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  • 1
    facet.materialart.
    Unknown
    Reimer, Berlin
    In:  Herausgeberexemplar
    Publication Date: 2024-04-18
    Description: Der Band enthält neben eines Beitrags zum Lebenswerk des Paläontologen Walter Georg Kühne aus Anlass seines 70. Geburtstags eine Reihe von Aufsätzen zu verschiedenen paläontologischen Themen von Angehörigen der geowissenschaftlichen Institute der Freien und Technischen Universität Berlin sowie der Technischen Fachhochschule Berlin.
    Description: commemorativepublication
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläontologie
    Language: German
    Type: doc-type:book
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  • 2
    Publication Date: 2024-04-18
    Description: Ausgehend von der Überlegung, daß sich unterschiedliche Faziesbedingungen nicht nur in sedimentologischen Merkmalen, sondern auch in ingenieurgeologischen Eigenschaften und damit im bodenmechanischen Verhalten widerspiegeln müssen, wird für die Sedimente des Küstenholozäns ein ingenieurgeologisches Ordnungsprinzip auf der Basis bodenmechanischer Kennziffern entwickelt. Für drei Gebiete der südlichen Nordsee (Emden, Wilhelmshaven, Bremerhaven) wird bodenmechanisches Datenmaterial aus eigenen Untersuchungen und aus zahlreichen Baugrundgutachten in das gültige geologisch lithologische Ordnungsschema (BARCKHAUSEN et a l . 1977) eingepaßt und dann auf seine ingenieurgeologische Gruppenstruktur hin untersucht. Von insgesamt 1200 lithofaziell zugeordneten Proben aus dem Untersuchungsschwerpunkt Emden-Krummhörn und den Vergleichsgebieten Wilhelmshaven-Voslapp und Bremerhaven liegen Daten über Korngrößenverteilung, Glühverlust, Porenziffer, Wassergehalt, Wichte, Konsistenzgrenzen, Aktivität, Kohäsion, Reibungswinkel, c -Festigkeit und Steifemoduln von vier Laststufen vor, die mit multivariaten statistischen Methoden gruppiert und korreliert werden…
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:624.151 ; ddc:551.3
    Language: German
    Type: doc-type:book
    Format: 71
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  • 3
    facet.materialart.
    Unknown
    Berlin, Reimer
    In:  SUB Göttingen | ZB 45198:55
    Publication Date: 2024-04-18
    Description: Im zentralen Anti-Atlas wurden die Deformationen im sedimentären Deckgebirge des präkambrischen Kristallin-Aufbruchs des J. Sirwa und angrenzender Grundgebirgs-Blöcke untersucht. Dabei konnten zwei unterschiedliche Deformationsformen erfaßt werden. Als erste Generation entstanden - bisher a l s tektonisch angesehen - in zwei Niveaus frühdiagenetische Deformationsstrukturen (Gleitfalten, Rutschungen und Setzungsstrukturen), die zum Teil sehr große Dimensionen erreichen. A l s Auslöser für diese Verformungen müssen Kompaktionserscheinungen und eine leichte Reliefbildung angenommen werden. Hinzu kam in einzelnen Fällen auch ein übernormaler Porenwasserdruck. Eine vermutlich spätpaläozoische tektonische Deformation hat diese frühen Deformationsstrukturen überprägt. Satelliten- und Luftbild-Interpretationen sowie Geländebeobachtungen zeigen, daß die während der variskischen Orogenese aufgestiegenen Kristall in-Dome an bereits im späten Präkambrium angelegte Bruchsysteme gebunden sind. Darüber hinaus geben die Deformationen im Deckgebirge keine Hinweise auf die Mechanismen der Dom-Aufstiege. Während dieser Aufstiege kam es zu einer weitspannigen Verfaltung der Sedimente des Deckgebirges. Vergleiche zwischen den ursprünglichen Faltenachsen-Richtungen der frühen Deformationsstrukturen und den tektonischen Faltenachsen sowie den Störungssystemen im Grund- und im Deckgebirge zeigen, daß auch das altpaläozoische Deckgebirge von den prakambrisch angelegten Störungssystemen beherrscht wird, wobei in einer frühen Phase der Sedimentation die frühdiagenetischen Deformationsstrukturen an den Störungslinien gebildet wurden. Die gleichen Störungssysteme haben dann im Spätpaläozoikum auch bei der Tektogenese das beherrschende Element dargestellt. Wie an postpaläozoischen Störungen und Kluftbildungen in mio-pliozänen Vulkaniten nachgewiesen werden konnte, sind die alten Störungs-Richtungen bis in jüngste Zeit reaktiviert worden und prägten sich auch bei der im Känozoikum erfolgten Hebung des Anti-Atlas aus.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:551.8 ; Geologie ; Deformation ; Antiatlas
    Language: German
    Type: doc-type:book
    Format: 84
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  • 4
    facet.materialart.
    Unknown
    Berlin: Reimer
    In:  Herausgeberexemplar
    Publication Date: 2024-04-18
    Description: Anatektische Schmelzen haben bei der Entstehung granitischer bis dioritischer Magmen in der Erdkruste eine entscheidende Bedeutung. Die große Tiefe und breite Ausdehnung, in der sich sialische Granitisations-Prozesse vollziehen, bedingen aber auch die Seltenheit ihres Aufschlusses an der Erdoberfläche. An Stelle dieser Übergänge metamorph -〉 magmatisch in situ (ERDMANNSDÖRFFER, 1948) wurden daher stets die wesentlich kleinräumigeren Erscheinungen in Migmatiten untersucht. Man ging dabei von der Voraussetzung aus, daß diese als "Modell Systeme" anzusehen sind (MEHNERT, 1968/71). Die meisten geochemischen Untersuchungen zu diesem Thema berücksichtigten bisher nur die Hauptelemente. Angaben über Spurenelement-Konzentrationen basieren meist nur auf wenigen Einzelanalysen. Als Grundlage der hier vorgelegten Zusammenfassung geochemischer Daten zur Migmatitgenese dienten im wesentlichen die petrologischen Untersuchungen anatektischer Gesteine von MEHNERT und von BÜSCH (Zitate im Text). Diese Basis wurde durch Hinzunahme von neueren Literaturdaten erweitert. Die Analyse einer möglichst großen Anzahl von Einzelproben von Gneisen, Leukosomen und Melanosomen auf Haupt-, Neben- und Spurenelemente und die Berücksichtigung der Auswirkungen der Streuungen erbrachte neue Erkenntnisse…
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:552.4 ; ddc:551.9 ; Geochemie ; Migmatit ; Schwarzwald
    Language: German
    Type: doc-type:book
    Format: 82
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  • 5
    facet.materialart.
    Unknown
    Berlin, Reimer
    In:  Herausgeberexemplar
    Publication Date: 2024-04-18
    Description: Mit Hilfe der Mikrofazies-Analyse wurde die paläogeographische Entwicklung des Sedimentationsraums der obertriassischen Gesteinsabfolge im Bereich der Vorarlberger Kalkalpen rekonstruiert. Die Entwicklung begann mit der Ausbildung eines weiträumigen, sehr flachen Schelfgebietes im Nor (Hauptdolomit). Durch stärkere, aber nicht einheitliche Absenkung im Oberen Hauptdolomit und im Plattenkalk-Niveau bildete sich ein Relief aus. Die hier einsetzende Schüttung terrigenen Materials erreichte während der Ablagerung der Kössener Schichten ihren Höhepunkt. Im obersten Rhät ließ diese Schüttung nach und das terrigene Material konnte nur noch gelegentlich in die flachen Regionen gelangen, die mit dem Aufbau des Rhätoliaskalks entstanden waren. Die normale Ausbildung der Kössener Schichten ist im allgemeinen durch eine mehrere Meter mächtige Kalkbank, in die kleine Biol ithit-Linsen eingelagert sind, unterbrochen, durch die sie sich in eine Untere und Obere Wechselfolge gliedern lassen. Ihre Entstehung wurde wahrscheinlich durch eine kurzfristig geringere Absenkungsrate begünstigt. Die Entwicklung des Rhätoliaskalks setzte hier nicht gleichzeitig ein. Im nördlichen Teil begann sie sehr früh. Durch die hohe biogene Karbonat-Produktion, weitgehend in Form von Biohermen, und die dadurch bedingte starke Schüttung bioklastischen Materials dehnte sich die Rhätoliaskalk-Ausbildung nach Süden aus. Mit der entstehenden flachen Plattform bildete sich der gebankte Rhätoliaskalk aus, ein Wechsel zwischen massigen Riffschuttkalken und Einlagerungen terrigenen Materials. Zum Abschluß dieser Entwicklung kommt es zu einer kleinräumigen Fazies-Verzahnung zwischen Oolithen, Lumachellen und Algen-Stromatolithen. Im Gegensatz zu anderen Gebieten der Nördlichen Kalkalpen, wo eine Gliederung des Ablagerungsraumes in einen Beckenbereich und einen Rhätoliaskalk-Riffgürtels gegeben ist, liegt hier ein mehr oder weniger flaches Schelfgebiet vor. Eine Ausnahme stellt nur die Zürser Schwelle dar. Hierbei handelt es sich um ein die gesamte Zeit über persistierendes Hochgebiet. Die Gesteinsausbildung entspricht durchgehend der des Hauptdolomits. Im Vergleich zu anderen Bereichen des Sedimentationsraumes der bearbeiteten Gesteinsserien kann zusammenfassend gesagt werden, daß wir uns im Gebiet der Vorarlberger Kalkalpen zur Zeit der Obertrias am westlichen Ende der sich öffnenden Tethys befanden, und daß der Ablagerungsraum hier die nördliche Zone des zu dieser Zeit noch bestehenden oberostalpinen, epikontinentalen Flachmeer-Bereichs representiert.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:554.3 ; Rätium ; Vorarlberg
    Language: German
    Type: doc-type:book
    Format: 91
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  • 6
    Publication Date: 2024-04-18
    Description: Das Untersuchungsgebiet der vorliegenden Arbeit ist der westliche und nordwestliche Rand der Adriaplatte bis in den Bereich der Vortiefen nördlich und östlich des Apennins sowie der Kontaktbereich der Adriaplatte zur europäischen Platte im Westalpenbogen und im Gebiet des Ligurischen Meeres. Für dieses Areal werden Aufbau und Struktur der Erdkruste beschrieben.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:551.13 ; Geophysik ; Erdkruste ; Geothermische Anomalie
    Language: German
    Type: doc-type:book
    Format: 122
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  • 7
    facet.materialart.
    Unknown
    Reimer
    In:  Herausgeberexemplar
    Publication Date: 2024-04-18
    Description: Die Erdkruste und der obere Erdmantel Westeuropas sind in den letzten 30 Jahren intensiv durch refraktionsseismische Messungen erforscht worden. Die Daten und Ergebnisse sind in zahlreichen Arbeiten veröffentlicht worden. Abgesehen von einigen regionalen Zusammenfassungen fehlt bislang jedoch eine überregionale Gesamtdarstellung dieses umfangreichen Materials. Es ist das Ziel dieser Arbeit, die in zahlreichen Publikationen verstreuten Einzeldaten und Ergebnisse zu sammeln, unter einheitlichen Gesichtspunkten auszuwerten und die Ergebnisse in einer Reihe von Karten darzustellen. Aus verschiedenen Publikationen, Forschungsberichten und den Archiven des geophysikalischen Institutes der Freien Universität Berlin wurden insgesamt 360 Sei smogrammon tagen in reduzierter Form (V = 6 km/s) gesammelt.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:554 ; Seismic refraction method
    Language: German
    Type: doc-type:book
    Format: 142
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  • 8
    facet.materialart.
    Unknown
    Reimer
    In:  Herausgeberexemplar
    Publication Date: 2024-04-18
    Description: Grundlage der seismologischen Untersuchungen in Irian Jaya bilden die von nationalen und internationalen Erdbebendiensten im Zeitraum 1900 - 1980 publizierten Erdbebendaten, ergänzt durch eigene Untersuchungen in Indonesien. Erfaßt und ausgewertet wurden 1818 Erdbeben, deren Hypozentren und Herdzeit hinreichend bekannt waren.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:551.22 ; ddc:551.8 ; Erdbeben ; Tektonik ; Seismologie
    Language: German
    Type: doc-type:book
    Format: 116
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  • 9
    facet.materialart.
