with a key role played by plume rooting.
    Description: U.S. Department of Energy http://dx.doi.org/10.13039/100000015
    Description: https://doi.org/10.5281/zenodo.6044338
    Keywords: ddc:551.5 ; convective parameterization ; spatial organization ; population dynamics ; thermals ; microgrid modeling ; shallow cumulus
    Language: English
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  • 71
    Publication Date: 2023-01-17
    Description: It is generally agreed that the resolution of a regular quadrilateral mesh is the side length of quadrilateral cells. There is less agreement on the resolution of triangular meshes, exacerbated by the fact that the numbers of edges or cells on triangular meshes are approximately three or two times larger than that of vertices. However, the geometrical resolution of triangular meshes, that is, maximum wavenumbers or smallest wavelengths that can be represented on such meshes, is a well defined quantity, known from solid state physics. These wavenumbers are related to a smallest common mesh cell (primitive unit cell), and the set of mesh translations that map it into itself. They do not depend on whether discrete degrees of freedom are placed on vertices, cells or edges. For equilateral triangles the smallest wavelength equals twice the triangle height. Resolutions of quadrilateral and triangular meshes approximately agree if they have the same numbers of vertices.
    Description: Plain Language Summary: Some models used in climate studies are formulated on triangular computational meshes. We discuss how to determine the smallest scales that are resolved on such meshes. They are referred to as a mesh resolution. The notion of mesh resolution is commonly used to relate climate model results simulated on different meshes.
    Description: Key Points: Geometrical resolution of an equilateral triangular mesh is defined by the height of its triangles. Quadrilateral and triangular meshes with the same number of vertices have approximately the same resolution.
    Description: Collaborative Research Centre
    Description: German Research Foundation
    Keywords: ddc:550 ; triangular meshes ; resolved wavenumbers
    Language: English
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  • 72
    Publication Date: 2023-01-17
    Description: In this study, we investigated the phase stability of Al‐free and Al‐bearing superhydrous phase B (shy‐B) up to 55 GPa and 2500 K. In comparison with Al‐free shy‐B, the incorporation of 11.7 wt.% Al2O3 in shy‐B expands the stability by ∼400–800 K at 20–30 GPa. The determined dehydration boundary for Al‐bearing phase D indicates that it could be present even at normal mantle geotherm conditions at 30–40 GPa. Up to 23.8 mol.% Al2O3 can be dissolved into the structures of akimotoite and bridgmanite as a result of the decomposition reactions of Al‐bearing shy‐B and phase D between 20 and 40 GPa. Results of further experiments indicate that δ‐AlOOH is the stable hydrous phase coexisting with Al‐depleted bridgmanite at pressures above 52 GPa. This study shows that the incorporation of Al in dense hydrous magnesium silicates can have a profound impact on our picture of the water cycle in the deep Earth.
    Description: Plain Language Summary: Constraining the deep cycle of water has a tremendous impact on our picture of the current state of the Earth and the evolution of the Earth's interior. Dense hydrous magnesium silicates (DHMSs) are considered potential H2O carriers in the Earth's mantle. However, the DHMSs can only be present at the relatively cold conditions of subduction slabs due their limited thermal stability. We determined the phase stability of Al‐bearing DHMSs at high pressure and temperature (P‐T) conditions. Our results show that the thermal stability of Al‐bearing shy‐B extends by 400–800 K with respect to its Al‐free counterpart at 600–800 km depth. The incorporation of Al also expands the phase stability of phase D and enhances the likelihood of its occurrence at normal mantle conditions at 800–1100 km. In addition, we observe that 23.8 mol.% Al2O3 can be dissolved into the structures of akimotoite and bridgmanite as a result of the decomposition reactions of Al‐bearing shy‐B and phase D between 600 and 100 km depth. Furthermore, δ‐AlOOH is the stable hydrous phase coexisting with Al‐depleted bridgmanite in the MgO‐SiO2‐Al2O3‐H2O system at pressures above 52 GPa and 1500 K.
    Description: Key Points: In comparison with Al‐free shy‐B, the incorporation of 11.7 wt.% Al2O3 in superhydrous phase B (shy‐B) expands the stability by ∼400–800 K at 20–30 GPa. Al‐bearing phase D could be present even at normal mantle geotherm conditions at 30–40 GPa. δ‐AlOOH is the stable hydrous phase coexisting with Al‐depleted bridgmanite at pressures above 52 GPa.
    Description: Center for Molecular Water Science, CMWS
    Description: https://doi.org/10.5281/zenodo.6320835
    Keywords: ddc:549 ; Al‐bearing superhydrous phase B ; phase D ; phase stability ; high pressure and temperature ; deep Earth water cycle
    Language: English
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  • 73
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    Wangari, E. G. ; Mwanake, R. M. ; Kraus, D. ; [et al.]
    Publication Date: 2023-01-17
    Description: Accurate quantification of landscape soil greenhouse gas (GHG) exchange from chamber measurements is challenging due to the high spatial‐temporal variability of fluxes, which results in large uncertainties in upscaled regional and global flux estimates. We quantified landscape‐scale (6 km2 in central Germany) soil/ecosystem respiration (SR/ER‐CO2), methane (CH4), and nitrous oxide (N2O) fluxes at stratified sites with contrasting landscape characteristics using the fast‐box chamber technique. We assessed the influence of land use (forest, arable, and grassland), seasonality (spring, summer, and autumn), soil types, and slope on the fluxes. We also evaluated the number of chamber measurement locations required to estimate landscape fluxes within globally significant uncertainty thresholds. The GHG fluxes were strongly influenced by seasonality and land use rather than soil type and slope. The number of chamber measurement locations required for robust landscape‐scale flux estimates depended on the magnitude of fluxes, which varied with season, land use, and GHG type. Significant N2O‐N flux uncertainties greater than the global mean flux (0.67 kg ha−1 yr−1) occurred if landscape measurements were done at 〈4 and 〈22 chamber locations (per km2) in forest and arable ecosystems, respectively, in summer. For CO2 and CH4 fluxes, uncertainties greater than the global median CO2‐C flux (7,500 kg ha−1 yr−1) and the global mean forest CH4‐C uptake rate (2.81 kg ha−1 yr−1) occurred at 〈2 forest and 〈6 arable chamber locations. This finding suggests that more chamber measurement locations are required to assess landscape‐scale N2O fluxes than CO2 and CH4, based on these GHG‐specific uncertainty thresholds.
    Description: Plain Language Summary: Greenhouse gas emissions are subject to high spatial and temporal variability, leading to large uncertainties in regional and global estimates. We quantified fluxes of soil and ecosystem respiration (SR/ER‐CO2), methane (CH4) and nitrous oxide (N2O) at the landscape scale (6 km2 in central Germany). We determine the number of measurement chambers required to estimate landscape fluxes within globally significant uncertainty thresholds. Our results show a stronger influence of season and land use, as opposed to soil type and topography. The number of chambers required for robust landscape‐wide flux estimates depended on the size of the fluxes, which varied by season, land use and GHG type. An increase in the number of monitoring sites significantly reduced the uncertainties estimation on the whole landscape. Significant uncertainties in N2O fluxes above the global annual mean was found when landscape measurements were made at 〈4 monitoring sites in forests and 〈22 monitoring sites (per km2) in cropland ecosystems during the summer period. For SR/ER‐CO2 fluxes, as few as 〈2 was sufficient in forest ecosystems and under 〈6 in cropland ecosystems. This result implies that in general more monitoring sites are needed to assess landscape‐scale N2O fluxes than for CO2 and CH4 fluxes.
    Description: Key Points: Land use and seasonality rather than soil type and slope strongly influenced soil greenhouse gas (GHG) fluxes at a landscape‐scale. The minimum number of chamber locations required for robust landscape‐scale flux estimates depends on the season, land use, and GHG type. Chamber locations required to reduce uncertainties of landscape flux estimates declined as follows N2O 〉 CO2 〉 CH4.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5281/zenodo.6821111
    Keywords: ddc:631.4 ; soil respiration ; ecosystem respiration ; methane uptake ; nitrous oxide fluxes ; spatial‐temporal variability ; stratfied sampling
    Language: English
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  • 74
    Publication Date: 2023-01-17
    Description: The collision between the Indian and Eurasian plates promotes the southeastward extrusion of the Indochina Peninsula while the internal dynamics of its crustal deformation remain enigmatic. Here, we make use of seismic data from 38 stations and employ the ambient noise tomography to construct a 3‐D crustal shear‐wave velocity (Vs) model beneath the Indochina Peninsula. A low‐Vs anomaly is revealed in the mid‐lower crust of the Shan‐Thai Block and probably corresponds to the southern extension of the crustal flow from SE Tibet. Although the Khorat Plateau behaves as a rigid block, the observed low‐Vs anomalies in the lower crust and also below the Moho indicate that the crust may have been partially modified by mantle‐derived melts. The strike‐slip shearing motions of the Red River Fault may have dominantly developed crustal deformation at its western flank where a low‐Vs anomaly is observed at the upper‐middle crust.
    Description: Plain Language Summary: The Indochina Peninsula was believed to behave as a rigid block where significant southeastward extrusion and clockwise rotation have occurred in response to the collision between the Indian and Eurasian plates. Here, we employ ambient noise data to obtain the shear‐wave velocity (Vs) images and find deformations in the interior of the crust beneath the Indochina Peninsula. A low‐Vs anomaly is observed in the mid‐lower crust of the Shan‐Thai Block and represents the crustal flow from SE Tibet. The crust of the Khorat Plateau, the core of the Indochina Block, has been partially modified by mantle‐derived melts. The strike‐slip shearing motions of the Red River Fault have brought crustal deformation at its southwestern flank characterized as a low‐Vs anomaly in the upper‐middle crust.