    Unknown
    Reimer
    In:  Herausgeberexemplar
    Publication Date: 2024-04-18
    Description: In der vorliegenden Arbeit wurde ein numerisches Verfahren für die zweidimensionale Simulation stationärer Strömung in porösen Medien entwickelt. Dabei können Modelle mit anisotroper Permeabilität und Wärmeleitfähigkeit ebenso berechnet werden wie Modelle in geneigten und gekrümmten Gebieten. Das Verfahren basiert auf einer Finite-Differenzen-Methode mit einem Schema 2. Ordnung (Il'in-Schema). Für das nichtlineare Gleichungssystem wird ein Iterationsansatz mit einer Art Mehrgittermethode verwendet. Um den großen Anwendungsbereich des entwickelten Verfahrens zu demonstrieren, wird es auf zwei unterschiedliche Fragestellungen aus der Hydrothermik und der Schneemetamorphose angewendet.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:550 ; Wärmeübertragung ; Schnee ; Porosität
    Language: German
    Type: doc-type:book
    Format: 118
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  • 10
    facet.materialart.
    Unknown
    Reimer
    In:  Herausgeberexemplar
    Publication Date: 2024-04-18
    Description: Die Bestimmung der Temperaturverteilung in der Erdkruste und im oberen Erdmantel ist von großer Bedeutung für die Behandlung geotektonischer Probleme. In dieser Arbeit wird die Temperaturverteilung längs eines Profils in Süditalien untersucht, das vom Südadriatischen Meer durch Kalabrien zum Tyrrhenischen Meer verläuft. Grundlage für diese Untersuchung bilden eine Anzahl publizierter Wärmeflußwerte und ein refraktionsseismisches Profil. Längs des ausgewählten geothermischen Profils sind die Temperatur-Tiefen-Funktionen für zwei Modelle der Wärmeproduktionsverteilung, Schichten- und Exponential-Modell , für den stationären Zustand berechnet worden.
    Description: The determination of temperature distribution in the earth's crust and upper mantle is of great importance for geotectonic problems. The temperature distribution is discussed along a profile in southern Italy, which runs from the Adriatic to the Tyrrhenian Seas. This study is based on published heat flow values and seismic refraction data. The temperature-depth-functions are calculated for layer and exponential models for the heat production assuming a stationary state.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:550 ; Geophysik ; Geothermie
    Language: German
    Type: doc-type:book
    Format: 56
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  • 11
    Publication Date: 2024-04-18
    Description: Die vorliegende Arbeit beschäftigt sich mit Strati graphischen, paläontologischen und paläogeographischen Untersuchungen im Jura und in der Kreide des tansanischen Küstenstreifens im Hinterland von Dar-es-Salaam und Bagamoyo. Die Sedimentgesteine werden in sechs lithostratigraphische Einheiten gegliedert, von denen vier neu aufgestellt werden: Ngerengere-Formation (bisher Ngerengere-Sandstein; Unterjura-tiefes Aalenium), Ruvu-Formation (bisher Ruvu-Schichten; Mittel aal enium-Oberaaleni um), Lugoba- Formation (Bajocium-?Bathonium) , Malivundo-Formation (Callovium-Mitteloxfordium), Magindu -Formation (Callovium) und Chalinze-Formation (Unterkreide). Sieben Profile des Jura und der Kreide werden einzeln beschrieben und ihr Makro- sowie Mikrofossilinhalt angegeben. Mit Ammoniten werden in der Ruvu -Formation zwei biostratigraphische Zonen des Mittel- und Oberaalenium festgestellt (Murehisonae- und Concavum-Zone). In der Malivundo-Formation werden aufgrund von Ammoniten drei Zonen (Athleta-Lamberti- , Mariae-Cordatum und Transversarium-Zone} nachgewiesen. Der höchste Teil der Chalinze-Formation wird mit planktonischen Foraminiferen in die Globigerinelloides algerianus-Zone des Oberaptium gestellt. Korrelationen des Jura im Untersuchungsgebiet mit anderen Gebieten innerhalb Tansanias sowie mit anderen Gebieten in der indo-madagassischen Provinz werden durchgeführt. Dreiundzwanzig Ammonitenarten (sechs Familien) aus der Ruvu-, Malivundo- und Magindu-Formation sowie siebzehn Foraminiferenarten (sechs Oberfamilien), die aus der Malivundo- und Chalinze-Formation stammen, werden systematisch beschrieben. Fazies, Ablagerungsbedingungen und Tektonik werden diskutiert. Im Mittelaalenium-Oberaalenium, weiter nördlich erst im Bajocium erfolgt die Transgression nach W auf fluviatile Sedimente der Ngerengere-Formation bzw. auf das Kristallin. Im Hangenden des Oxfordium setzt mit erneuter Riffbildung eine regressive Phase im höheren Oberjura ein. Erst mit der Unterkreide erfolgt mit der Chalinze-Formation eine erneute Transgression. Die paläobiogeographischen Beziehungen der Ammoniten zu anderen Gebieten in der indo-madagassischen Provinz, zu Europa und Südamerika werden aufgezeigt. Unter Berücksichtigung sämtlicher bisher bekannter Fundorte der Mayaitiden-Gattungen ergibt sich, daß sie hauptsächlich auf die indo-madagassische Provinz beschränkt sind.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:556 ; ddc:560 ; Jura ; Kreide ; Daressalam ; Bagamojo
    Language: German
    Type: doc-type:book
    Format: 77
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  • 12
    Publication Date: 2024-04-18
    Description: VORWORT ... 1 ; INHALTSVERZEICHNIS ... 2 ; 1 PÖHLMANN, G.: Basiskarten arider Gebiete ... 3 ; 2 MEISSNER, B.: Topographische Interpretation von Fernerkundungsdaten für "Basiskarten zur thematischen Kartierung arider Gebiete" ... 57 ; 3 MEISSNER, B. & RIPKE, U. : Luft- und Satellitenbild-Interpretation für die Karte "MUT 1 : 100 000"... 69 ; 4 KRAMER, G.: Topographische Ergänzungsmessungen ... 85 ; 5 RIPKE, U.: Die Herstellung des Kartenblattes MUT 1 : 100 000 ... 97 ; 6 ZIRN, V.: Höhenlinienstudie South Bir Tarfawi ... 105 ;
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:526 ; Thematische Kartografie ; Trockengebiet ; Trockengebiet ; Kartierung
    Language: German
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  • 13
    Publication Date: 2024-04-18
    Description: Einer Anregung des 11. Arbeitskurses Niederdollendorf folgend, wurde eine Methode der Bearbeitung farbiger Originale kartographischer Landschaftsdarstellung entwickelt und erprobt. Eine erste Bestandsaufnahme hatte einen Bedarf an solchen Darstellungen bestätigt; geeignete Techniken stehen zur Verfügung, es fehlt jedoch eine lern- und lehrbare Methode der Bearbeitung, die unabhängig von der Person des Bearbeiters vergleichbare Ergebnisse liefert. Hier wurde nun ein in der thematischen Kartographie als Anleitung zu planmäßigen Vorgehen bewährtes System von Arbeitsschritten mit einigen Modifikationen als Richtlinie für die Bearbeitung von Landschaftskarten eingesetzt. Nicht zuletzt wird die Arbeitsweise von den verfügbaren Unterlagen beeinflußt und entweder der Ableitung topographischer Folgemaßstabskarten oder der freien Bearbeitung thematischer Karten entsprechen.
    Description: According to a suggestion made by the 11th study group of Niederdollendorf a method of how to treat coloured originals of cartographic landscape representation has been developed and testet. A first stocktaking had confirmed the demand for such types of representation; although suitable techniques are available, a learnable and teachable method of treatment is needed which provides comparable results independent of the person incharge. In this case a slightly modified system of working steps has been used as a guideline for the treatment of maps which is a time-tested instruction for systematic procedure in thematic cartography. This method is not least influenced by the available records, corresponding either to a derivation of topographic maps on a consecutive scale or to the free treatment of thematic maps.
    Description: PUHLMANN, G.: Eine Methode der Bearbeitung farbiger Originale kartographischer Landschaftsdarstellung ... 5 ; KOCHLER, J.: "Landschaften" in China und die Präzisierung dieser Kategorie in verschiedenen Typologien zur Gliederung des chinesischen Territoriums ... 13 ; STRAUB, W.: Eine Vegetationskarte der Volksrepublik China ... 23 ; MERTINS, M.: Eine Landschaftskarte der Volksrepublik China ... 71 ; BETKE, D. : Anmerkungen zu zwei kartographischen Neuerscheinungen zur Landnutzung und Vegetation der VR China ... 123 ;
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:526 ; ddc:555 ; Landschaftskartierung ; Kartografie ; China
    Language: German
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  • 14
    Publication Date: 2024-04-18
    Description: MEISSNER, B.: Fernerkundung bei der Grünplanung für die Stadtregion Berlin (West) ... 5 ; FIETZ, M. & MEISSNER, B.: Zur Auswertung von Color-Infrarot-Luftbildem (Berlin/West 1979) bei der Vegetationskartierung ... 23 ; FÖRSTER, U.: Vitalitätsbestimmung von Straßenbäumen. - Erfahrungen und Ergebnisse der Color-Infrarot-Bef 1 iegung in Berlin (West) 1979 ... 43 ; FIETZ, M.: Lebensbedingungen von Straßenbäumen in Berlin-Neukölln ... 53 ; BALTSCHUN, M. : Botanischer Garten - Karte der Gehölze - 1 : 1250 ... 65 ; BORYS, 6.: Karte zum Straßenbaumkataster - Berlin (West) - 1 : 2000 ... 101 ; ZEUNERT, C.: Karte zur Grünflächenplanung Berlin (West) - 1 : 4000 ... 121 ; MEISSNER, B.: Grünverteilung in Berlin (West) 1 : l0 000, eine Inventur - Bestandsaufnahme städtischer Vegetation mit Hilfe von reprotechnischen Mitteln und stark limitierter Bildinterpretation durch Color-Infrarot-Luftbilder... 141 ; MEISSNER, B., DOBBRICK, K. & MUNIER, C.: Satelliten-Fernerkundungs-Daten für städtische Grünübersicht? - Zur Einsatzfähigkeit von multispektralen Landsat-Scanner-Daten für jährliche Übersichts-Inventuren des Stadtgrüns von Berlin (West) ... 147 ; ANHANG ... 153 ;
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:526 ; Grünfläche ; Straßenbau ; Luftbild ; Kartografie
    Language: German
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  • 15
    Publication Date: 2024-04-18
    Description: Ausgangspunkt der Untersuchungen war die Erfordernis, die Standsicherheitsverhältnisse des Naturdenkmals Teufelstisch im Hinblick auf die Gefährdung seiner Besucher zu überprüfen. Für diese Beurteilung war es notwendig, das geometrisch komplizierte Gebilde meßtechnisch exakt zu erfassen; dies wurde durch die Photogrammetrie mit der erforderlichen Genauigkeit erreicht. Außerdem wurden Untersuchungen zur geologisch-petrographischen Beschaffenheit, den geotechnischen Eigenschaften der Gesteine, der Abwitterungsrate und den statischen Verhältnissen durchgeführt. Als Ergebnis läßt sich feststellen, daß in den nächsten Jahrzehnte neine ausreichende Standsicherheit des Teufelstisches gegeben und aufgrund des Verwitterungsfortschrittes keine wesentliche Änderung dieser Situation zu erwarten ist.
    Description: Abstract: Starting point of the investigations was the requirement to study fhe stability of the natural monument "Teufelstisch" (near Hinterweidenthal, SW-Germany) concerning the endangering of its visitors. It was necessary to record the complicated geometric shape; this object was achieved with the required precision by means of photogrammetry. Furthermore investigations were carried through according the geological-petrographical structure, the geotechnical characteristics, the rate of weathering and the statics. As a result the stability of the "Teufelstisch" can be guaranteed for some decades. Looking to the rate of weathering no important change of the present situation can be expected.
    Description: 1. Einleitung 2. Untersuchungsobjekt und Standort 3. Geologischer Aufbau 4. Petrographie 5. Photogrammetrische Vermessung 6. Abmessungen des Teufelstisches 7.Gesteinseigenschaften 8. Überlegungen zur Verwitterungsrate 9. Standsicherheitsbeurteilung Schriften
    Description: research
    Keywords: ddc:554.3 ; Buntsandstein ; Pfalz ; Verwitterung ; Naturdenkmal ; Petrographie ; Standsicherheit
    Language: German
    Type: doc-type:article , publishedVersion
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  • 16
    facet.materialart.
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    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 34 no. 6, pp. 175-175
    Publication Date: 2024-04-18
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 17
    facet.materialart.
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    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 55 no. 3, pp. 300-300
    Publication Date: 2024-04-18
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 18
    facet.materialart.
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    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 34 no. 6, pp. 174-174
    Publication Date: 2024-04-18
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 19
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    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 34 no. 6, pp. 175-175
    Publication Date: 2024-04-18
    Repository Name: National Museum of Natural History, Netherlands
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  • 20
    Publication Date: 2024-04-18
    Description: Science makes progress through a constant process of re-evaluation. Revision and error correction are inevitable and generally healthy for the advancement of science. In biodiversity literature, re-evaluation of earlier work can lead to new conclusions, such as a revised taxonomic determination. When significant errors are discovered, conscientious authors may correct the record by publishing an erratum or corrigendum.
    Repository Name: National Museum of Natural History, Netherlands
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  • 21
    Publication Date: 2024-04-18
    Description: We document aggregations of an undescribed benthic solitary tunicate of the family Pyuridae from the Arabian Sea. This new genus was found forming dense thickets in shallow rocky substrates around Masirah Island and the Dhofar area in Oman. Such aggregations of tunicates have not been reported before from coral reefs in the Indo-West Pacific region and the Atlantic. This observation contributes to our understanding of the ecology and biogeography of ascidians, setting the stage for a comprehensive species description and in-depth analysis of this species.
    Keywords: Indian Ocean ; Masirah Island ; Ascidiacea ; Oman ; phylogeny ; anatomy
    Repository Name: National Museum of Natural History, Netherlands
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  • 22
    Publication Date: 2024-04-18
    Description: Using CO1 sequence analysis, we investigated the relationships of Western Palearctic and Nearctic Cotesia that spin aggregated cocoons in the shape of a ball, and as adults are morphologically very similar. The analysis included the conceptual taxa C. tibialis, C. ofella, C. vanessae, C. ruficrus, C. xylina and C. yakutatensis, as well as the newly described species C. trivaliae sp. nov. The examined specimens of C. tibialis, C. ofella, C. vanessae, C. ruficrus and C. trivaliae sp. nov. were collected in several European countries, and C. xylina and C. yakutatensis in Canada and the USA. Molecular analyses showed that C. ruficrus is not closely related to the other studied taxa. Based on the genetic distances as well as biology and morphology, C. vanessae and C. ofella are confirmed as solid taxa. The species C. yakutatensis comprises two entities. Having 8 haplotypes, C. tibialis also emerges as a species complex, divided into two clusters. With 26 detected haplotypes, C. xylina shows the highest diversity, being composed of three segregates. The conceptual species C. tibialis, C. xylina and C. yakutatensis seem to be species complexes containing several candidates for recognition as distinct species. One from the European C. tibialis complex is here described as new, and the impediments to be overcome before the description of further species are outlined
    Keywords: DNA barcoding ; genetic distance ; hosts ; species aggregates
    Repository Name: National Museum of Natural History, Netherlands
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  • 23
    Publication Date: 2024-04-18
    Description: This study provides a new methodology for the rapid analysis of numerous venom samples in an automated fashion. Here, we use LC-MS (Liquid Chromatography–Mass Spectrometry) for venom separation and toxin analysis at the accurate mass level combined with new in-house written bioinformatic scripts to obtain high-throughput results. This analytical methodology was validated using 31 venoms from all members of a monophyletic clade of Australian elapids: brown snakes (Pseudonaja spp.) and taipans (Oxyuranus spp.). In a previous study, we revealed extensive venom variation within this clade, but the data was manually processed and MS peaks were integrated into a time-consuming and labour-intensive approach. By comparing the manual approach to our new automated approach, we now present a faster and more efficient pipeline for analysing venom variation. Pooled venom separations with post-column toxin fractionations were performed for subsequent high-throughput venomics to obtain toxin IDs correlating to accurate masses for all fractionated toxins. This workflow adds another dimension to the field of venom analysis by providing opportunities to rapidly perform in-depth studies on venom variation. Our pipeline opens new possibilities for studying animal venoms as evolutionary model systems and investigating venom variation to aid in the development of better antivenoms.
    Keywords: LC-MS ; snake venom ; high throughput ; data analysis
    Repository Name: National Museum of Natural History, Netherlands
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  • 24
    Publication Date: 2024-04-18
    Repository Name: National Museum of Natural History, Netherlands
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  • 25
    Publication Date: 2024-04-18
    Keywords: Ecology ; Ecology ; Evolution ; Behavior and Systematics
    Repository Name: National Museum of Natural History, Netherlands
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  • 26
    Publication Date: 2024-04-18
    Description: Since the introduction of non-native rodents to the Caribbean region, these invaders have successfully occupied many, if not most, islands where they pose tremendous threats to native biodiversity and ecosystems. The objective of our study was to conduct a preliminary assessment of the relative abundance of invasive alien rodents in different vegetation types on the small Caribbean island of St. Eustatius, which has no native rodent species. We used tracking tunnels (baited ink cards placed in tunnels to identify the prints of animals lured to the card) to determine the presence of rodent species. We collected data in 25 x 25 m (n = 13) and 5 x 5m (n = 130) plots to determine whether elevation, number of tree species, canopy cover or other microhabitat components were correlated with rodent relative abundance. Invasive rodents are present in varying relative abundances in rural areas on St. Eustatius. House mice (Mus musculus) were not recorded inside the terrestrial protected areas, whereas black rats (Rattus rattus) were detected in all elevations and all but one vegetation type sampled. We determined significant correlations between some of the habitat characteristics, especially elevation, canopy height, leaf litter cover and number of tree species, which showed significant collinearity with 27 of 45 pairwise comparisons. There was a significant correlation between rodent relative abundance and the number of tree species, but not between elevation, number of living trees, number of shrubs, rainfall, canopy cover, canopy height, leaf litter cover, leaf litter depth, or slope. There was a significant difference within vegetation types for the frequency of traps containing rat versus mouse tracks. Our study was impacted by two major hurricanes in September 2017.
    Keywords: Nature and Landscape Conservation ; Ecology ; Ecology ; Evolution ; Behavior and Systematics
    Repository Name: National Museum of Natural History, Netherlands
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  • 27
    Publication Date: 2024-04-18
    Description: Specimen data in taxonomic literature are among the highest quality primary biodiversity data. Innovative cybertaxonomic journals are using workflows that maintain data structure and disseminate electronic content to aggregators and other users; such structure is lost in traditional taxonomic publishing. Legacy taxonomic literature is a vast repository of knowledge about biodiversity. Currently, access to that resource is cumbersome, especially for non-specialist data consumers. Markup is a mechanism that makes this content more accessible, and is especially suited to machine analysis. Fine-grained XML (Extensible Markup Language) markup was applied to all (37) open-access articles published in the journal Zootaxa containing treatments on spiders (Order: Araneae). The markup approach was optimized to extract primary specimen data from legacy publications. These data were combined with data from articles containing treatments on spiders published in Biodiversity Data Journal where XML structure is part of the routine publication process. A series of charts was developed to visualize the content of specimen data in XML-tagged taxonomic treatments, either singly or in aggregate. The data can be filtered by several fields (including journal, taxon, institutional collection, collecting country, collector, author, article and treatment) to query particular aspects of the data. We demonstrate here that XML markup using GoldenGATE can address the challenge presented by unstructured legacy data, can extract structured primary biodiversity data which can be aggregated with and jointly queried with data from other Darwin Core-compatible sources, and show how visualization of these data can communicate key information contained in biodiversity literature. We complement recent studies on aspects of biodiversity knowledge using XML structured data to explore 1) the time lag between species discovry and description, and 2) the prevelence of rarity in species descriptions.
    Keywords: Araneae ; Biodiversity informatics ; Data mining ; Open access ; Spiders ; Taxonomy ; XML ; markup
    Repository Name: National Museum of Natural History, Netherlands
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  • 28
    Publication Date: 2024-04-18
    Description: The vast extent of the Amazon Basin has historically restricted the study of its tree communities to the local and regional scales. Here, we provide empirical data on the commonness, rarity, and richness of lowland tree species across the entire Amazon Basin and Guiana Shield (Amazonia), collected in 1170 tree plots in all major forest types. Extrapolations suggest that Amazonia harbors roughly 16,000 tree species, of which just 227 (1.4%) account for half of all trees. Most of these are habitat specialists and only dominant in one or two regions of the basin. We discuss some implications of the finding that a small group of species—less diverse than the North American tree flora—accounts for half of the world’s most diverse tree community.
    Keywords: hyperdominance ; Amazonia ; Amazon Basin ; Guiana Shield ; trees ; commonness ; rarity ; richness ; tree species
    Repository Name: National Museum of Natural History, Netherlands
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  • 29
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    Unknown
    In:  Persoonia - Molecular Phylogeny and Evolution of Fungi vol. 25 no. 1, pp. 117-159
    Publication Date: 2024-04-18
    Repository Name: National Museum of Natural History, Netherlands
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  • 30
    facet.materialart.
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    In:  Persoonia - Molecular Phylogeny and Evolution of Fungi vol. 24 no. 1, pp. 127-139
    Publication Date: 2024-04-18
    Repository Name: National Museum of Natural History, Netherlands
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  • 31
    Publication Date: 2024-04-18
    Description: Background Males of Opadometa are difficult to associate with conspecific females, and sex-matching errors may persist in the taxonomic literature. Recommended best practices for definitive sex matching in this genus suggest finding a male in the web of a female, or better yet, mating pairs. New information A male Opadometa was observed hanging on a frame line of the web of a female Opadometa sarawakensis, a species for which the male was previously undescribed. This occurred during a tropical ecology field course held at the Danau Girang Field Centre in Sabah, Malaysia. A taxonomic description was completed as a course activity.
    Keywords: Ecology ; Ecology ; Evolution ; Behavior and Systematics
    Repository Name: National Museum of Natural History, Netherlands
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  • 32
    Publication Date: 2024-04-18
    Description: The Caspian Sea is an evolutionary island whose rich and endemic fauna have evolved in partial isolation over the past two million years. Baseline studies of pre-20th Century communities are needed in order to assess the severity of the current Caspian biodiversity crisis, which mostly involves invasive species. An inventory of late Holocene shelly assemblages (c. 2000–2500 cal yr BP) from outcrops in and around Great Turali Lake (Dagestan, Russia) shows a diverse nearshore community consisting of 24 endemic Caspian species, two invasive species and two Caspian native species that lived in a shallow embayment with mesohaline salinities of circa 5–13 psu (parts per thousands). This pre-crisis Holocene Caspian mollusc community serves as a baseline against which modern mollusc diversity measurements can be evaluated. Examination of faunas from similar environments living today and in the past illustrates the dramatic changes in nearshore communities during the 20th Century. Our study identifies a habitat that may have served as a refuge, but that is currently under threat from invasive species. The severity of the Caspian biodiversity crisis is comparable with other well-known biodiversity crises in semi-isolated ecosystems such as the cichlid fish communities of Lake Victoria, Africa.
    Keywords: Biodiversity crisis ; Mollusc assemblages ; Pontocaspian biota ; Invasive species ; Endemic species ; Marie Skłodowska-Curie Actions ; Action: H2020-MSCA-ITN-2014 ; PRIDE ; Grant agreement no: 642973
    Repository Name: National Museum of Natural History, Netherlands
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  • 33
    Publication Date: 2024-04-18
    Description: This paper investigates Bostryx species from Peru, which show variation in shells shape and are partly carinated, using both ecological and molecular data. The study area is situated in a valley at the western side of the Andes, with a total length of 25 km and an altitudinal range of almost 1,140 m, but focuses on two localities: El Infernillo at ca. 3,350 m and Tambo de Viso at ca. 2,700 m. The morphological variation of the species presents a rather complex picture that cannot completely be resolved by ecological data alone. Molecular data points to three taxa, two of which are variable in shell shape and each restricted to one of the localities mentioned; the third taxon is constant in shell shape and occurs over a large range of the study area. The species originally described as Bostryx multiconspectus Breure, 2008 and B. primigenius Breure, 2008 are redefined as a result.