    Description: Key Points: A 3‐D crustal shear‐wave velocity (Vs) model was constructed for the Indochina Peninsula from ambient noise tomography. Low‐Vs in the middle‐lower crust of the Shan‐Thai Block may represent the southern extension of the crustal flow from SE Tibet. The crust of the rigid Khorat Plateau has been partially modified by intrusion of mantle‐derived melts.
    Description: National Natural Science Foundation of China http://dx.doi.org/10.13039/501100001809
    Description: the State Key Laboratory of Marine Geology, Tongji University
    Description: Shanghai Sheshan National Geophysical Observatory
    Description: https://doi.org/10.5281/zenodo.5235658
    Keywords: ddc:551.1 ; Indochina Peninsula ; crustal structure ; lower‐crustal flow ; ambient noise tomography
    Language: English
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  • 75
    Publication Date: 2023-01-11
    Description: Diese Bergordnung wurde am 7. Januar 1474 für die Bergwerke in Schwaz von Herzog Siegmund von Österreich erlassen. Mit dem ab 1470 stark ansteigenden Bergbauaktivitäten kam es gleichzeitig zu zahlreichen Missständen bei der Dienstdurchführung der Hutleute sowie zu offensichtlich chaotischen Zuständen bei der Vermessung der Grubenfelder. In 16 Paragrafen wurden deshalb die Rechte der Gruben an ihren Feldern, das ordentliche Vermessen der Grubenfelder und das Verhalten bei Durchschlägen beschrieben sowie die Zuständigkeiten der Hutleute klar benannt. In einem später eingefügten Zusatz wurde das Fällen von Bäumen im gesamten Bergbaubezirk verboten.
    Description: source
    Keywords: Herzog Siegmund von Österreich ; Österreich ; Tirol ; Schwaz ; Freundsberg, Burg ; Schlitters ; Innsbruck ; Silberbergbau ; Bergordnung
    Language: German
    Type: doc-type:book , updatedVersion
    Format: 7
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  • 76
    Publication Date: 2023-01-14
    Description: Climate model simulations typically exhibit a bias, which can be corrected using statistical approaches. In this study, a geostatistical approach for bias correction of daily precipitation at ungauged locations is presented. The method utilizes a double quantile mapping with dry day correction for future periods. The transfer function of the bias correction for the ungauged locations is established using distribution functions estimated by ordinary kriging with anisotropic variograms. The methodology was applied to the daily precipitation simulations of the entire CORDEX‐Africa ensemble for a study region located in the West African Sudanian Savanna. This ensemble consists of 23 regional climate models (RCM) that were run for three different future scenarios (RCP 2.6, RCP 4.5, and RCP 8.5). The evaluation of the approach for a historical 50‐year period (1950–2005) showed that the method can reduce the inherent strong precipitation bias of RCM simulations, thereby reproducing the main climatological features of the observed data. Moreover, the bias correction technique preserves the climate change signal of the uncorrected RCM simulations. However, the ensemble spread is increased due to an overestimation of the rainfall probability of uncorrected RCM simulations. The application of the bias correction method to the future period (2006–2100) revealed that annual precipitation increases for most models in the near (2020–2049) and far future (2070–2099) with a mean increase of up to 165mm⋅a−1 (18%). An analysis of the monthly and daily time series showed a slightly delayed onset and intensification of the rainy season.
    Description: Adapting water management strategies to future precipitation projected by climate models is associated with high uncertainty in sparsely gauged catchments. Kriging was utilized to estimate distribution parameters for ungauged locations in a West African region to perform a bias correction of the CORDEX‐Africa ensemble. The application of the bias correction method revealed higher annual precipitation amounts and an intensifaction of the rainy season but only little change to the onset of the rainy season.
    Description: German Federal Ministry of Education and Research, Bonn (BMBF), West African Science Service Centre on Climate Change and Adapted Land Use (WASCAL)
    Keywords: ddc:551.6 ; bias correction ; climate change ; CORDEX‐Africa ; geostatistical approaches ; precipitation ; quantile mapping ; West Africa
    Language: English
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  • 77
    Publication Date: 2023-01-14
    Description: The Paris Agreement marks a significant milestone in international climate politics. With its adoption, Parties call for non‐ and sub‐state actors to contribute to the global climate agenda and close the emissions gap left by states. Such a facilitative setting embraces non‐state climate action through joint efforts, synergies, and different modes of collaboration. At the same time, non‐state actors have always played a critical and confrontational role in international climate governance. Based on a systematic literature review, we identify and critically assess the role of non‐state climate action in a facilitative post‐Paris climate governance regime. We thereby highlight three constitutive themes, namely different state‐non‐state relations, competing level of ambition, and a variety of knowledge foundations. We substantiate these themes, derived from an inductive analysis of existing literature, with illustrative examples and propose three paradigmatic non‐state actor roles in post‐Paris climate governance on a continuum between compliance and critique. We thereby highlight four particular threats of a facilitative setting, namely substitution of state action, co‐optation, tokenism, and depoliticization. Future research should not limit itself to an effective integration of NSSAs into a facilitative climate regime, but also engage with the merits of contestation. This article is categorized under: Policy and Governance 〉 Multilevel and Transnational Climate Change Governance
    Description: Three constitutive themes—different state‐non‐state relations, levels of ambition, and knowledge foundations—define the multiple roles non‐ and sub‐state actors can occupy in the post‐Paris climate governance regime. Yet, calls for voluntary, collaborative, and synergetic non‐state climate action in a facilitative post‐Paris climate governance setting run the risk to overshadow fundamental tensions when governing climate change.
    Description: Svenska Forskningsrådet Formas http://dx.doi.org/10.13039/501100001862
    Description: Deutsche Forschungsgemeinschaft (DFG)
    Keywords: ddc:341.7 ; climate change governance ; contestation ; environmental politics ; non‐state actors ; Paris Agreement ; transformation
    Language: English
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  • 78
    Publication Date: 2023-01-14
    Description: We theoretically and empirically investigate the investments of water users in a stylized local irrigation system. We model irrigation self‐management as an interdependent interaction of users in an evolutionary game and study the resilience of the irrigation system. The theoretical model implies multiple stable equilibria at different efficiency levels. Users may be trapped in a low level of collective investment or succeed by being locked in a high collective investment level, implying an irrigation system resilient against external shocks. The study seeks to empirically identify such lock‐ins in experimental interactions among Central Asian farmers. Furthermore, we inquire into whether a pre‐play cheap talk opportunity with peer‐monitoring or sanctioning treatments influence the self‐reinforcing dynamic. Our findings revealed several stable states. Among these states, there are both low and high levels of efficiency, which we measure in the size of public good. Communication among users results in higher collective investment levels. However, this does not guarantee the complete elimination of inferior conventions from best‐response play. Penalties crowded out the intrinsic motivation to cooperate as they reduced collective investment in both low‐ and high‐level equilibria. Our findings imply that institutional settings tailored to each community can improve resilience to climate‐driven perturbations in water resources.
    Description: VolkswagenStiftung (Volkswagen Foundation) http://dx.doi.org/10.13039/501100001663
    Description: Federal Ministry for Economic Cooperation (BMZ) http://dx.doi.org/10.13039/501100001663
    Keywords: ddc:333.91 ; Central Asia ; experiment ; multiple equilibria ; resilience ; water management ; Asie centrale ; expérimentation ; équilibres multiples ; résilience ; gestion de l'eau
    Language: English
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  • 79
    Publication Date: 2023-01-14
    Description: Spaceborne impact ionization mass spectrometers, such as the Cosmic Dust Analyzer on board the past Cassini spacecraft or the SUrface Dust Analyzer being built for NASA's upcoming Europa Clipper mission, are of crucial importance for the exploration of icy moons in the Solar System, such as Saturn's moon Enceladus or Jupiter's moon Europa. For the interpretation of data produced by these instruments, analogue experiments on Earth are essential. To date, thousands of laboratory mass spectra have been recorded with an analogue experiment for impact ionization mass spectrometers. Simulation of mass spectra of ice grains in space is achieved by a Laser Induced Liquid Beam Ion Desorption (LILBID) approach. The desorbed cations or anions are analyzed in a time‐of‐flight mass spectrometer. The amount of unstructured raw data is increasingly challenging to sort, process, interpret and compare with data from space. Thus far this has been achieved manually for individual mass spectra because no database containing the recorded reference spectra was available. Here we describe the development of a comprehensive, extendable database containing cation and anion mass spectra from the laboratory LILBID facility. The database is based on a Relational Database Management System with a web server interface and enables filtering of the laboratory data using a wide range of parameters. The mass spectra can be compared not only with data from past and future space missions but also mass spectral data generated by other, terrestrial, techniques. The validated and approved subset of the database is available for general public (https://lilbid-db.planet.fu-berlin.de).
    Description: Plain Language Summary: Thousands of laboratory mass spectra, each with an individual set of experimental parameters, have been recorded so far using a facility situated at Freie Universität Berlin, Germany. The mass spectra help analyze and interpret data returned from spacecraft in the vicinity of icy moons in the Solar System. The unstructured laboratory data is increasingly challenging to sort and compare to the data from space. We developed an extendable database containing the laboratory data. The database is available for general public and allows filtering the stored data for a wide range of experimental parameters and, in turn, significantly improves analysis of data not only from past space missions but also future missions in particular.
    Description: Key Points: We describe the development of a comprehensive spectral database containing laboratory analogue data for spaceborne mass spectrometers. The database is based on a Relational Database Management System with a web interface and accessible for community use. Filtering the laboratory data using a wide range of experimental parameters allows a straightforward analysis of returned flight data.
    Description: EC, Horizon 2020 Framework Programme (H2020) http://dx.doi.org/10.13039/100010661
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5281/zenodo.6863855
    Description: https://sbnarchive.psi.edu/pds3/cassini/cda/COCDA_0007.tar.gz
    Keywords: ddc:550 ; mass spectral database ; analogue experiments ; ice grains ; ocean worlds ; SUDA ; ENIA ; LILBID ; TOF‐MS
    Language: English
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  • 80
    Publication Date: 2023-01-14
    Description: Over the last decades, treatment of domestic wastewater promoted by environmental regulations have reduced human health risks and improved water quality. However, ecological risks caused by effluents of wastewater treatment plants (WWTPs) discharged into rivers still persist. Moreover, the evolution of these ecological risks in the future is intimately related to effects of changing climate, especially regarding streamflow in receiving rivers. Here, we present an analytical and transferable framework for assessing the ecological risks posed by WWTP‐effluents at the catchment scale. The framework combines the size‐class k of WWTPs, which is a load‐proxy, with their outflows' location in river networks, represented by stream‐order ω. We identify ecological risks by using three proxy indicators: the urban discharge fraction and the local‐scale concentrations of each total phosphorous and ammonium‐nitrogen discharged from WWTPs. About 3,200 WWTPs over three large catchments (Rhine, Elbe, and Weser) in Central Europe were analyzed by incorporating simulated streamflow for the most extreme projected climate change scenario. We found that WWTPs causing ecological risks in the future prevail in lower ω, across almost all k. Distinct patterns of ecological risks are identified in the k‐ω framework for different indicators and catchments. We show, as climate changes, intensified risks are especially expected in lower ω receiving effluents of intermediate‐k WWTPs. We discuss the implications of our findings for prioritizing WWTPs upgrading and urging updates on environmental regulations. Further discussions underline the feasibility of applying the framework to any geographical regions and highlight its potentials to help in achieving global long‐term commitments on freshwater security.
    Description: Key Points: An analytical, generic framework was developed to assess wastewater treatment plants causing ecological risks in rivers under climate change. Smaller streams will face higher ecological risks for almost all load classes of wastewater treatment plants in future climate. Of the legally regulated effluent parameters for treated wastewater, ammonium‐nitrogen concentration will pose the greatest ecological risk.
    Description: Helmholtz Association http://dx.doi.org/10.13039/501100009318
    Keywords: ddc:551.48 ; analytical assessment framework ; wastewater treatment plants emissions ; river stream‐order ; dilution ; local‐scale nutrients concentrations
    Language: English
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  • 81
    Publication Date: 2023-01-14
    Description: Specular meteor radars (SMRs) have significantly contributed to the understanding of wind dynamics in the mesosphere and lower thermosphere (MLT). We present a method to estimate horizontal correlations of vertical vorticity (Qzz) and horizontal divergence (P) in the MLT, using line‐of‐sight multistatic SMRs velocities, that consists of three steps. First, we estimate 2D, zonal, and meridional correlation functions of wind fluctuations (with periods less than 4 hr and vertical wavelengths smaller than 4 km) using the wind field correlation function inversion (WCFI) technique. Then, the WCFI's statistical estimates are converted into longitudinal and transverse components. The conversion relation is obtained by considering the rotation about the vertical direction of two velocity vectors, from an east‐north‐up system to a meteor‐pair‐dependent cylindrical system. Finally, following a procedure previously applied in the upper troposphere and lower stratosphere to airborne wind measurements, the longitudinal and transverse spatial correlations are fitted, from which Qzz, P, and their spectra are directly estimated. The method is applied to a special Spread spectrum Interferometric Multistatic meteor radar Observing Network data set, obtained over northern Germany for seven days in November 2018. The results show that in a quasi‐axisymmetric scenario, P was more than five times larger than Qzz for the horizontal wavelengths range given by ∼50–400 km, indicating a predominance of internal gravity waves over vortical modes of motion as a possible explanation for the MLT mesoscale dynamics during this campaign.
    Description: Key Points: We investigate the horizontal correlation functions of vertical vorticity and horizontal divergence for mesoscale wind fluctuations in the mesosphere and lower thermosphere. 2D zonal and meridional correlation functions and 1D longitudinal and transverse correlation functions as a function of horizontal lags are analyzed. The divergence dominated over the vorticity during November 2018 in northern Germany.
    Description: Leibniz SAW
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: French Ministry of Foreign and European
    Description: https://doi.org/10.22000/536
    Keywords: ddc:551.5 ; MLT ; vorticity ; correlation function ; meteor radar ; mesoscales ; divergence
    Language: English
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  • 82
    Publication Date: 2023-01-14
    Description: High‐resolution flight data obtained from in situ measurements in the free atmosphere aboard the High Altitude and Long Range Research Aircraft (HALO) are used to determine eddy dissipation rates along extended flights during the recent Southern Hemisphere Transport, Dynamics, and Chemistry aircraft campaign (SOUTHTRAC) in the 2019 austral winter. These data are analyzed and correlated with quantities characterizing the ambient airflow and the magnitudes of vertical energy propagation through internal gravity waves. The observed turbulence events are strongly correlated with elevated shear values, and overturning gravity waves do not appear to play a role. A highlight of the analysis is the validation of a recently implemented Clear Air Turbulence (CAT) forecast index in the European Centre for Medium‐Range Weather Forecast integrated forecast system. Here we find a slightly better correlation of the CAT prediction with the HALO research aircraft observations compared to those of commercial aircraft. The observed turbulence during SOUTHTRAC was never stronger than moderate, as EDR values remained below 0.3 m2/3 s−1. In general, light and light‐to‐moderate turbulence events were extremely rare, occurring in only about 5% of the flight time, and stronger events in less than 0.2%. These results are also reflected in the local atmospheric conditions, which were dominated by a thermally very stable airflow with low vertical shear and large Richardson numbers.
    Description: Plain Language Summary: This study analyzes high‐resolution data of velocity components in the upper troposphere and lower stratosphere collected with the German research aircraft High Altitude and Long Range Research Aircraft during the Southern Hemisphere Transport, Dynamics, and Chemistry (SOUTHTRAC) campaign in September–November 2019. Flights were conducted predominantly over the southern part of South America, the Drake Passage, and the Antarctic Peninsula. The objective of the analysis was to determine the eddy dissipation rates during the 22 flights. The cubic root of eddy dissipation rates is a common measure used to characterize turbulent regions in the atmosphere. High quality observations with a very accurately calibrated sensor are rare, especially in the remote areas of the SOUTHTRAC campaign. Observed eddy dissipation rates have been correlated with gravity wave activity, but these correlations are very small. A much stronger dependence of the eddy dissipation rates exists on the vertical shear of the horizontal wind. Thus, mechanical generation of turbulence appears to dominate in the observed cases. Overall, the observed turbulence was never stronger than moderate. Turbulence events were extremely rare, occurring in only about 5% of the flight time, and stronger events less than 0.2%. Finally, the observed eddy dissipation rates were compared with weather model forecasts, demonstrating their reliability in predicting turbulent regions.
    Description: Key Points: Small eddy dissipation rates were observed in the free atmosphere along extended research flights during Southern Hemisphere Transport, Dynamics, and Chemistry in austral winter 2019. Stronger turbulence events are rare and are mostly correlated with enhanced vertical shear of the horizontal wind. EDR predictions of a 15‐member ensemble shows higher correlation with research aircraft observations than with those by commercial aircraft.
    Description: Federal Ministry for Education and Research
    Description: German Science Foundation
    Description: https://halo-db.pa.op.dlr.de/mission/116
    Description: https://halo-db.pa.op.dlr.de/dataset/8497
    Description: https://halo-db.pa.op.dlr.de/dataset/8496
    Description: https://apps.ecmwf.int/codes/grib/param-db/?id=260290
    Description: https://doi.org/10.21957/xbar-5611
    Description: https://halo-db.pa.op.dlr.de/dataset/8955
    Description: https://madis.ncep.noaa.gov/acars_variable_list.shtml
    Keywords: ddc:551.5 ; turbulence in the free atmosphere ; eddy dissipation rate ; clear‐air turbulence predictions ; ECMWF integrated forecast system
    Language: English
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  • 83
    Publication Date: 2023-01-14
    Description: Distributed models have been increasingly applied at finer spatiotemporal resolution. However, most diagnostic analyses aggregate performance measures in space or time, which might bias subsequent inferences. Accordingly, this study explores an approach for quantifying the parameter sensitivity in a spatiotemporally explicit way. We applied the Morris method to screen key parameters within four different sampling spaces in a grid‐based model (mHM‐Nitrate) for NO3‐N simulation in a mixed landuse catchment using a 1‐year moving window for each grid. The results showed that an overly wide range of aquatic denitrification rates could mask the sensitivity of the other parameters, leading to their spatial patterns only related to the proximity to outlet. With adjusted parameter space, spatial sensitivity patterns were determined by NO3‐N inputs and hydrological transport capacity, while temporal dynamics were regulated by annual wetness conditions. The relative proportion of parameter sensitivity further indicated the shifts in dominant hydrological/NO3‐N processes between wet and dry years. By identifying not only which parameter(s) is(are) influential, but where and when such influences occur, spatial sensitivity analysis can help evaluate current model parameterization. Given the marked sensitivity in agricultural areas, we suggest that the current NO3‐N parameterization scheme (land use‐dependent) could be further disentangled in these regions (e.g., into croplands with different rotation strategies) but aggregated in non‐agricultural areas; while hydrological parameterization could be resolved into a finer level (from spatially constant to land use‐dependent especially in nutrient‐rich regions). The spatiotemporal sensitivity pattern also highlights NO3‐N transport within soil layers as a focus for future model development.