    Keywords: carination ; ecology ; taxonomy ; Peru ; Orthalicoidea
    Repository Name: National Museum of Natural History, Netherlands
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  • 34
    Publication Date: 2024-04-18
    Description: Automatic detection and classification of animal sounds has many applications in biodiversity monitoring and animal behavior. In the past twenty years, the volume of digitised wildlife sound available has massively increased, and automatic classification through deep learning now shows strong results. However, bioacoustics is not a single task but a vast range of small-scale tasks (such as individual ID, call type, emotional indication) with wide variety in data characteristics, and most bioacoustic tasks do not come with strongly-labelled training data. The standard paradigm of supervised learning, focussed on a single large-scale dataset and/or a generic pretrained algorithm, is insufficient. In this work we recast bioacoustic sound event detection within the AI framework of few-shot learning. We adapt this framework to sound event detection, such that a system can be given the annotated start/end times of as few as 5 events, and can then detect events in long-duration audio—even when the sound category was not known at the time of algorithm training. We introduce a collection of open datasets designed to strongly test a system’s ability to perform few-shot sound event detections, and we present the results of a public contest to address the task. Our analysis shows that prototypical networks are a very common used strategy and they perform well when enhanced with adaptations for general characteristics of animal sounds. However, systems with high time resolution capabilities perform the best in this challenge. We demonstrate that widely-varying sound event durations are an important factor in performance, as well as nonstationarity, i.e. gradual changes in conditions throughout the duration of a recording. For fine-grained bioacoustic recognition tasks without massive annotated training data, our analysis demonstrate that few-shot sound event detection is a powerful new method, strongly outperforming traditional signal-processing detection methods in the fully automated scenario.
    Keywords: Bioacoustics ; Deep learning ; Event detection ; Few-shot learning
    Repository Name: National Museum of Natural History, Netherlands
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  • 35
    Publication Date: 2024-04-18
    Description: We document the benthic ctenophores Coeloplana sp. and Vallicula multiformis from Oman, extending their geographic range. A new Coeloplana species was found forming aggregations on gorgonians of two octocoral host genera, Melithaea and Euplexaura, representing associations previously unknown to occur in the Indo-West Pacific region. Our findings also illustrate the concurrent presence of the ectocommensal ophiuroid Ophiothela mirabilis, which adversely affects other Coeloplana species in the tropical West Atlantic, where it is considered invasive. This exploration contributes to our understanding of the biogeography, species distribution, and ectosymbiotic associations of these genera, setting the stage for a comprehensive species description and in-depth analysis of host relationships in future studies.
    Keywords: Ctenophora ; Octocorallia ; Arabian Sea ; Platyctenida ; Oman ; Masirah Island ; ectosymbiotic
    Repository Name: National Museum of Natural History, Netherlands
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  • 36
    Publication Date: 2024-04-18
    Description: The Caspian Sea has been a highly dynamic environment throughout the Quaternary and witnessed major oscillations in lake level, which were associated with changes in salinity and habitat availability. Such environmental pressures are considered to drive strong phylogeographic structures in species by forcing populations into suitable refugia. However, little is actually known on the effect of lake-level fluctuations in the Caspian Sea on its aquatic biota. We compared the phylogeographic patterns of the aquatic Neritidae snail genus Theodoxus across the Pontocaspian region with refugial populations in southern Iran. Three gene fragments were used to determine relationships and divergence times between the sampled populations in both groups. A dated phylogeny and statistical haplotype networks were generated in conjunction with the analyses of molecular variance and calculations of isolation by distance using distance-based redundancy analyses. Extended Bayesian skyline plots were constructed to assess demographic history. Compared with the southern Iranian populations, we found little phylogeographic structure for the Pontocaspian Theodoxus group, with more recent diversification, homogeneity of haplotypes across the Pontocaspian region and a relatively stable demographic history since the Middle Pleistocene. Our results argue against a strong influence of Caspian Sea low stands on the population structure post the early Pleistocene, whereas high stands may have increased the dispersal possibilities and homogenization of haplotypes across the Pontocaspian region during this time. However, during the early Pleistocene, a more dramatic low stand in the Caspian Sea, around a million years ago, may have caused the reduction in Theodoxus diversity to a single lineage in the region. In addition, our results provide new insights into Theodoxus taxonomy and outlooks for regional conservation.
    Keywords: ancient lakes ; Pontocaspian ; lake-level fluctuations ; salinity ; molluscs ; Marie Skłodowska-Curie Actions ; Action: H2020-MSCA-ITN-2014 ; PRIDE ; Grant agreement no: 642973
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  • 37
    Publication Date: 2024-04-18
    Description: Understanding and reversing biodiversity decline in the Anthropocene requires robust data on species taxonomic identity, distribution, ecology, and population trends. Data deficits hinder biodiversity assessments and conservation, and despite major advances over the past few decades, our understanding of bee diversity, decline and distribution in Europe is still hampered by such data shortfalls. Using a unique digital dataset of wild bee occurrence and ecology, we identify seven critical shortfalls which are an absence of knowledge on geographic distributions, (functional) trait variation, population dynamics, evolutionary relationships, biotic interactions, species identity, and tolerance to abiotic conditions. We describe “BeeFall,” an interactive online Shiny app tool, which visualizes these shortfalls and highlights missing data. We also define a new impediment, the Keartonian Impediment, which addresses an absence of high-quality in situ photos and illustrations with diagnostic characteristics and directly affects the outlined shortfalls. Shortfalls are highly correlated at both the provincial and national scales, identifying key areas in Europe where knowledge gaps can be filled. This work provides an important first step towards the long-term goal to mobilize and aggregate European wild bee data into a multiscale, easy access, shareable, and updatable database which can inform research, practice, and policy actions for the conservation of wild bees.
    Keywords: Knowledge gaps ; Big data ; Online tool ; Biodiversity decline ; Citizen science ; Biodiversity monitoring
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  • 38
    Publication Date: 2024-04-18
    Description: Background During a study on the outdoor floating leaf blade production of Nymphoides peltata (S.G. Gmel.) O. Kuntze (Fringed Water Lily), initial leaf blade decomposition was studied by simultaneously measuring infected, damaged and lost area of floating leaf blades. Methods Data on initial decomposition over time were collected for all leaves during one growth season in four plots: two in outdoor mesocosms and two in an oxbow lake. Each leaf was tagged uniquely upon appearance in a plot. The vegetation in the mesocosms differed with respect to plant species, one contained a monoculture of N. peltata and the other N. peltata associated with Glyceria fluitans (L.) R. Br. and G. maxima (Hartm.) Holmb. The lake plots were situated within a monospecific N. peltata stand, differing in depth and position within the stand. Leaf length, visually estimated percentages of damaged area for each damage type, and decay of the tagged leaves were recorded bi-weekly. When the leaf blades sunk under the water surface or disappeared completely, they were no longer followed. Under water the leaves decayed and were consumed by snails completely, so contributing to the detritus food chain. Results The observed causes of damage on floating leaves were consumption and/or damage by waterbirds (Fulica atra), pond snails, caterpillars (Elophila nymphaeata, Cataclysta lemnata), chironomid larvae (Cricotopus trifasciatus), infection by a phytopathogenic fungus (Septoria villarsiae), senescence by autolysis, and microbial decay. Successional changes in causes of leaf decomposition and impacts of different causes are discussed.
    Keywords: Enclosure ; Herbivores ; Laminae ; Mesocosm ; Nymphaeid growth form ; Senescence ; Succession decomposition causes
    Repository Name: National Museum of Natural History, Netherlands
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  • 39
    Publication Date: 2024-04-18
    Description: Ocean color remote sensing has been used for more than 2 decades to estimate primary productivity. Approaches have also been developed to disentangle phytoplankton community structure based on spectral data from space, in particular when combined with in situ measurements of photosynthetic pigments. Here, we propose a new ocean color algorithm to derive the relative cell abundance of seven phytoplankton groups, as well as their contribution to total chlorophyll a (Chl a ) at the global scale. Our algorithm is based on machine learning and has been trained using remotely sensed parameters (reflectance, backscattering, and attenuation coefficients at different wavelengths, plus temperature and Chl a ) combined with an omics-based biomarker developed using Tara Oceans data representing a single-copy gene encoding a component of the photosynthetic machinery that is present across all phytoplankton, including both prokaryotes and eukaryotes. It differs from previous methods which rely on diagnostic pigments to derive phytoplankton groups. Our methodology provides robust estimates of the phytoplankton community structure in terms of relative cell abundance and contribution to total Chl a concentration. The newly generated datasets yield complementary information about different aspects of phytoplankton that are valuable for assessing the contributions of different phytoplankton groups to primary productivity and inferring community assembly processes. This makes remote sensing observations excellent tools to collect essential biodiversity variables (EBVs) and provide a foundation for developing marine biodiversity forecasts.
    Keywords: Cell Biology ; Developmental Biology ; Embryology ; Anatomy ; SELF-ORGANIZING MAPS ; OCEAN COLOR ; MARINE-PHYTOPLANKTON ; MEDITERRANEAN ; SEALIGHT-ABSORPTION ; BIODIVERSITY ; PIGMENTS
    Repository Name: National Museum of Natural History, Netherlands
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  • 40
    facet.materialart.