    Description: Key Points: A diagnostic analysis was conducted to disentangle the parameter sensitivity for NO3‐N simulations in catchment modeling in space and time. Sensitivity differed within sampling spaces, but was controlled spatially by NO3‐N supply/water fluxes while temporally by wetness condition. Analysis suggests finer‐level parameterization needs in arable land, and prioritizes NO3‐N transport in soils for improved conceptualization.
    Description: Chinese Scholarship Council
    Description: Leverhulme Trust http://dx.doi.org/10.13039/501100000275
    Description: Einstein Stiftung Berlin http://dx.doi.org/10.13039/501100006188
    Description: Berlin University Alliance http://dx.doi.org/10.13039/501100021727
    Description: https://doi.org/10.5281/zenodo.6497225
    Description: https://fred.igb-berlin.de/data/package/629
    Keywords: ddc:551 ; spatial time‐varying sensitivity analysis ; distributed nitrate modeling
    Language: English
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  • 84
    Publication Date: 2023-01-14
    Description: Invasive alien species continue to spread and proliferate in waterways worldwide, but environmental drivers of invasion dynamics lack assessment. Knowledge gaps are pervasive in the Global South, where the frequent heavy human‐modification of rivers provides high opportunity for invasion. In southern Africa, the spatio‐temporal ecology of a widespread and high‐impact invasive alien snail, Tarebia granifera, and its management status is understudied. Here, an ecological assessment was conducted at seven sites around Nandoni Reservoir on the Luvuvhu River in South Africa. The distribution and densities of T. granifera were mapped and the potential drivers of population structure were explored. T. granifera was widespread at sites impacted to varying extents due to anthropogenic activity, with densities exceeding 500 individuals per square meter at the most impacted areas. T. granifera predominantly preferred shallow and sandy environments, being significantly associated with sediment (i.e., chlorophyll‐a, Mn, SOC, SOM) and water (i.e., pH, conductivity, TDS) variables. T. granifera seemed to exhibit two recruitment peaks in November and March, identified via size‐based stock assessment. Sediment parameters (i.e., sediment organic matter, sediment organic carbon, manganese) and water chemistry (i.e., pH, total dissolved solids, conductivity) were found to be important in structuring T. granifera populations, with overall snail densities highest during the summer season. We provide important autecological information and insights on the distribution and extent of the spread of T. granifera. This may help in the development of invasive alien snail management action plans within the region, as well as modelling efforts to predict invasion patterns elsewhere based on environmental characteristics.
    Description: Alexander von Humboldt‐Stiftung http://dx.doi.org/10.13039/100005156
    Description: National Research Foundation http://dx.doi.org/10.13039/501100001321
    Description: University of Venda http://dx.doi.org/10.13039/501100008976
    Keywords: ddc:577.6 ; aquatic non‐native invasions ; environmental gradients ; Global South ; human‐modified river ; quilted melania ; reservoir
    Language: English
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  • 85
    Publication Date: 2023-01-14
    Description: The seasonal deposition and sublimation of CO2 constitute a major element in Martian volatile cycles. We reprocess the Mars Orbiter Laser Altimeter (MOLA) data and apply co‐registration procedures to obtain spatio‐temporal variations in levels of the Seasonal North Polar Cap (SNPC). The maximum level over the Residual North Polar Cap (RNPC) is 1.3 m, approximately half of that at the south pole (2.5 m). However, the maximum level in the dune fields at Olympia Undae can be up to 3.8 m. Furthermore, off‐season decreases up to 3 m during the northern winter at Olympia Undae are observed. These are likely due to metamorphism effects accentuated by the reduced snowfall at this period. Meanwhile, off‐season increases of up to 2 m during the northern spring are noted, the cause of which remains to be explored. The volume of the SNPC peaks at the end of northern winter and is estimated to be approximately 9.6 × 1012 m3, which is 2% more than that of the Seasonal South Polar Cap. The bulk density of the SNPC can go through phased decreases in accordance with phased accumulation at northern high‐latitudes. These findings can put important constraints on the Martian volatile cycling models.
    Description: Plain Language Summary: Due to its axial tilt, seasons also exist on Mars. Up to one third of the atmosphere's CO2 is in annual exchange with the polar regions through seasonal deposition/sublimation processes. Here, we make use of previously proposed approaches of analyzing the Mars Orbiter Laser Altimeter profiles and obtain spatio‐temporal level variations of the Seasonal North Polar Cap (SNPC). Particularly, we bring attention to abnormal behavior of the SNPC in the dune fields at Olympia Undae. Maximum level there can be all the way up to 4 m which is much higher than a maximum of 1.5 m over the Residual North Polar Cap. Meanwhile, off‐season decreases during the northern winter with magnitudes up to 3 m and off‐season increases during the northern spring of magnitudes up to 2 m are observed. These could possibly be related to metamorphism of the seasonal deposits and phased snowfall. The maximum volume of the SNPC is constrained to be 9.6 × 1012 m3. The bulk density of the SNPC does not continuously increase as previously assumed but can go through phased decreases in accordance with phased snowfall at the north pole. These findings can put important constraints on the Martian climate models.
    Description: Key Points: Through co‐registration of laser altimetry profiles, spatio‐temporal level variations of the Seasonal North Polar Cap (SNPC) of Mars are obtained. Maximum level of the SNPC can be up to 3.8 m at Olympia Undae and up to 1.3 m over the Residual North Polar Cap. Northern winter decreases of up to 3 m and northern spring increases of up to 2 m are observed at Olympia Undae.
    Description: China Scholarship Council
    Description: Deutsche Forschungsgemeinschaft
    Description: Institut National des Sciences de l’Univers
    Description: Centre National de la Recherche Scientifique
    Description: Centre National d’Etudes Spatiales
    Description: https://doi.org/10.17632/x953mzxxvv.1
    Description: https://doi.org/10.17632/z59b9nd6s9.2
    Description: https://pds-geosciences.wustl.edu/missions/mgs/pedr.html
    Description: https://naif.jpl.nasa.gov/pub/naif/pds/data/mgs-m-spice-6-v1.0/mgsp_1000/data/
    Description: https://www.uahirise.org/hiwish/browse
    Keywords: ddc:523 ; Mars ; seasonal polar cap ; CO2 ice ; MOLA ; level variation ; pseudo cross‐over
    Language: English
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  • 86
    Publication Date: 2023-01-13
    Description: The thermal conductivities of mantle and core materials have a major impact on planetary evolution, but their experimental determination requires precise knowledge of sample thickness at high pressure. Despite its importance, thickness in most diamond anvil cell (DAC) experiments is not measured but inferred from equations of state, assuming isotropic contraction upon compression or assuming isotropic expansion upon decompression. Here we provide evidence that in DAC experiments both assumptions are invalid for a range of mechanically diverse materials (KCl, NaCl, Ar, MgO, silica glass, Al2O3). Upon compression, these samples are ∼30–50% thinner than expected from isotropic contraction. Most surprisingly, all the studied samples continue to thin upon decompression to 10–20 GPa. Our results partially explain some discrepancies among the highly controversial thermal conductivity values of iron at Earth's core conditions. More generally, we suggest that in situ characterization of sample geometry is essential for conductivity measurements at high pressure.
    Description: Plain Language Summary: The thermal and electrical conductivities of the materials making up Earth's core and lowermost mantle are crucial inputs for modeling Earth's interior and the geodynamo mechanism. Yet, large disagreements between published values of conductivity are common, including a factor‐of‐seven discrepancy in the thermal conductivity of iron at core‐mantle boundary conditions. One possible source of systematic uncertainty is the estimate of sample thickness during high‐pressure experiments. Here we show that common materials in compression experiments tend to thin by much more than previously assumed. Surprisingly, the thinning continues upon decompression. These thinning trends could lead to ∼30–50% systematic error, partially explaining the discrepancy in iron conductivity. In situ thickness measurements are thus crucial for accurate determination of conductivities of Earth's mantle and core.
    Description: Key Points: Samples in diamond anvil cell experiments contract and expand in a strongly non‐isotropic fashion upon compression and decompression. Experimental reports on iron conductivity at high pressure contain errors due to the assumption of isotropic contraction or expansion. Accurate in situ determination of sample geometry is necessary for thermal and electrical conductivity measurements at high pressure.
    Description: Helmholtz Association http://dx.doi.org/10.13039/501100009318
    Description: National Science Foundation http://dx.doi.org/10.13039/100000001
    Description: https://doi.org/10.17632/wnvbty8y83.4
    Keywords: ddc:551.12 ; diamond anvil cell ; thermal conductivity ; high pressure
    Language: English
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  • 87
    Publication Date: 2023-01-13
    Description: Polarities of seismic reflections at the discontinuity atop the D" region (PdP and SdS) indicate the sign of the velocity contrast across the D" reflector. Recent studies found PdP polarities matching and opposite those of P and PcP. While anisotropy could explain this behavior, we find that the ratio of the change in S wave velocity over change in P wave velocity (R‐value) can influence polarity behavior of D" reflected P waves. For R‐values exceeding 3, the P wave reverses polarity in the absence of anisotropy while S wave polarity is not influenced by the R‐value. Using sets of one million models for normal mantle and MORB with varying minerals and processes across the boundary, we carry out a statistical analysis (Linear Discriminant Analysis) finding that there is a marked difference in mantle mineralogy to explain R‐values larger and smaller than 3, respectively. Based on our results we can attribute different mineralogy to a number of cases. In particular, we find that when velocities increase across D" and polarities of PdP and SdS are opposite the post‐perovskite phase transition is still the best explanation whereas MORB is the best explanation when PdP and SdS are the same. When the velocities are decreasing, the post‐perovskite phase transition within MORB is the best explanation if PdP and SdS polarities are the same but if PdP and SdS are opposite, our results indicate that primordial material or mantle enriched in bridgmanite can explain the polarity behavior, further constraining mineralogy within the large low seismic velocity provinces.
    Description: Plain Language Summary: Polarities of seismic waves reflecting at structures in the Earth's mantle indicate seismic velocity changes there. For the lowermost mantle reflector, a velocity increase generates a polarity that is the same for the main wave and the core‐reflected wave. If, however, the percentage change of the velocity of the S wave increases at least three times as much as that of the P wave velocity (expressed as the R‐value, the ratio dVs/dVp), the polarity of the D"‐reflected PdP wave changes polarity, becoming opposite to both the main P wave and the reflection from the core‐mantle boundary below it. Here, we analyze sets of 1 million models with variable compositions of mantle material and mid‐ocean ridge basalt and use an advanced statistical method to identify those combinations of minerals that produce large positive R‐values. We distinguish four cases and find that previous explanations for three of these cases concur with our analysis. For regions where velocities decrease over the D" reflector, our analysis shows that enrichment with the lower‐mantle mineral bridgmanite is responsible for the observed polarity behavior of P and S waves. This means that for regions such as large low‐velocity anomalies in the lowermost mantle, primitive or bridgmanite‐enriched material is the preferred explanation.
    Description: Key Points: Ratio (R) of S‐ over P wave velocity changes (%) controls the polarity of P wave reflections at D" reflector. Thermochemical modeling and statistical analysis show specific minerals contributing to large R‐values. Polarity observations indicate that part of the Pacific large low seismic velocity province is due to bridgmanite enrichment.
    Description: Deutsche Forschungsgemeinschaft and Agence Nationale de la Recherche http://dx.doi.org/10.13039/501100001659
    Description: Nederlandse Organisatie voor Wetenschappelijk Onderzoek http://dx.doi.org/10.13039/501100003246
    Description: Deutscher Akademischer Austauschdienst http://dx.doi.org/10.13039/501100001655
    Description: https://doi.org/10.7914/SN/XE_2003
    Description: https://doi.org/10.7914/SN/TA
    Keywords: ddc:551.12 ; seismology ; wave polarity ; statistics ; thermochemical modeling ; D
    Language: English
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  • 88
    Publication Date: 2023-01-13
    Description: Managed aquifer recharge (MAR) refers to a suite of methods that is increasingly being applied worldwide for sustainable groundwater management to tackle drinking or irrigation water shortage or to restore and maintain groundwater ecosystems. The potential for MAR is far from being exhausted, not only due to geological and hydrogeological conditions or technical and economic feasibility but also due to its lack of acceptance by the public and policymakers. One approach to enable the safe and accepted use of MAR could be to provide comprehensive risk management, including the identification, analysis, and evaluation of potential risks related to MAR. This article reviews current MAR risk assessment methodologies and guidelines and summarizes possible hazards and related processes. It may help planners and operators select the appropriate MAR risk assessment approaches and support the risk identification process. In addition to risk assessment (and subsequent risk treatment) related to the MAR implementation phase, this review also addresses risk assessment for MAR operation. We also highlight the limitations and lessons learned from the application and development of risk assessment methodologies. Moreover, developments are recommended in the area of MAR‐related risk assessment methodologies and regulation. Depending on data availability, collected methodologies may be applicable for MAR sites worldwide. Integr Environ Assess Manag 2022;18:1513–1529. © 2022 The Authors. Integrated Environmental Assessment and Management published by Wiley Periodicals LLC on behalf of Society of Environmental Toxicology & Chemistry (SETAC).
    Description: Key Points: The past two decades have seen a marked increase in the literature on MAR‐related risk assessment, and a further increase is expected, since more attractive strategies are being used worldwide for integrated groundwater management. The development of holistic risk management plans can improve social acceptability and contribute to safer implementation and operation of MAR schemes. In connection with holistic risk management, MAR can be seen as a viable option for reaching the United Nations Sustainable Development Goal #6. Widely lacking regulations worldwide for risk assessment of MAR schemes is identified to hinder MAR implementation and safe operation worldwide.
    Description: DEEPWATER‐CE
    Description: ENeRAG
    Keywords: ddc:553.7 ; Groundwater management ; Guidelines ; Managed aquifer recharge ; Methodologies ; Risk assessment
    Language: English
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  • 89
    Publication Date: 2023-01-13
    Description: A volcanic eruption is usually preceded by seismic precursors, but their interpretation and use for forecasting the eruption onset time remain a challenge. A part of the eruptive processes in open conduits of volcanoes may be similar to those encountered in geysers. Since geysers erupt more often, they are useful sites for testing new forecasting methods. We tested the application of Permutation Entropy (PE) as a robust method to assess the complexity in seismic recordings of the Strokkur geyser, Iceland. Strokkur features several minute‐long eruptive cycles, enabling us to verify in 63 recorded cycles whether PE behaves consistently from one eruption to the next one. We performed synthetic tests to understand the effect of different parameter settings in the PE calculation. Our application to Strokkur shows a distinct, repeating PE pattern consistent with previously identified phases in the eruptive cycle. We find a systematic increase in PE within the last 15 s before the eruption, indicating that an eruption will occur. We quantified the predictive power of PE, showing that PE performs better than seismic signal strength or quiescence when it comes to forecasting eruptions.
    Description: Plain Language Summary: When a volcano shows the first sign of activity, it is challenging to determine whether and when the actual eruption will occur. Usually, researchers create earthquake lists and locate these events to assess this. However, an alternative and simpler method can be directly applied to continuous seismic data. We tested a method that assesses the complexity of signals. We first created synthetic data to find reasonable parameter settings for this method. While volcanoes do not erupt very often, frequent eruptions at geysers allow us to systematically study and compare several eruptions. We analyzed the continuous record of 63 eruptions of the Strokkur geyser, Iceland. Our results show a distinct pattern that repeats from one eruption to the next one. We also find a clear pattern that indicates about 15 s before the next eruption that an eruption will occur. We show that this method performs better in eruption forecasting than assessing the seismic noise or silence caused by the geyser.
    Description: Key Points: Permutation Entropy (PE) is a simple tool to assess the complexity of a time series. We analyzed the PE evolution for 63 eruptive cycles of Strokkur geyser and found characteristic changes in PE during recharge. PE is found to be an useful statistical predictor of the eruption times and highlights the precursor 15 s before eruptions.
    Description: Deutscher Akademischer Austauschdienst http://dx.doi.org/10.13039/501100001655
    Description: https://geofon.gfz-potsdam.de/doi/network/7L/2017
    Description: https://gitup.uni-potsdam.de/pujiastutisudibyo/permutationentropy
    Keywords: ddc:551.21 ; permutation entropy ; forecasting ; geyser ; eruption ; hydrothermal system ; volcano‐seismology
    Language: English
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  • 90
    Publication Date: 2023-01-13
    Description: Low‐level mixed‐phase clouds (MPCs) occur extensively in the Arctic, and are known to play a key role for the energy budget. While their characteristic structure is nowadays well understood, the significance of different precipitation‐formation processes, such as aggregation and riming, is still unclear. Using a 3‐year data set of vertically pointing W‐band cloud radar and K‐band Micro Rain Radar (MRR) observations from Ny‐Ålesund, Svalbard, we statistically assess the relevance of aggregation in Arctic low‐level MPCs. Combining radar observations with thermodynamic profiling, we find that larger snowflakes (mass median diameter larger than 1 mm) are predominantly produced in low‐level MPCs whose mixed‐phase layer is at temperatures between −15 and −10°C. This coincides with the temperature regime known for favoring aggregation due to growth and subsequent mechanical entanglement of dendritic crystals. Doppler velocity information confirms that these signatures are likely due to enhanced ice particle growth by aggregation. Signatures indicative of enhanced aggregation are however not distributed uniformly across the cloud deck, and only observed in limited regions, suggesting a link with dynamical effects. Low Doppler velocity values further indicate that significant riming of large particles is unlikely at temperatures colder than −5°C. Surprisingly, we find no evidence of enhanced aggregation at temperatures warmer than −5°C, as is typically observed in deeper cloud systems. Possible reasons are discussed, likely connected to the ice habits that form at temperatures warmer than −10°C, increased riming, and lack of particle populations characterized by broader size distributions precipitating from higher altitudes.
    Description: Plain Language Summary: Low‐level mixed‐phase clouds (MPCs), that is, shallow clouds containing both liquid droplets and ice crystals, form frequently in the Arctic region. Their characteristic structure—consisting of one or multiple liquid layers at sub‐zero temperatures, from which ice crystals form and precipitate—is nowadays well understood. However, the processes that lead to the growth of ice crystals into snow have been overlooked. Using a 3‐year data set of radar observations from Ny‐Ålesund, in Svalbard, Norway, we are able to identify situations when the ice particle growth is dominated by aggregation of several individual crystals. Combining radar observations with temperature information, we find that larger snowflakes are only produced in MPCs if their liquid portion is at temperatures between −15 and −10°C. This coincides with the temperature regime known for favoring aggregation due to growth and subsequent entanglement of branched crystals. Surprisingly, we find no evidence of enhanced ice aggregation at temperatures warmer than −5°C, as is typically observed in deeper cloud systems. Possible reasons are discussed, likely connected to the ice crystal shapes that develop at temperatures warmer than −10°C, increased liquid droplet production, and lack of particles precipitating from higher altitudes.