    Unknown
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 36 no. (4,5,6), pp. 108-171
    Publication Date: 2024-04-18
    Description: In Noordwest-Europa is de taxonomie van bramen (Rubus L. subgenus Rubus) goed op orde en de verspreiding van bramen in de verschillende landen goed bekend dankzij herbarium- en veldonderzoek vanaf de jaren 1970. De meeste soorten zijn gestabileerde apomicten die zonder bevruchting zaad vormen. De nakomelingen van een zich apomictisch voortplantende braam zijn hierdoor genetisch gelijk aan de moederplant. In Nederland dateert onderzoek aan bramen pas van na 1900 met een actieve periode na de Tweede Wereldoorlog. Dit resulteerde in 1956 in de Rubi Neerlandici door W. Beijerinck, een overzicht gebaseerd op de kunstmatig soortsopvatting van H. Sudre (Rubi Europae; 1908–1913). Het moderne, op typemateriaal en veldwerk gebaseerde onderzoek startte begin jaren 1970 en resulteerde in de decennia erna tot de herkenning en beschrijving van tal van nieuwe regionale soorten en nieuwe namen voor verkeerd geïnterpreteerde soorten. Door de meeste Europese bramendeskundigen wordt een soortsopvatting gehanteerd die inhoudt dat taxa met een areaaldiameter kleiner dan 50 km niet worden beschreven als soort. Deze opvatting wordt ook door ons gehanteerd. Op de naamlijst van Nederlandse bramen van het subgenus Rubus staan 191 soorten verdeeld over 4 secties: Rubus (Zwarte braam; ‘Rubus fruticosus agg.’; 147 soorten), Corylifolii Lindl. (Wasbraam; ‘Rubus corylifolius agg.’; 34 soorten), Caesii Lej. & Courtois (Dauwbraam; 2 soorten) en Subidaei (Focke) A.Beek (Purperbraam; 8 soorten). De laatste sectie omvat gestabiliseerde soorten met R. idaeus L. (Framboos) als voorouder. Nomenclatorische aspecten van de Nederlandse taxa en de beschrijving van enkele nieuwe wasbramen zijn in begeleidende artikelen ondergebracht. Alle taxa – secties, subsecties, series en soorten – zijn voorzien van Nederlandse namen. Aangezien areaalgrootte een belangrijke rol speelt in de taxonomie, is elke soort toegekend aan een areaalcategorie: W1 (zeer wijdverbreid; areaaldiameter 〉1500 km), W2 (wijdverbreid; idem 500–1500 km), R1 (bovenregionaal; idem 250–500 km) of R2 (regionaal; idem 50–250 km). Van de Nederlandse bramen hebben 97 soorten (51%) een regionale verspreiding; slechts 32 soorten (17%) zijn zeer wijdverbreid. Alle digitaal beschikbare verspreidingsgegevens van soorten uit het subgenus Rubus (excl. R. caesius L.) zijn samengebracht in een database, in totaal ruim 43.000 records waarvan 37.000 met een nauwkeurigheid op km-hokniveau of beter. Van alle soorten (excl. Rubus caesius) is de landelijke zeldzaamheid bepaald op grond van Rode Lijst-criteria. Bijna 80 soorten zijn landelijk zeer zeldzaam, 60 zeldzaam, 25 vrij zeldzaam en ongeveer 20 vrij algemeen of algemeen. Zeer algemene soorten ontbreken, wat niet alleen heeft te maken met het hoge aandeel regionale soorten, maar ook met het feit dat in de klei- en veengebieden zeer weinig bramen voorkomen. De regionale verspreiding wordt per soort gegeven als percentage van het aantal uurhokken per floradistrict. Hotspots van soortenrijkdom met meer dan 40 soorten per uurhok liggen in oude boslandschappen in het Rijk van Nijmegen, de Liemers, de Oude IJsselstreek en aangrenzende Veluwezoom en de omgeving van Winterswijk (Achterhoek), Epen-Vijlen (Zuid Limburg) en Oldenzaal (Twente). De regionale soorten dragen sterk bij aan de identiteit van de regio’s. De relatief grote landelijke soortenrijkdom met regionale hotspots onderstreept de ligging van ons land in het centrum van de (sub)atlantische bramendiversiteit in Europa. The taxonomy and distribution of brambles (Rubus L. subgenus Rubus) are well-known in northwestern Europe due to herbarium studies and extensive field work from the 1970s onwards. Most brambles are stabilized apomictic species that form fruits without prior fertilization. Therefore, offspring is genetically identical with the mother plant. In the Netherlands, the study of brambles did not start until 1900, with a relatively active period occuring after World War II. This resulted in the publication of Rubi Neerlandici by W. Beijerinck in 1956, an overview based on the artificial species circumscription of H. Sudre (Rubi Europae; 1908–1913). Modern research, based on the study of type material supplemented with field work began in the 1970s and lead to the recognition of several newly described regional species as well as new names for misapplied species. Most bramble experts in Europe agree on a species circumscription that includes a geographic constraint: taxa with a range less than 50 km in diameter are not described as species. We adhere to this view as well. The Dutch checklist of subgenus Rubus comprises 191 species in 4 sections: Rubus (‘Rubus fruticosus agg.’; 147 species), Corylifolii Lindl. (‘Rubus corylifolius agg.’; 34 species), Caesii Lej. & Courtois (2 species) and Subidaei (Focke) A.Beek (8 species). The latter section includes stabilized species with Rubus idaeus L. as an ancestor. Nomenclatural aspects of the Dutch taxa and the description of some new Corylifolii taxa are dealt with in accompanying papers. All taxa on the checklist are provided with Dutch names, including sections, subsections and series. Since range size is taxonomically important, this feature has been classified and assigned to each species as W1 (very widespread; range diameter 〉1500 km), W2 (widespread; 500–1500 km), R1 (supraregional; 250–500 km) or R2 (regional; 50–250 km). The Dutch checklist contains 97 regional species (51%); only 32 species (17%) are very widespread. All digitally available distribution data for species of Rubus subgenus Rubus (excluding Rubus caesius L.) have been merged into a database, currently comprising about 43,000 records, including 37,000 with an accuracy of one kilometer or better. National rarity of species (Rubus caesius excluded) has been coded according to Dutch Red List criteria based on the number of occupied 5×5 km-squares. Almost 80 species are nationally very rare, 60 rare, 25 rather rare and about 20 rather common or common. Very common species are absent from the section Rubus, which is not only caused by the large proportion of regional species, but also by the low frequency of brambles on clay and peat soils in the western and northern parts of the country. Regional occurrence is expressed as percentage occupied relative to the total number of 5×5 km-squares for each flora district. Hotspots of species richness with more than 40 species per 5×5 km-square occur in old woodland landscapes in physiogeographic gradients with sandy and loamy soils. The national species richness in a European context, the high numbers of regional species, and the occurrence of hotspots of bramble diversity emphasize the central position of the Netherlands within the (sub) atlantic range of brambles in Europe.
    Repository Name: National Museum of Natural History, Netherlands
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  • 41
    Publication Date: 2024-04-18
    Description: Ceratopsids represent one of the most iconic groups of non-avian dinosaurs. These large quadrupedal ornithischians are well-known for their bizarre cranial ornamentations, which are distinctive among different ceratopsids. However, only very little data exist on ceratopsid osteohistology and growth rates. Here, we present a detailed osteohistological analysis on Triceratops horridus preserved in a relatively large bonebed from the Lance Formation (eastern Wyoming, USA) as well as additional Triceratops cf. prorsus specimens from Canada. Deciphering the bone microstructure of this iconic dinosaur allows to better understand the growth and development of ceratopsids. The Triceratops limb elements show a distinct pattern of slower growing parallel-fibred and faster growing woven-parallel bone tissue that serves as basis for the definition of histologic ontogenetic stages (HOS). Lower (i.e., younger) HOS correspond to woven-parallel tissue while higher (i.e., older) HOS correspond to parallel-fibred tissue. The intraskeletal variation in histology is best explained through the Three-Front Model, indicating significant differences in cortical thickness between different limb bones. The Triceratops primary growth record is poorly expressed, and the few growth marks preserved show irregular spacing inconsistent with expected growth patterns. The HOS scheme provides seven stages that correspond to biological age classes and that show a correlation with body size. Our analysis suggests that the taxonomic ambiguity between Torosaurus and Triceratops cannot be solved based purely on histological data, but requires additional taphonomic, taxonomic and histological analyses. This study expands the current ceratopsian histological database and helps to better understand ceratopsid growth patterns.
    Keywords: Ceratopsian ; Ontogeny ; Skeletochronology ; Bone remodelling ; Histovariability
    Repository Name: National Museum of Natural History, Netherlands
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  • 42
    Publication Date: 2024-04-18
    Description: Phenological responses to climate change frequently vary among trophic levels, which can result in increasing asynchrony between the peak energy requirements of consumers and the availability of resources. Migratory birds use multiple habitats with seasonal food resources along migration flyways. Spatially heterogeneous climate change could cause the phenology of food availability along the migration flyway to become desynchronized. Such heterogeneous shifts in food phenology could pose a challenge to migratory birds by reducing their opportunity for food availability along the migration path and consequently influencing their survival and reproduction. We develop a novel graph-based approach to quantify this problem and deploy it to evaluate the condition of the heterogeneous shifts in vegetation phenology for 16 migratory herbivorous waterfowl species in Asia. We show that climate change-induced heterogeneous shifts in vegetation phenology could cause a 12% loss of migration network integrity on average across all study species. Species that winter at relatively lower latitudes are subjected to a higher loss of integrity in their migration network. These findings highlight the susceptibility of migratory species to climate change. Our proposed methodological framework could be applied to migratory species in general to yield an accurate assessment of the exposure under climate change and help to identify actions for biodiversity conservation in the face of climate-related risks.
    Keywords: bird migration ; climate change ; graph-based approach ; heterogeneous shifts ; network integrity ; phenological asynchrony ; vegetation phenology
    Repository Name: National Museum of Natural History, Netherlands
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  • 43
    Publication Date: 2024-04-18
    Description: Planet Earth hosts an incredible biological diversity. Estimated numbers of species occurring on Earth range from 5 to 11 million eukaryotic species including 400,000-450,000 species of plants. Much of this biodiversity remains poorly known and many species have not yet been named or even been discovered. This is not surprising, as the majority of species is known to be rare and ecosystems are generally dominated by a limited number of common species. Tropical rainforests are the most species-rich terrestrial ecosystems on Earth. The general higher level of species richness is often explained by higher levels of energy near the Equator (latitudinal diversity gradient). However, when comparing tropical rainforest biomes, African rainforests host fewer plant species than either South American or Asian ones. The Central African country of Gabon is situated in the Lower Guinean phytochorical region. It is largely covered by what is considered to be the most species-rich lowland rainforest in Africa while the government supports an active conservation program. As such, Gabon is a perfect study area to address that enigmatic question that has triggered many researchers before: “What determines botanical species richness?”. In the past 2.5 million years, tropical rainforests have experienced 21 cycles of global glaciations. They responded to this by contracting during drier and cooler glacials into larger montane and smaller riverine forest refugia and expanding again during warmer and wetter interglacials. The current rapid global climate change coupled with change of land use poses new threats to the survival of many rainforest species. The limited availability of resources for conservation forces governments and NGOs to set priorities. Unfortunately, for many plant species, lack of data on their distribution hampers well-informed decision making in conservation. Species distribution models (SDMs) offer opportunities to bridge at least partly this knowledge gap. SDMs are correlative models that infer the spatial distribution of species using only a limited set of known species occurrence records coupled with high resolution environmental data. SDMs are widely applied to study the past, present and future distribution of species, assess the risk of invasive species, infer patterns of species richness and identify hotspots, as well as to assess the impact of climate change. The currently available methods form a pipeline, with which data are selected and cleaned, models selected, parameterized, evaluated and projected to other areas and climatic scenarios, and biodiversity patterns are computed from these SDMs. In this thesis, SDMs of all Gabonese plant species were generated and patterns of species richness and of weighted endemism were computed (chapter 4 & 5). Although this pipeline enables the rapid generation of SDMs and inferring of biodiversity patterns, its effective use is limited by several matters of which three are specifically addressed in this thesis. Not knowing the true distribution limits the opportunities to assess the accuracy of models and assess the impact of assumptions and limitations of SDMs. The use of simulated species has been advocated as a method to systematically assess the impact of specific matters of SDMs (virtual ecologist). Following this approach, in chapter 2, I present a novel method to simulate large numbers of species that each have their own unique niche. One matter of SDMs that is usually ignored but has been shown to be of great impact on model accuracy is the number of species occurrence records used to train a model. In chapter 2, I quantify the effect of sample size on model accuracy for species of different range size classes. The results show that the minimum number of records required to generate accurate SDMs is not uniform for species of every range size class and that larger sample sizes are required for more widespread species. By applying a uniform minimum number of records, SDMs of narrow-ranged species are incorrectly rejected and SDMs of widespread species are incorrectly accepted. Instead, I recommend to identify and apply the unique minimum numbers of required records for each individual species. The method presented here to identify the minimum number of records for species of particular range size classes is applicable to any species group and study area. The range size or prevalence is an important plant feature that is used in IUCN Red List classifications. It is commonly computed as the Extent Of Occurrence (EOO) and Area Of Occupancy (AOO). Currently, these metrics are computed using methods based on the spatial distribution of the known species occurrences. In chapter 3, using simulated species again, I show that methods based on the distribution of species occurrences in environmental parameter space clearly outperform those based on spatial data. In this chapter, I present a novel method that estimates the range size of a species as the fraction of raster cells within the minimum convex hull of the species occurrences, when all cells from the study area are plotted in environmental parameter space. This novel method outperforms all ten other assessed methods. Therefore, the current use of EOO and AOO based on spatial data alone for the purpose of IUCN Red List classification should be reconsidered. I recommend to use the novel method presented here to estimate the AOO and to estimate the EOO from the predicted distribution based on a thresholded SDM. In chapter 4, I apply the currently best possible methods to generate accurate SDMs and estimate the range size of species to the large dataset of Gabonese plant species records. All significant SDMs are used here to assess the unique contribution of narrow-ranged, widespread, and randomly selected species to patterns of species richness and weighted endemism. When range sizes of species are defined based on their full range in tropical Africa, random subsets of species best represent the pattern of species richness, followed by narrow-ranged species. Narrow-ranged species best represent the weighted endemism pattern. Moreover, the results show that the applied criterion of widespread and narrow-ranged is crucial. Too often, range sizes of species are computed on their distribution within a study area defined by political borders. I recommend to use the full range size of species instead. Secondly, the use of widespread species, of which often more data are available, as an indicator of diversity patterns should be reconsidered. The effect of global climate change on the distribution patterns of Gabonese plant species is assed in chapter 5 using SDMs projected to the year 2085 for two climate change scenarios assuming either full or no dispersal. In Gabon, predicted loss of plant species ranges from 5% assuming full dispersal to 10% assuming no dispersal. However, these numbers are likely to be substantially higher, as for many rare, narrow-ranged species no significant SDMs could be generated. Predicted species turnover is as high as 75% and species-rich areas are predicted to loose many species. The explanatory power of individual future climate anomalies to predicted future species richness patterns is quantified. Species loss is best explained by increased precipitation in the dry season. Species gain and species turnover are correlated with a shift from extreme to average values of annual temperature range. In the final chapter, the results are placed in a wider scientific context. First, the results on the methodological aspects of SDMs and their implications of the SDM pipeline are discussed. The method presented in this thesis to simulate large numbers of species offers opportunities to systematically investigate other matters of the pipeline, some of which are discussed here. Secondly, the factors that shape the current and predicted future patterns of plant species richness in Gabon are discussed including the location of centres of species richness and of weighted endemism in relation to the hypothesized location of glacial forest refugia. Factors that may contribute to the lower species richness of African rainforests compared with South American and Asian forests are discussed. I conclude by reflecting on the conservation of the Gabonese rainforest and its plant species as well as on the opportunities SDMs offer for this in the wider socio-economic context of a changing world with growing demand for food and other ecosystem services.