    Description: Key Points: Low‐level mixed‐phase clouds (MPCs) at Ny‐Ålesund produce large aggregates predominantly at dendritic‐growth temperatures. Enhanced aggregation due to dendritic growth occurs intermittently in limited regions of the MPC. The typically observed enhanced aggregation zone close to 0°C is absent in low‐level MPCs at the site.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: ddc:551.5 ; Arctic mixed‐phase clouds ; aggregation ; riming ; dendritic‐growth zone ; radar
    Language: English
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  • 91
    Publication Date: 2023-01-13
    Description: Massif‐type anorthosite and comagmatic associations of rutile‐bearing ilmenitite (RBI) and oxide‐apatite‐rich amphibolite (OARA) from the Chiapas Massif Complex (CMC) in southeastern Mexico display a protracted billion‐year accessory mineral record encompassing magmatic crystallization at c. 1.0 Ga to recent ductile shear deformation at c. 3.0 Ma. Multiple discrete zircon populations between these age end‐members resulted from neoformation/recrystallization during local to regional metamorphism that affected the southeastern portion of the CMC. The ubiquitous presence of relict baddeleyite (ZrO2), along with various zircon generations spatially associated with pristine to partly retrogressed Zr‐bearing igneous and metamorphic minerals (e.g., ilmenite, rutile, högbomite and garnet), suggests significant Zr diffusive re‐equilibration (exsolution) during slow cooling and mineral breakdown followed by crystallization of baddeleyite. The subsequent transformation of baddeleyite into zircon was likely driven by reaction with Si‐bearing fluids in several geochronologically identified metamorphic stages. Strikingly contrasting compositional signatures in coeval zircon from anorthosite (silicate‐dominated) and comagmatic RBI (Ti‐Fe‐oxide‐dominated) indicate a major role of fluids locally equilibrating with the rock matrix, as indicated by distinct zircon trace element and oxygen isotopic compositions. A high‐grade metamorphic event at c. 950 Ma is likely responsible for the formation of coarse‐grained rutile (~0.1–10 mm in diameter), srilankite, zircon and garnet with rutile inclusions as well as metamorphic högbomite surrounding Fe‐Mg spinel. Zr‐in‐rutile minimum temperatures suggest 〉730°C for this event, which may correlate to rutile‐forming granulite facies metamorphism in other Grenvillian‐aged basement rocks in Mexico and northern South America. A younger generation of baddeleyite exsolution occurred during post‐peak cooling of coarse‐grained rutile, reflected in rimward Zr depletion and formation of discontinuous baddeleyite coronas. Baddeleyite around rutile was then transformed into zircon possibly during subsequent metamorphism at c. 920 or 620 Ma, resulting from syn‐kinematic and contact metamorphism, respectively. Regional metamorphism at c. 450 and 250 Ma extensively overprinted the existing zircon population, especially during the Triassic event, as suggested by a significant presence of zircon with this age. Nearly pristine baddeleyite occurring interstitial to ilmenite yielded an isochron age of c. 232 Ma according to in situ U–Pb secondary ion mass spectrometry (SIMS), suggesting either formation during metamorphic peak conditions or post‐peak cooling. Zircon with ages of c. 80–100 Ma in anorthosite is identified for the first time within the CMC and coincides with cooling ages of c. 100 Ma for coarse‐grained rutile. This age is similar to those of rocks occurring ~200 km further to the east in Guatemala, which are also bounded to the Polochic fault system but overprinted by eclogite facies metamorphism. A high‐pressure event in the southern CMC after 200 Ma, however, is presently unsupported. Although the abundance of rutile and ilmenite is unusually high in the CMC anorthosite assemblage compared with common igneous rocks, the reactions documented here nonetheless stress the importance of these phases for generating Zr‐bearing accessory minerals over a wide range of metamorphic conditions.
    Description: Consejo Nacional de Ciencia y Tecnología (CONACYT) http://dx.doi.org/10.13039/501100003141
    Description: Deutsche Forschungsgemeinschaft (DFG)
    Keywords: ddc:549 ; Diffusion ; SIMS ; Srilankite ; Ti‐Fe deposits ; Ti‐in‐zircon ; Zr‐in‐rutile
    Language: English
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  • 92
    Publication Date: 2023-01-13
    Description: Recent observations by the Juno spacecraft have shown that electrons contributing to Jupiter's main auroral emission appear to be frequently characterized by broadband electron distributions, but also less often mono‐energetic electron distributions are observed as well. In this work, we quantitatively derive the occurrence rates of the various electron distributions contributing to Jupiter's aurora. We perform a statistical analysis of electrons measured by the JEDI‐instrument within 30–1,200 keV from Juno's first 20 orbits. We determine the electron distributions, either pancake, field‐aligned, mono‐energetic, or broadband, through energy and pitch angles to associate various acceleration mechanisms. The statistical analysis shows that field‐aligned accelerated electrons at magnetic latitudes greater than 76° are observed in 87.6% ± 7.2% of the intervals time averaged over the dipole L‐shells according the main oval. Pancake distributions, indicating diffuse aurora, are prominent at smaller magnetic latitudes (〈76°) with an occurrence rate of 86.2% ± 9.6%. Within the field‐aligned electron distributions, we see broadband distributions 93.0% ± 3.8% of the time and a small fraction of isolated mono‐energetic distribution structures 7.0% ± 3.8% of the time. Furthermore, these occurrence statistics coincide with the findings from our energy flux statistics regarding the electron distributions. Occurrence rates thus also characterize the overall energetics of the different distribution types. This study indicates that stochastic acceleration is dominating the auroral processes in contrast to Earth where the discrete aurora is dominating.
    Description: Plain Language Summary: With the Juno spacecraft arriving in the magnetosphere of Jupiter, first flyby particle measurements have changed the knowledge about the developing process of Jupiter's intense aurora. The observations of auroral particles show a stochastic behavior rather than a preference for specific energy. Our statistical analysis of the first 20 flybys at Jupiter compares the occurrence of different particle distributions and highlights the importance of different generation theories for Jupiter's aurora. A generation via stochastic rather than mono‐energetic behavior is deduced and supports previous observations.
    Description: Key Points: We present a statistical study of Jupiter's auroral electrons within 30–1,200 keV based on Juno's first 20 perijoves. Broadband electron distributions dominates Jupiter's main auroral zone as they are observed in 93% ± 3% of the intervals studied here. Dominance of broadband distributions underlines the importance of a turbulent or stochastic acceleration process.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Universität zu Köln http://dx.doi.org/10.13039/501100008001
    Description: https://lasp.colorado.edu/home/mop/files/2015/02/CoOrd_systems7.pdf
    Description: https://pds-ppi.igpp.ucla.edu/mission/JUNO/JNO/JEDI
    Description: https://lasp.colorado.edu/home/mop/files/2020/04/20190412_Imai_MagFootReader_UIowa_rev.pdf
    Keywords: ddc:523 ; auroral precipitation budget ; particle distribution ; Jupiter ; Juno
    Language: English
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  • 93
    Publication Date: 2023-01-13
    Description: Management of hydropower plants strongly influences streamflow dynamics and hence the interaction between surface water and groundwater. As dam operations cause variations in river stages, these can result in changes in the groundwater level at multiple temporal scales. In this work, we study the case of an Alpine aquifer, where weekly fluctuations are particularly pronounced. We consider an area with four river reaches differently impacted by reservoir operations and investigate the influence of these rivers on the common aquifer. Using continuous wavelet transform and wavelet coherence analysis, we show that weekly fluctuations in the groundwater table are particularly pronounced in dry years, in particular in the winter season, although the area of the aquifer impacted by dam operations remains almost unchanged. We thus observe that in Alpine catchments, surface water‐groundwater interaction is sensitive to the conditions determined by a specific hydrological year. We also investigate the influences of the river‐aquifer water fluxes and show that under dry conditions hydropeaking mainly affects their temporal dynamics. Our observations have significant consequences for predicting nutrient and temperature dynamics/regimes in river‐aquifer systems impacted by hydropower plant management.
    Description: Plain Language Summary: The operation of hydropower plants affects the water level in the downstream part of the river, which in turn can alter the groundwater level. In this work, we study an Alpine aquifer crossed by rivers differently impacted by hydropower production. We use statistical tools to analyze the interaction between the rivers and the groundwater, and observe that this interaction is sensitive to the conditions of the hydrological year, such as dry periods.
    Description: Key Points: Wavelet power spectrum and coherence analysis is used to study river‐aquifer interactions under dam operations in an Alpine catchment. The impact of reservoir operations on the aquifer is strongest under low flow conditions but the area impacted shows little variation. Under low flow conditions, dam operations considerably influence the frequency of the water exchange between rivers and aquifer.