    Keywords: plants ; biodiversity ; species diversity ; speciesdistribution ; biogeography ; central africa ; biosystematics ; tropical rain forests ; modeling
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/doctoralThesis
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  • 44
    Publication Date: 2024-04-18
    Description: Octocorallia (primarily soft corals and gorgonians) occur in cold-water environments as well as in tropical seas and can form a major component of reef communities. Because of their abundance and three-dimensional structure octocorals are an important habitat for symbiotic species such as crustaceans, worms, fishes and molluscs. Among the latter group are snails of the family Ovulidae, obligate associates of octocorals. Ovulid snails have adapted their morphological appearance to avoid predation. They can either be perfectly camouflaged or ambiguously coloured to advertise their toxic properties. It was therefore expected that these morphological adaptations would have an evolutionary background, which would corresponds with that of their octocoral hosts. In this thesis the evolutionary history of the Ovulidae and Octocorallia are examined within and between both taxa by using a multifaceted approach, consisting of (calibrated) phylogenetic and co-evolutionary analyses, taxonomic revisions and coral bioactivity research. The results show that snails and octocorals did not coevolve, but that the evolutionary history between both groups is best described as sequential evolution in which the host affects the symbiont but not vice versa.
    Keywords: Octocorallia ; Cospeciaton ; Ovulidae ; Co-evolution ; Sequential evolution ; Phylogeny ; Taxonomy ; Systematics
    Repository Name: National Museum of Natural History, Netherlands
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  • 45
    Publication Date: 2024-04-18
    Description: The late Quaternary history of Sumatra has experienced relatively little attention compared to that of the other large islands in the Indonesian archipelago. The first reports of fossils from the island date to the 1880s; they were discovered largely through the efforts of Dubois in the caves of the Padang Highlands. Following these efforts, focus shifted in the 1920s and 1930s to the archaeological records of the midden deposits of northern Sumatra and the Hoabinhian cultures preserved therein. There was little new fieldwork between 1940 and 1970, but by the mid-1970s several new campaigns seemed to herald a renewed interest in the history and prehistory of the island. This enthusiasm does not appear to have been sustained, however, and work was intermittent again in the 1980s and 1990s. Beginning in the mid-1990s and extending into the first two decades of the twenty-first century, more work at existing sites and new investigations have both taken place, extending our knowledge of both the deep-time and more recent history of the island. The application of new techniques on existing sites and the exploration and excavation of new sites are making an increasingly significant contribution to understanding the role of Sumatra in human biological and cultural evolution.
    Keywords: Hoabinhian ; Dubois ; van Stein Callenfels ; caves ; fossils ; history of archaeology ; sumatralith
    Repository Name: National Museum of Natural History, Netherlands
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  • 46
    Publication Date: 2024-04-18
    Description: The Arctic Ocean is home to a unique fauna that is disproportionately affected by global warming but that remains under-studied. Due to their high mobility and responsiveness to global warming, cephalopods and fishes are good indicators of the reshuffling of Arctic communities. Here, we established a nekton biodiversity baseline for the Fram Strait, the only deep connection between the North Atlantic and Arctic Ocean. Using universal primers for fishes (12S) and cephalopods (18S), we amplified environmental DNA (eDNA) from seawater (50–2700 m) and deep-sea sediment samples collected at the LTER HAUSGARTEN observatory. We detected 12 cephalopod and 31 fish taxa in the seawater and seven cephalopod and 28 fish taxa in the sediment, including the elusive Greenland shark (Somniosus microcephalus). Our data suggest three fish (Mallotus villosus, Thunnus sp., and Micromesistius poutassou) and one squid (Histioteuthis sp.) range expansions. The detection of eDNA of pelagic origin in the sediment also suggests that M. villosus, Arctozenus risso, and M. poutassou as well as gonatid squids are potential contributors to the carbon flux. Continuous nekton monitoring is needed to understand the ecosystem impacts of rapid warming in the Arctic and eDNA proves to be a suitable tool for this endeavor.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 47
    Publication Date: 2024-04-18
    Description: Ice-binding proteins (IBPs) are a group of ecologically and biotechnologically relevant enzymes produced by psychrophilic organisms. Although putative IBPs containing the domain of unknown function (DUF) 3494 have been identified in many taxa of polar microbes, our knowledge of their genetic and structural diversity in natural microbial communities is limited. Here, we used samples from sea ice and sea water collected in the central Arctic Ocean as part of the MOSAiC expedition for metagenome sequencing and the subsequent analyses of metagenome-assembled genomes (MAGs). By linking structurally diverse IBPs to particular environments and potential functions, we reveal that IBP sequences are enriched in interior ice, have diverse genomic contexts and cluster taxonomically. Their diverse protein structures may be a consequence of domain shuffling, leading to variable combinations of protein domains in IBPs and probably reflecting the functional versatility required to thrive in the extreme and variable environment of the central Arctic Ocean.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 48
    Publication Date: 2024-04-18
    Description: In Fram Strait, we combined underway-sampling using the remote-controlled Automated Filtration System for Marine Microbes (AUTOFIM) with CTD-sampling for eDNA analyses, and with high-resolution optical measurements in an unprecedented approach to determine variability in plankton composition in response to physical forcing in a sub-mesoscale filament. We determined plankton composition and biomass near the surface with a horizontal resolution of ~ 2 km, and addressed vertical variability at five selected sites. Inside and near the filament, plankton composition was tightly linked to the hydrological dynamics related to the presence of sea ice. The comprehensive data set indicates that sea-ice melt related stratification near the surface inside the sub-mesoscale filament resulted in increased sequence abundances of sea ice-associated diatoms and zooplankton near the surface. In analogy to the physical data set, the underway eDNA data, complemented with highly sampled phytoplankton pigment data suggest a corridor of 7 km along the filament with enhanced photosynthetic biomass and sequence abundances of sea-ice associated plankton. Thus, based on our data we extrapolated an area of 350 km2 in Fram Strait with enhanced plankton abundances, possibly leading to enhanced POC export in an area that is around a magnitude larger than the visible streak of sea-ice.
    Repository Name: EPIC Alfred Wegener Institut
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  • 49
    Publication Date: 2024-04-18
    Description: The Beagle Channel is a remote subantarctic environment where mussel aquaculture initiatives have existed since the early 1990s. Here we analyze phytoplankton biomass and composition, and the occurrence of harmful microalgae species and their toxins at three sites during the period 2015–2016. The occurrence of potentially harmful algae was observed throughout the study period, including toxigenic dinoflagellates such as Alexandrium catenella (Group I of the A. tamarense complex), A. ostenfeldii, Dinophysis acuminata, Gonyaulax spinifera, Azadinium sp., and the diatoms Pseudo-nitzschia australis and P. fraudulenta. Toxic dinoflagellates were detected in low densities whereas a Pseudo-nitzschia bloom was observed in late February. Isolates of A. catenella and P. delicatissima sensu stricto were phylogenetically characterized. The toxin profile of A. catenella was dominated by GTX4, while P. delicatissima sensu stricto showed no production of the neurotoxin domoic acid in culture conditions. The results provide base-line information for the management of harmful algal blooms in this little explored subantarctic area.
    Repository Name: EPIC Alfred Wegener Institut
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  • 50
    Publication Date: 2024-04-18
    Description: The Argentine Sea is worldwide recognized as a highly productive area, characterized by extensive phytoplankton blooms during spring and summer. Despite the well-known importance of frontal areas for biomass accumulation, phytoplankton diversity remains poorly studied. In an unprecedented approach for the Argentine Sea, we combined microscopy and 18Sv4 metabarcoding analyses for a refined assessment of summer phytoplankton composition in three understudied frontal areas of the Argentine Sea (≈43°−55°S), with contrasting oceanographic conditions. Metabarcoding and microscopy analyses agreed on the detection of the dominant phytoplanktonic groups in the different frontal areas studied; chlorophytes in Valdés Peninsula, dinoflagellates in waters off Blanco Cape, and diatoms in de los Estados Island. The analysis of the phytoplankton community was significantly enriched by combining both techniques, microscopy provided cell abundances and biomass data and metabarcoding provided greater detail on species composition, revealing an important specific richness of dinoflagellates, diatoms and other delicate groups, such as chlorophytes. However, we also considered differences between the methods for certain taxa at a lower taxonomic level (species/genus) of the dominant taxa, such as the underestimation of the diatoms Asterionellopsis glacialis and Pseudo-nitzschia spp. and the overestimation of Chaetoceros contortus by metabarcoding in comparison to microscopic counts. The detection of several taxa belonging to small and delicate groups, previously overlooked due to the lack of distinct morphological features, establishes a baseline for future studies on phytoplankton diversity in the Argentine Sea.
    Repository Name: EPIC Alfred Wegener Institut
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  • 51
    Publication Date: 2024-04-18
    Repository Name: EPIC Alfred Wegener Institut
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  • 52
    Publication Date: 2024-04-18
    Description: Not filtered water samples were taken in 10 ml ampoules (sealed immediately after being acidified with phosphoric acid to pH〈2, sampling), or 40 ml screw-lid vials, and measured onboard at sampling or next days, or frozen (-20°C) until being acidified and measured in home labs. Carbon measurement was by high-temperature catalytic oxydation in a 10 cm column packed with 5% Pt on aluminum oxide beads at 900°C in a stream of oxygen, and CO2 detection by infrared extinction after the removal of moisture and SO2 by appropriate traps (cold trap, Mg-percarbonate, Na-pyrophosphate, tin, bronze or Sulfix). The apparatus was the dual channel Dimatek 2000 equipped with a Binos 200 detector.
    Keywords: CTD/Rosette; CTD-RO; M27/2; M27/2-CTD-026_022; M27/2-CTD-027_023; M27/2-CTD-028_024; M27/2-CTD-029_025; M27/2-CTD-030_026; M27/2-CTD-031_027; M27/2-CTD-032_028; M27/2-CTD-033_029; M27/2-CTD-034_030; M27/2-CTD-035_031; Meteor (1986)
    Type: Dataset
    Format: application/zip, 10 datasets
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  • 53
    facet.materialart.
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    PANGAEA
    In:  Supplement to: Pfannkuche, Olaf (1992): Organic carbon flux through the benthic community in the temperate abyssal northeast Atlantic. In: Rowe, G T & Pariente, V (eds.), Deep-sea food chains and the global carbon cycle. Dordrecht, Kluwer Academic Publishers, 183-198
    Publication Date: 2024-04-18
    Description: In order to assess the carbon flux through the deep-sea benthic boundary layer, sediment community oxygen consumption (SCOC) was measured in different months and years at the BIOTRANS area in the abyssal northeastern Atlantic. SCOC varied seasonally with a maximum in July/August. Evidence is given for a direct coupling between a substantial sedimentation of phytodetritus and the seasonal increase in SCOC. Rapid colonization, growth and decomposition rates indicate that the deep-sea benthic microbial and protozoan biota can react quickly to substantial falls of particulate organic matter. They seem to be the most important groups to generate seasonal changes in deep-sea benthic carbon flux rates.
    Keywords: ADEPD; ANT-IV/1a; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Biotrans; Giant box corer; GKG; M69; M69_KG1046; M69_KG1047; M69_KG1048; M69_KG1049; M69_KG1050; M69_KG1051; M69_KG1052; M69_KG1053; M69_MC10; Meteor (1964); MUC; MultiCorer; NOAMP III; North Atlantic Ocean; Polarstern; PS08_KG1088; PS08_KG1092; PS08_KG1094; PS08_KG1101; PS08_KG1103; PS08_KG1107; PS08_KG1110; PS08_KG1112; PS08_MC25; PS08_MC27; PS08_MC28; PS08_MC31; PS08_MC33; PS08_MC34; PS08_MC35; PS08_MC36; PS08_MC37; PS08_MC38; PS08_MC39; PS08 NOAMP
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 54
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Pfannkuche, Olaf; Theeg, R; Thiel, Hjalmar (1983): Benthos activity, abundance and biomass under an area of low upwelling off Morocco, Northwest Africa. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe D Biologie, Gebrüder Bornträger, Berlin, Stuttgart, D36, 85-96
    Publication Date: 2024-04-18
    Description: Macro- and meiobenthic abundance and biomass as well as metabolic activity (respiration, ETS activity) have been studied along a transect ranging from 130 to 3000 m water depth off northern Morocco (35° N) during "Meteor" cruise No. 53 (1980). The distribution of chloroplastic pigment concentration (chlorophyll a, pheophytins) in the sediment has been investigated as a measure of sedimented primary organic matter. High chloroplastic pigment concentrations were found on the shelf and around the shelf break, but values declined rapidly between 200 and 600 m depth. Below 1200 m pigment concentrations remained at a relatively uniform low level. Macrobenthic abundance and biomass (wet weight) decreased with increasing water depth and with distance from the shore. Significant changes occurred between the shelf and upper slope and below 2000 m depth. Meiobenthic abundance and biomass (ash free dry weight) followed the same general pattern, but changes were found below 400 and 800 m depth. In the depth range of 1200 to 3000 m values differ only slightly. Meiofauna abundance and biomass show a good correlation with the sedimentary chloroplastic pigment concentrations. Respiratory activity of sediment cores, measured by a shipboard technique at ambient temperatures, decreased with water depth and shows a good correlation with the pigment concentrations. ETS activity was highest on the shelf and decreased with water depth, with significant changes between 200 and 400 m, and below 1200 m depth, respectively. Activity was generally highest in the top 5 cm of the sediment and was measurable, at all stations, down to 15 cm sediment depth. Shelf and upper slope stations exhibited a vertical distribution pattern of ETS activity in the sediment column, different from that of deeper stations. The importance of biological activity measurements as an estimate of productivity is discussed. To prove the thesis that differences in benthic abundance, biomass and activity reflect differences in pelagic surface primary production, in the case of the NW-African coast caused by different upwelling intensities, the values from 35° N were compared with data from 21° N (permanent upwelling activity) and 17° N (ca. 9 months upwelling per year). On the shelf and upper slope (〈 500 m) hydrographical conditions (currents, internal waves) influence the deposition of organic matter and cause a biomass minimum between 200 and 400 m depth in some regions. But, in general, macrobenthic abundance and biomass increases with enhanced upwelling activity and reaches a maximum in the area off Cape Blanc (21° N). On the shelf and in the shelf break region meiofauna densities are higher at 35° N in comparison to 21° N; but in contrast to the decreasing meiofauna abundance with increasing water depth at 35° N, an abundance maximum between 400 and 1200 m depth is formed in the Cape Blanc region; this maximum coincides with the maximum of sedimentary chloroplastic pigment equivalents. The comparison of ETS activities between 35° N and 21° N shows on the shelf activity at 21° N is up to 14 times higher and on the slope 4-9 times higher, which demonstrates that benthic activity responds to the surface productivity regime.
    Keywords: Giant box corer; GIK15672-2; GKG; M53; M53_155-4; M53_158-4; M53_162-4; M53_164-4; M53_166-4; M53_168-1; M53_169-2; M53_170-1; M53_172-1; M53_173-2; M53_KG-804; M53_KG-808; M53_KG-812; M53_KG-816; M53_KG-820; M53_KG-822; M53_KG-824; M53_KG-827; M53_KG-833; Meteor (1964); off West Africa
    Type: Dataset
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  • 55
    Publication Date: 2024-04-18
    Description: Modern planktonic foraminifera collected with a sediment trap and subfossil assemblages from surface sediments from Galway Mound in the Porcupine Seabight off southwestern Ireland, northeastern Atlantic, were studied to show recent assemblage variations. The sediment trap operated from April to August 2004 and covers the spring bloom and early summer conditions with sampling intervals of 8 days. Eleven different species were recorded. Glorotalia hirsuta, Turborotalita quinqueloba and Globigerinita glutinata appeared predominately in spring. Neogloboquadrina incompta, Globigerina bulloides and Globorotalia inflata were abundant in spring and summer. The highest foraminiferal tests flux occured in June. The faunal composition was similar to subfossil assemblages from surface sediments, but the species proportions were different. This was mainly affected by the subtropical G. hirsuta, which was frequent in 2004 and rare in surface sediment samples and in earlier plankton collections from the southern Porcupine Seabight that were performed during the 1990s. The weight of deposited foraminifera is mainly influenced by spring bloom as indicated by sea-surface chlorophyll-a data. The top three-ranked species, G. hirsuta, N. incompta and G. bulloides contributed 87 % to the foraminiferal carbonate flux at Galway Mound. Foraminiferal carbonate and shell flux as well as the shell size revealed variations, which are related to lunar periodicity. The data infer a lunar pacing of reproduction for the main species as well as for G. glutinata and G. inflata, which was not recorded before.
    Keywords: Belgica Mound Province, Galway Mound; GeoB9205-1; Giant box corer; GKG; M61/3; M61/3_552; Meteor (1986)
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 56
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Pfannkuche, Olaf; Sommer, Stefan; Kähler, A (2000): Coupling between phytodetritus and the small-sized benthic biota in the deep Arabian Sea: analyses of biogenic sediment compound. Deep Sea Research Part II: Topical Studies in Oceanography, 47(14), 2805-2833, https://doi.org/10.1016/S0967-0645(00)00050-3
    Publication Date: 2024-04-18
    Description: As part of the large-scale, interdisciplinary deep-sea study "BIGSET", the relationship between the monsoon-induced regional and temporal variability of POC deposition and the small-sized benthic community was investigated at several sites 2316-4420 m deep in the Arabian Sea during four cruises between 1995 and 1998. Vertical and horizontal distribution patterns of chloroplastic pigments (a measure of phytodetritus deposition), readily soluble protein and activity, and biomass parameters of the small-sized benthic community (Electron Transport System Activity (ETSA); bacterial ectoenzymatic activity (FDA turnover) and DNA concentrations) were measured concurrently with the vertical fluxes of POC and chloroplastic pigments. Sediment chlorophyll a (chl. a) profiles were used to calculate chl. a flux rates and to estimate POC flux across the sediment water interface using two different transport reaction models. These estimates were compared with corresponding flux rates determined in sediment traps. Regional variability of primary productivity and POC deposition at the deep-sea floor creates a trophic gradient in the Arabian Basin from the NW to the SE, which is primarily related to the activity of monsoon winds and processes associated with the topography of the Arabian Basin and the vicinity of land masses. Inventories of sediment chloroplastic pigments closely corresponded to this trophic gradient. For ETSA, FDA and DNA, however, no clear coupling was found, although stations WAST (western Arabian Sea) and NAST (northern Arabian Sea) were characterised by high concentrations and activities. These parameters exhibited high spatial and temporal variability, making it impossible to recognise clear mechanisms controlling temporal and spatial community patterns of the small-sized benthic biota. Nevertheless, the entire Arabian Basin was recognised as being affected by monsoonal activity. Comparison of two different transport reaction models indicates that labile chl. a buried in deeper sediment layers may escape rapid degradation in Arabian deep-sea sediments.
    Keywords: 109, M31/3-109_MC2; 11#1; 11#2; 110#1, M31/3-110.1_MC2; 110#2, M31/3-110.2_MC2; 110#3, M31/3-110.3_MC1; 110#4, M31/3-110.4_MC3; 13#3; 19#2; 19#7; 19#9; 22#1; 24#1; 26; 3; 30#4; 31#9; 34#1; 35#4; 36#2; 36#3; 41; 43#4; 46; 49#1; 49#8; 50#1; 54; 58#3, CAST; 581; 585; 587; 6#2; 60#3; 603; 611; 614; 633; 637; 641, CAST; 655; 661; 662; 666; 668; 67#1; 671; 70#3, NAST; 73#1; 76#2; 80; 85#1; 88#1; 9#2; 9#4; Arabian Sea; BIGSET; BIGSET-1; BIGSET-2/JGOFS-IN-4; Biogeochemical Fluxes of Matter and Energy in the Deep Sea; Central Arabian Sediment Trap; Eastern Arabian Sediment Trap; M31/3; M31/3_MC-02; M31/3_MC-05; M31/3_MC-07; M31/3_MC-10; M31/3_MC-12; M31/3_MC-15; M31/3_MC-17; M31/3-108_MC1/1, 108; M31/3-112_MC1, MC377, GeoB3010-3; M33/1; M33/1_MC-01; M33/1_MC-04; M33/1_MC-06; M33/1_MC-08; M33/1_MC-10; M33/1_MC-12; M33/1_MC-16; M33/1_MC-18; M33/1_MC-21; M33/1_MC-22; M33/1_MC-24; M33/1_MC-26; M33/1_MC-29; M33/1_MC-31; M33/1_MC-34; Meteor (1986); MUC; MultiCorer; Northern Arabian Sediment Trap; Northern Arabian Sediment Trap/Western Arabian Sediment Trap; SO118; SO118_MC-07; SO118_MC-08; SO118_MC-09; SO118_MC-10; SO118_MC-12; SO118_MC-14; SO118_MC-19; SO118_MC-20; SO118_MC-22; SO118_MC-24; SO118_MC-27; SO118_MC-30; SO118_MC-33; SO118_MC-35; SO118_MC-37; SO118_MC-39; SO118_MC-43; SO118_MC-44; SO118_MC-45; SO118_MC-47; SO118_MC-48; SO118_MC-50; SO129; SO129_MC-01; SO129_MC-04; SO129_MC-06; SO129_MC-08; SO129_MC-10; SO129_MC-11; SO129_MC-13; SO129_MC-15; SO129_MC-17; SO129_MC-18; SO129_MC-20; SO129_MC-21; SO129_MC-23; Sonne; Southern Arabian Sediment Trap; Southern Arabian Sediment Trap/Eastern Arabian Sediment Trap; Southern Arabian Sediment Trap/Western Arabian Sediment Trap; Western Arabian Sediment Trap; Western Arabian Sediment Trap/Central Arabian Sediment Trap; Western Arabian Sediment Trap/Southern Arabian Sediment Trap; Western Arabian Sediment Trap-Kuppe; Western Arabian Sediment Trap Plain; Western Arabian Sediment Trap Top
    Type: Dataset
    Format: application/zip, 57 datasets
    Location Call Number Expected Availability
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  • 57
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Kurbjeweit, Frank; Schmiedl, Gerhard; Schiebel, Ralf; Hemleben, Christoph; Pfannkuche, Olaf; Wallmann, Klaus; Schäfer, Priska (2000): Distribution, biomass and diversity of benthic foraminifera in relation to sediment geochemistry in the Arabian Sea. Deep Sea Research Part II: Topical Studies in Oceanography, 47(14), 2913-2955, https://doi.org/10.1016/S0967-0645(00)00053-9
    Publication Date: 2024-04-18
    Description: The distribution, biomass, and diversity of living (Rose Bengal stained) deep-sea benthic foraminifera (〉30 µm) were investigated with multicorer samples from seven stations in the Arabian Sea during the intermonsoonal periods in March and in September/October, 1995. Water depths of the stations ranged between 1916 and 4425 m. The distribution of benthic foraminifera was compared with dissolved oxygen, % organic carbon, % calcium carbonate, ammonium, % silica, chloroplastic pigment equivalents, sand content, pore water content of the sediment, and organic carbon flux to explain the foraminiferal patterns and depositional environments. A total of six species-communities comprising 178 living species were identified by principal component analysis. The seasonal comparison shows that at the western stations foraminiferal abundance and biomass were higher during the Spring Intermonsoon than during the Fall Intermonsoon. The regional comparison indicates a distinct gradient in abundance, biomass, and diversity from west to east, and for biomass from north to south. Highest values are recorded in the western part of the Arabian Sea, where the influence of coastal and offshore upwelling are responsible for high carbon fluxes. Estimated total biomass of living benthic foraminifera integrated for the upper 5 cm of the sediment ranged between 11 mg Corg m**-2 at the southern station and 420 mg Corg m**-2 at the western station. Foraminifera in the size range from 30 to 125 ?m, the so-called microforaminifera, contributed between 20 and 65% to the abundance, but only 3% to 28% to the biomass of the fauna. Highest values were found in the central and southern Arabian Sea, indicating their importance in oligotrophic deep-sea areas. The overall abundance of benthic foraminifera is positively correlated with oxygen content and pore volume, and partly with carbon content and chloroplastic pigment equivalents of the sediment. The distributional patterns of the communities seem to be controlled by sand fraction, dissolved oxygen, calcium carbonate and organic carbon content of the sediment, but the critical variables are of different significance for each community.