    Description: Consejo Nacional de Ciencia y Tecnología http://dx.doi.org/10.13039/501100003141
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Consejo Veracruzano de Investigación Científica y Desarrollo Tecnológico
    Description: https://doi.org/10.17632/97jchhz4s8.2
    Keywords: ddc:551 ; surface water‐groundwater interaction ; hydropower ; managed rivers ; groundwater modeling
    Language: English
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  • 94
    Publication Date: 2023-01-13
    Description: During the last 20 years some very hot and dry summers affected Europe, resulting in regionally record‐breaking high temperature or low precipitation values. Long‐term changes of such extremely hot and dry summers are of great relevance for our society, as they are connected with manifold negative impacts on human society, natural ecosystems, and diverse economic sectors. Long‐term variations in drought and five record drought summer half years are studied based on 63 stations across Europe with high‐quality precipitation and temperature time series spanning the period 1901–2018. Eight drought indices are deployed to analyse drought intensity, frequency, and duration; four of them purely precipitation‐based and four integrating potential evapotranspiration in the computation. Additionally, three heavy precipitation indices and simultaneous increases in drought and heavy precipitation are studied. The five driest summer half years over Europe are identified (1947, 2018, 2003, 1921, and 1911). They are analysed by aggregating eight drought indices into the aggregated drought evaluation index (ADE) for five subregions. The ADE shows increasing summer drought conditions over most of Europe, except for some stations in northern Europe. The increase in drought conditions during the warm part of the year is particularly pronounced for indices integrating evapotranspiration in their definition. At the same time, the intensity of heavy precipitation events shows a positive trend, as well as an increased contribution to total precipitation. Several stations in central Europe show simultaneously increasing drought conditions and increasing heavy precipitation events. This increases the risks connected with precipitation extremes.
    Description: Drought and heavy precipitation trends are studied for selected stations with long time series. Both extreme events are related to specific impacts on different economic sectors and thus society. Stations that simultaneously show increasing trends in drought and heavy precipitation mainly occur in central Europe. This indicates a probably higher exposure to these risks in central Europe as well as a demand for broader adaptation options in this region.
    Keywords: ddc:551.6 ; climate indices ; climate variability and change ; dry periods ; mRAI ; WBAI
    Language: English
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  • 95
    Publication Date: 2023-01-19
    Description: Detailed imaging of accretionary wedges reveals splay fault networks that could pose a significant tsunami hazard. However, the dynamics of multiple splay fault activation during megathrust earthquakes and the consequent effects on tsunami generation are not well understood. We use a 2‐D dynamic rupture model with complex topo‐bathymetry and six curved splay fault geometries constrained from realistic tectonic loading modeled by a geodynamic seismic cycle model with consistent initial stress and strength conditions. We find that all splay faults rupture coseismically. While the largest splay fault slips due to a complex rupture branching process from the megathrust, all other splay faults are activated either top down or bottom up by dynamic stress transfer induced by trapped seismic waves. We ascribe these differences to local non‐optimal fault orientations and variable along‐dip strength excess. Generally, rupture on splay faults is facilitated by their favorable stress orientations and low strength excess as a result of high pore‐fluid pressures. The ensuing tsunami modeled with non‐linear 1‐D shallow water equations consists of one high‐amplitude crest related to rupture on the longest splay fault and a second broader wave packet resulting from slip on the other faults. This results in two episodes of flooding and a larger run‐up distance than the single long‐wavelength (300 km) tsunami sourced by the megathrust‐only rupture. Since splay fault activation is determined by both variable stress and strength conditions and dynamic activation, considering both tectonic and earthquake processes is relevant for understanding tsunamigenesis.
    Description: Plain Language Summary: In subduction zones, where one tectonic plate moves beneath another, earthquakes can occur on many different faults. Splay faults are relatively steep faults that branch off the largest fault (the megathrust) in a subduction zone. As they are steeper than the megathrust, the same amount of movement on them could result in more vertical displacement of the seafloor. Therefore, splay faults are thought to play an important role in the generation of tsunamis. Here, we use computer simulations to study if an earthquake can break multiple splay faults at once and how this affects the resulting tsunami. We find that multiple splay faults can indeed fail during a single earthquake due to the stress changes from trapped seismic waves, which promote rupture on splay faults. Rupture on splay faults results in larger seafloor displacements with smaller wavelengths, so the ensuing tsunami is bigger and results in two main flooding episodes at the coast. Our results show that it is important to consider rupture on splay faults when assessing tsunami hazard.
    Description: Key Points: Multiple splay faults can be activated during a single earthquake by megathrust slip and dynamic stress transfer due to trapped waves. Splay fault activation is facilitated by their favorable orientation with respect to the local stress field and their closeness to failure. Long‐term geodynamic stresses and fault geometries affect dynamic splay fault rupture and the subsequent tsunami.
    Description: Volkswagen Foundation (VolkswagenStiftung) http://dx.doi.org/10.13039/501100001663
    Description: Royal Society (The Royal Society) http://dx.doi.org/10.13039/501100000288
    Description: EC | H2020 | H2020 Priority Excellent Science | H2020 European Research Council (ERC) http://dx.doi.org/10.13039/100010663
    Description: Deutsche Forschungsgemeinschaft (DFG) http://dx.doi.org/10.13039/501100001659
    Description: National Science Foundation (NSF) http://dx.doi.org/10.13039/100000001
    Description: https://github.com/TUM-I5/SWE
    Description: https://doi.org/10.5281/zenodo.6969455
    Keywords: ddc:551 ; earthquake ; tsunami ; subduction zone ; dynamic rupture ; splay fault ; numerical modeling
    Language: English
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  • 96
    Publication Date: 2023-01-19
    Description: Realistic prediction of the near‐future response of Arctic Ocean primary productivity to ongoing warming and sea ice loss requires a mechanistic understanding of the processes controlling nutrient bioavailability. To evaluate continental nutrient inputs, biological utilization, and the influence of mixing and winter processes in the Laptev Sea, the major source region of the Transpolar Drift (TPD), we compare observed with preformed concentrations of dissolved inorganic nitrogen (DIN) and phosphorus (DIP), silicic acid (DSi), and silicon isotope compositions of DSi (δ30SiDSi) obtained for two summers (2013 and 2014) and one winter (2012). In summer, preformed nutrient concentrations persisted in the surface layer of the southeastern Laptev Sea, while diatom‐dominated utilization caused intense northward drawdown and a pronounced shift in δ30SiDSi from +0.91 to +3.82‰. The modeled Si isotope fractionation suggests that DSi in the northern Laptev Sea originated from the Lena River and was supplied during the spring freshet, while riverine DSi in the southeastern Laptev Sea was continuously supplied during the summer. Primary productivity fueled by river‐borne nutrients was enhanced by admixture of DIN‐ and DIP‐rich Atlantic‐sourced waters to the surface, either by convective mixing during the previous winter or by occasional storm‐induced stratification breakdowns in late summer. Substantial enrichments of DSi (+240%) and DIP (+90%) beneath the Lena River plume were caused by sea ice‐driven redistribution and remineralization. Predicted weaker stratification on the outer Laptev Shelf will enhance DSi utilization and removal through greater vertical DIN supply, which will limit DSi export and reduce diatom‐dominated primary productivity in the TPD.
    Description: Plain Language Summary: Ongoing warming and sea ice loss in the Arctic Ocean may significantly impact biological productivity, which is mainly controlled by light and nutrient availability. To investigate nutrient inputs from land, biological utilization, and the influence of water mass mixing and winter processes on the nutrient distributions, we measured nutrient concentrations and silicon isotopes in the Laptev Sea. We found high concentrations in the southeastern Laptev Sea in agreement with nutrient inputs from the Lena River. Toward the northern Laptev Sea, nutrient concentrations decreased in the surface layer and the silicon isotope signatures shifted to heavier values, consistent with nutrient utilization by phytoplankton. In contrast to the depleted surface layer, the bottom layer beneath the Lena River plume was strongly enriched in some nutrients, which we attribute to different physical and biogeochemical processes. These observations are important for our understanding of nutrient bioavailability in the Laptev Sea and the Transpolar Drift (TPD), which is a surface current that connects the Laptev Sea with the central Arctic Ocean and the Fram Strait. The changing hydrography of the Laptev Sea will likely cause a decrease in silicic acid concentrations and thus a reduction in nutrient export and diatom‐dominated primary productivity in the TPD.
    Description: Key Points: Surface dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (DIP), silicic acid (DSi), and Si isotope dynamics are controlled by marine and riverine inputs and uptake by phytoplankton. Strong DIP and DSi enrichments beneath the Lena River plume are due to sea ice‐driven nutrient redistribution and remineralization. Enhanced DSi utilization in the Laptev Sea will lead to a reduced diatom‐dominated primary productivity in the Transpolar Drift.
    Description: Bundesministerium für Bildung und Forschung http://dx.doi.org/10.13039/501100002347
    Description: Ocean Frontier Institute http://dx.doi.org/10.13039/501100010784
    Description: Canada First Research Excellence Fund http://dx.doi.org/10.13039/501100010785
    Description: https://doi.pangaea.de/10.1594/PANGAEA.931257
    Description: https://doi.pangaea.de/10.1594/PANGAEA.931240
    Description: https://doi.pangaea.de/10.1594/PANGAEA.931209
    Description: https://doi.pangaea.de/10.1594/PANGAEA.938259
    Keywords: ddc:577.7 ; Arctic Ocean ; Laptev Sea ; transpolar drift ; nutrients ; silicon isotopes ; diatoms
    Language: English
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  • 97
    Publication Date: 2023-01-19
    Description: Climate change, pollution, and deforestation have a negative impact on global mental health. There is an environmental justice dimension to this challenge as wealthy people and high‐income countries are major contributors to climate change and pollution, while poor people and low‐income countries are heavily affected by the consequences. Using state‐of‐the art data mining, we analyzed and visualized the global research landscape on mental health, climate change, pollution and deforestation over a 15‐year period. Metadata of papers were exported from PubMed®, and both relevance and relatedness of terms in different time frames were computed using VOSviewer. Co‐occurrence graphs were used to visualize results. The development of exemplary terms over time was plotted separately. The number of research papers on mental health and environmental challenges is growing in a linear fashion. Major topics are climate change, chemical pollution, including psychiatric medication in wastewater, and neurobiological effects. Research on specific psychiatric syndromes and diseases, particularly on their ethical and social aspects is less prominent. There is a growing body of research literature on links between mental health, climate change, pollution, and deforestation. This research provides a graphic overview to mental healthcare professionals and political stakeholders. Social and ethical aspects of the climate change‐mental health link have been neglected, and more research is needed.
    Description: Plain Language Summary: Climate change, deforestation, and pollution are having a major effect on mental health all around the world. Yet there are huge disparities on how these negative consequences affect people within and between countries. We analyzed large databases of research articles using digital tools (data mining) to uncover the direction of scientific research and areas that have received less scholarly attention. While research linking climate change to mental health issues is expanding, a detailed examination of the social justice dimension of how climate change and pollution are affecting the different groups of people is still relatively scarce. We provide a graphical overview of the most important research keywords of the last 15 years.
    Description: Key Points: Climate change, pollution, and deforestation threaten global mental health and need to be addressed as a mental health issue. Data mining can help to uncover trends and gaps in research. Mental health research on climate change and pollution is growing, while research linking these to environmental injustice is less prominent.
    Description: Clinician Scientist Programme of the Medical Faculty of Ulm University
    Keywords: ddc:363.7 ; climate change ; mental health ; data mining ; medical ethics ; contamination ; environmental justice
    Language: English
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  • 98
    Publication Date: 2023-01-19
    Description: The Atmosphere and Ocean De‐Aliasing Level‐1B (AOD1B) product provides a priori information about temporal variations in the Earth's gravity field induced by non‐tidal circulation processes in atmosphere and ocean. It is routinely applied as a background model in the Gravity Recovery and Climate Experiment (GRACE)/GRACE Follow‐On (GRACE‐FO) satellite gravimetry data processing. We here present three new datasets in preparation for the upcoming release RL07 of AOD1B, that are based on either the global ERA5 reanalysis or the ECMWF operational data together with simulations from the Max‐Planck‐Institute for Meteorology general circulation model forced consistently with the fields of the same atmospheric data set. The oceanic simulations newly include an updated bathymetry around Antarctica including cavities under the ice shelves, the explicit implementation of the feedback effects of self‐attraction and loading to ocean dynamics as well as a refined harmonic tidal analysis. Comparison to the current release of AOD1B in terms of GRACE‐FO K‐band range‐acceleration pre‐fit residuals, LRI line‐of‐sight gravity differences and band‐pass filtered altimetry data reveals an overall improvement in the representation of the high‐frequency mass variability. Potential benefits of enhancing the temporal resolution remain inconclusive so that the upcoming release 07 will be sampled again every 3 hr.
    Description: Plain Language Summary: Satellite gravimetry missions such as the Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow‐On (GRACE‐FO), which play a vital role in the monitoring of the Earth's mass transports, require a priori background information on the high‐frequency mass variations which can not be resolved by the monthly gravity solutions. The Atmosphere and Ocean De‐Aliasing Level‐1B (AOD1B) data product provides the required background information for non‐tidal high‐frequency mass changes in the atmosphere and oceans. However, the accurate representation of these mass variations remains challenging and deficiencies in the background models have a significant impact on the overall gravity field errors. Thus, we here present three new datasets in preparation for an upcoming release of AOD1B (RL07). The datasets improve over previous releases by incorporating the effects of the self attraction and solid earth deformation caused by anomalous water masses (SAL), an improved representation of the bathymetry and atmospheric forcing around Antarctica, making use of the new ERA5 atmospheric reanalysis as well as an updated estimation and subtraction of atmospherically induced tidal signals. We compare the new data to the previous release of AOD1B using microwave‐ and laser‐ranging data from GRACE‐FO as well as Jason‐3 altimetry data and show a global improvement in the representation of high‐frequency mass changes.
    Description: Key Points: Atmospheric mass variability from ECMWF’s latest global reanalysis ERA5 is discussed. Ocean response from Max‐Planck‐Institute for Meteorology Ocean Model includes feedback of self‐attraction and loading. Applicable for Gravity Recovery and Climate Experiment (GRACE), GRACE Follow‐On, and legacy data from SLR satellites.
    Description: Deutsche Forschungsgemeinschaft, DFG http://dx.doi.org/10.13039/501100001659
    Description: https://doi.org/10.5880/GFZ.1.3.2022.003
    Keywords: ddc:526.7 ; AOD1B RL07 ; GRACE ; ERA5 ; self‐attraction and loading ; satellite gravimetry
    Language: English
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  • 99
    Publication Date: 2023-01-19
    Description: About 10% of Europe's surface area is prone to rapid flooding of rivers confined in valleys. The devastating potential of such floods is exacerbated by the deficits of existing gauging networks, including low station densities and recording frequencies, and lack of information beyond stage height. Here, we use seismic data of the July 2021 Ahrtal flood, Germany, to extract information to complement sparse hydrometric data, and to reconstruct the rapid evolution of this fatal event. We show that a seismic station can deliver essential flood metrics such as magnitude, propagation velocity and debris transport rate. These seismic products provide high resolution insight to the non‐linear flood behavior. We argue that an approach combining distributed low‐cost seismometers with existing seismic stations, can provide important real time data on future catastrophic floods and associated hazards in upland catchments, offering precious response time also in currently ungauged landscapes.
    Description: Plain Language Summary: Rapidly evolving floods are a major hazard for 10% of European landscapes. They are hard to adequately detect and describe by the classic gauge station scheme, but seismic sensors provide a valuable alternative to this difficulty. A seismometer can sense a flood like the devastating one that hit the Ahr valley, Germany, in July 2021 up to 1.5 km away. The seismic footprint of the flood allows to provide information on flood magnitude, velocity and trajectory at sub‐minute resolution and at near real time. We show how this new approach can be utilized for future flood protection.
    Description: Key Points: Seismic sensing of valley confined floods improves classic detection approaches. Near‐real time information on flood magnitude, trajectory, and velocity. Gate keeper seismometer networks can improve flood risk management in Europe.
    Description: GFZ German Research Centre for Geosciences
    Description: Helmholtz Centre Potsdam—GFZ German Research Centre for Geosciences http://dx.doi.org/10.13039/501100010956
    Description: German Research Foundation
    Keywords: ddc:622.1592 ; hazard ; realtime warning ; flash flood ; seismic
    Language: English
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  • 100
    Publication Date: 2023-01-19
    Description: Along ultraslow spreading ridges melt is distributed unequally, but melt focusing guides melt away from amagmatic segments toward volcanic centers. An interplay of tectonism and magmatism is thought to control melt ascent, but the detailed process of melt extraction is not yet understood. We present a detailed image of the seismic velocity structure of the Logachev volcanic center and adjacent region along the Knipovich Ridge. With travel times of P‐ and S‐waves of 3,959 earthquakes we performed a local earthquake tomography. We simultaneously inverted for source locations, velocity structure and the Vp/Vs‐ratio. An extensive low velocity anomaly coincident with high Vp/Vs‐ratios 〉1.9 lies underneath the volcanic center at depths of 10 km below sea level in an aseismic area. More shallow, tightly clustered earthquake swarms connect the anomaly to a shallow anomaly with high Vp/Vs‐ratio beneath the basaltic seafloor. We consider the deep low‐velocity anomaly to represent an area of partial melt from which melts ascent vertically to the surface and northwards into the adjacent segment. By comparing tomographic studies of the Logachev and Southwest Indian Ridge Segment‐8 volcano we conclude that volcanic centers of ultraslow spreading ridges host spatially confined, circular partial melt areas below 10 km depth, in contrast to the shallow extended melt lenses along fast spreading ridges. Lateral feeding over distances of 35 km is possible at orthogonal spreading segments, but limited at the obliquely spreading Knipovich Ridge.
    Description: Plain Language Summary: Mid‐ocean ridges mark the tectonic plate boundaries, where the plates drift apart. Fresh magma rises into the gap and builds new seafloor. The slower the plates drift apart, the less magma is present underneath the ridge. At very slow spreading ridges there is not enough magma to build new seafloor along the entire length of the ridge. Rather, melt is guided toward individual volcanic centers spaced at about 100 km, where melt accumulates and ascents. In our study we try to find melt storage areas and ascent paths of such a volcanic center. With velocities of different seismic wave types from earthquakes we map the velocity structure of the area underneath the major Logachev volcanic center. Lower velocities indicate an area partly including melt at depths of more than 10 km, far deeper than at mid‐ocean ridges with sufficient melt supply. From the deep magma reservoir, many earthquake swarms map the long ascent path of melt to the surface. The interplay of magmatic and tectonic activity is important here. In a comparison with results from another volcanic center, we find that lateral magma feeding is possible in orthogonal spreading, but limited in oblique spreading, as at the Knipovich Ridge.
    Description: Key Points: Active volcanic centers at ultraslow spreading ridges host deeper and more confined partial melt areas than faster spreading ridges. Earthquake swarms delineate melt ascent paths from the partial melt area to the surface. Lateral feeding at shallow depths into subordinate segments is prevented by ridge obliquity.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: ddc:551.22 ; ultraslow spreading ; Knipovich Ridge ; local earthquake tomography ; seismicity ; mid‐ocean ridge ; partial melt area
    Language: English
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