    Keywords: 110, M31/3_MC376, WAST; 581, NAST; 621, WAST-T; 622, WAST; 640, CAST; 661, EAST; 666, SAST; Arabian Sea; BIGSET; Biogeochemical Fluxes of Matter and Energy in the Deep Sea; Central Arabian Sediment Trap; Eastern Arabian Sediment Trap; M31/3; M31/3_111#1,GeoB3007-3,WAST-T; M31/3_111#2,GeoB3008-5,WAST-Flank; M31/3_MC-08; M31/3_MC-11; M31/3-110.4_MC1; M33/1; M33/1_MC-03; M33/1_MC-13; M33/1_MC-15; M33/1_MC-19; M33/1_MC-25; M33/1_MC-30; Meteor (1986); MUC; MultiCorer; Northern Arabian Sediment Trap; Southern Arabian Sediment Trap; Western Arabian Sediment Trap
    Type: Dataset
    Format: application/zip, 33 datasets
    Location Call Number Expected Availability
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  • 58
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Schiebel, Ralf; Hemleben, Christoph (2000): Interannual variability of planktic foraminiferal populations and test flux in the eastern North Atlantic Ocean (JGOFS). Deep Sea Research Part II: Topical Studies in Oceanography, 47(9-11), 1809-1852, https://doi.org/10.1016/S0967-0645(00)00008-4
    Publication Date: 2024-04-18
    Description: Planktic foraminiferal assemblages vary in response to seasonal fluctuations of hydrographic properties, between water masses, and after periodical changes and episodic events (e.g. reproduction, storms). Distinct annual variability of the planktic foraminiferal flux is also known from sediment trap data. In this paper we discuss the short-term impacts on interannual flux rates based on data from opening-closing net hauls obtained between the ocean surface and 500 m water depth. Data were recorded during April, May, June, and August at around 47°N, 20°W (BIOTRANS) in 1988, 1989, 1990, 1992, 1993, and during May 1989 and 1992 at 57°N, 20-22°W. Species assemblages closely resemble each other when comparing the mixed layer fauna with the fauna of the upper 100 m and the upper 500 m of the water column. In addition, species assemblages 〉100 µm are almost indistinguishable from assemblages that are 〉125 µm in test size. The standing stock of planktic foraminifers at BIOTRANS can vary by more than one order of magnitude over different years; however, species assemblages may be similar when comparing corresponding seasons. Early summer assemblages (June) are distinctly different from late summer assemblages (August). Significant variations in the species composition during spring (April/May) are independent of the mixed layer depth. Spring assemblages are characterized by high numbers of Globigerinita glutinata. In particular, day-to-day variations of the number of specimens and in species composition may have the same order of magnitude as interannual variations. This appears to be independent of the reproduction cycle. Species assemblages at 47°N and 57°N are similar during spring, although surface water temperatures and salinities differ by up to 10°C and 0.7 (PSU). We suggest that the main factors controlling the planktic foraminiferal fauna are the trophic properties in the upper ocean productive layer. Planktic foraminiferal carbonate flux as calculated from assemblages reveals large seasonal variations, a quasi-annual periodicity in flux levels, and substantial differences in timing and magnitude of peak fluxes. At the BIOTRANS station, the average annual planktic foraminiferal CaCO3 fluxes at 100 and 500 m depth are estimated to be 22.4 and 10.0 g/m**2/yr, respectively.
    Keywords: 102; 111; 129; 148; 158; 164; 167; 172; 173; 176; 177; 1781; 181; 187; 188; 199; 204; 211; 219; 224; 225; 227; 228; 230; 231; 247; 25; 250; 277; 285; 286; 289; 292; 30; 301; 302; 306; 309; 311; 314; 319; 320; 322; 323; 324; 325; 327; 328; 351; 357; 367; 373; 374; 381; 389; 390; 396; 407; 430; 437; 440; 445; 45; 452; 455; 460; 463; 475; 481; 485; 487; 492; 499; 52; 553; 562; 569; 77; 80; 87; 887; 895; 896; 899; 900; 901; 92; 96; 99; Aegir Ridge; Arquipelago; Azores front; Bear Island; Biotrans; FCA97; FCA97C_MSN1339; FCA97C_MSN1340; FCA97C_MSN1343; FCA97C_MSN1344; FCA97C_MSN1345; FCA97C_MSN1346; GeoTü; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; JGOFS; Joint Global Ocean Flux Study; Lofoten Basin; M10/2; M10/2_MSN218; M10/2_MSN219; M10/2_MSN229; M10/2_MSN231; M10/2_MSN232; M10/2_MSN234; M10/2_MSN238; M10/2_MSN251; M10/2_MSN261; M10/2_MSN262; M10/2_MSN265; M10/2_MSN268; M10/2_MSN284; M10/2_MSN295; M10/2_MSN297; M10/2_MSN298; M10/2_MSN315; M10/2_MSN317; M10/2_MSN319; M10/2_MSN322; M10/2_MSN332; M10/2_MSN334; M11/1; M11/1_MSN517; M11/1_MSN520; M11/1_MSN522; M11/1_MSN524; M11/1_MSN526; M11/1_MSN528; M12/3; M12/3_MSN533; M12/3_MSN535; M12/3_MSN536; M12/3_MSN538; M12/3_MSN541; M12/3_MSN543; M12/3_MSN545; M12/3_MSN547; M12/3_MSN557; M12/3_MSN558; M12/3_MSN559; M12/3_MSN560; M12/3_MSN561; M12/3_MSN562; M21/1; M21/1_MSN603; M21/1_MSN604; M21/1_MSN605; M21/1_MSN606; M21/1_MSN607; M21/1_MSN608; M21/1_MSN609; M21/1_MSN610; M21/1_MSN611; M21/1_MSN613; M21/1_MSN614; M21/1_MSN615; M21/1_MSN619; M21/1_MSN620; M21/2; M21/2_MSN624; M21/2_MSN627; M21/2_MSN628; M21/2_MSN629; M21/2_MSN638; M21/2_MSN639; M21/2_MSN640; M21/2_MSN641; M21/2_MSN642; M21/2_MSN643; M21/2_MSN644; M21/2_MSN647; M21/2_MSN648; M21/2_MSN649; M21/2_MSN650; M21/2_MSN651; M21/2_MSN652; M21/2_MSN656; M21/2_MSN657; M21/2_MSN658; M21/3; M21/3_MSN661; M21/3_MSN662; M21/3_MSN663; M21/3_MSN671; M21/3_MSN674; M21/3_MSN675; M21/3_MSN676; M21/3_MSN687; M21/3_MSN688; M21/4; M21/4_MSN694; M21/4_MSN695; M21/4_MSN696; M21/4_MSN697; M21/4_MSN698; M21/4_MSN699; M21/4_MSN700; M21/4_MSN701; M21/4_MSN702; M21/4_MSN703; M21/4_MSN704; M21/4_MSN705; M21/4_MSN706; M21/4_MSN707; M21/4_MSN710; M21/4_MSN711; M21/4_MSN712; M21/4_MSN713; M21/4_MSN714; M21/4_MSN715; M21/4_MSN716; M21/4_MSN717; M21/4_MSN718; M21/4_MSN719; M21/4_MSN720; M21/4_MSN721; M21/4_MSN722; M21/4_MSN723; M21/4_MSN724; M21/5; M21/5_MSN728; M21/5_MSN729; M21/5_MSN730; M21/5_MSN731; M21/5_MSN732; M21/5_MSN733; M21/5_MSN734; M21/5_MSN735; M21/5_MSN736; M21/5_MSN739; M21/5_MSN740; M21/5_MSN741; M21/5_MSN742; M21/5_MSN743; M21/6; M21/6_MSN766; M21/6_MSN767; M21/6_MSN768; M21/6_MSN776; M21/6_MSN777; M21/6_MSN778; M21/6_MSN784; M21/6_MSN785; M21/6_MSN786; M21/6_MSN787; M21/6_MSN788; M21/6_MSN789; M26/1; M26/1_MSN843; M26/1_MSN844; M26/1_MSN845; M27/2; M27/2_MSN879; M27/2_MSN882; M27/2_MSN883; M27/2_MSN884; M36/2; M36/2_MSN1107; M36/6; M36/6_MSN1193; M36/6_MSN1194; M36/6_MSN1195; M36/6_MSN1196; M36/6_MSN1197; M36/6_MSN1198; M42/3; M42/3_MSN1359; M42/3_MSN1360; M42/3_MSN1361; M42/3_MSN1362; M42/3_MSN1363; M42/3_MSN1364; M42/3_MSN1365; M42/3_MSN1366; M42/3_MSN1367; M42/3_MSN1368; M42/3_MSN1369; M42/3_MSN1370; M6/7; M6/7_MSN100; M6/7_MSN116; M6/7_MSN119; M6/7_MSN125; M6/7_MSN137; M6/7_MSN140; M6/7_MSN148; M6/7_MSN150; M6/7_MSN91; M6/7_MSN95; M6/7_MSN96; Madeira Basin; Meteor (1986); MSN; Multiple opening/closing net; NE Atlantic; North Atlantic; Northeast Atlantic; Norwegian Sea; Paleoceanography at Tübingen University; PO200F; POS200/6; POS200/6_MSN837; POS231/3; POS231/3_MSN1329; POS231/3_MSN1330; POS231/3_MSN1331; POS231/3_MSN1332; POS231/3_MSN1333; POS231/3_MSN1334; POS231/3_MSN1335; POS231/3_MSN1336; POS231/3_MSN1337; POS231/3_MSN1338; POS247; POS247/2_MSN1371; POS247/2_MSN1372; POS247/2_MSN1373; POS247/2_MSN1374; POS247/2_MSN1375; POS247/2_MSN1376; POS247/2_MSN1377; POS247/2_MSN1378; POS247/2_MSN1379; POS247/2_MSN1380; POS247/2_MSN1381; POS247/2_MSN1382; POS247/2_MSN1383; POS247/2_MSN1384; POS247/2_MSN1385; POS247/2_MSN1386; POS247/2_MSN1387; POS247/2_MSN1388; POS247/2_MSN1389; POS247/2_MSN1390; POS247/2_MSN1391; Poseidon; Rockall Plateau
    Type: Dataset
    Format: application/zip, 153 datasets
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  • 59
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Ragueneau, Olivier; Gallinari, Morgane; Corrin, Lydie; Grandel, Sibylle; Hall, Per; Hauvespre, Anne; Lampitt, Richard Stephen; Rickert, Dirk; Ståhl, Henrik; Tengberg, Anders; Witbaard, Rob (2001): The benthic silica cycle in the Northeast Atlantic: annual mass balance, seasonality, and importance of non-steady-state processes for the early diagenesis of biogenic opal in deep-sea sediments. Progress in Oceanography, 50(1-4), 171-200, https://doi.org/10.1016/S0079-6611(01)00053-2
    Publication Date: 2024-04-18
    Description: Within the framework of the EU-funded BENGAL programme, the effects of seasonality on biogenic silica early diagenesis have been studied at the Porcupine Abyssal Plain (PAP), an abyssal locality located in the northeast Atlantic Ocean. Nine cruises were carried out between August 1996 and August 1998. Silicic acid (DSi) increased downward from 46.2 to 213 µM (mean of 27 profiles). Biogenic silica (BSi) decreased from ca. 2% near the sediment-water interface to 〈1% at depth. Benthic silicic acid fluxes as measured from benthic chambers were close to those estimated from non-linear DSi porewater gradients. Some 90% of the dissolution occurred within the top 5.5 cm of the sediment column, rather than at the sediment-water interface and the annual DSi efflux was close to 0.057 mol Si/m**2/yr. Biogenic silica accumulation was close to 0.008 mol Si/m**2/yr and the annual opal delivery reconstructed from sedimentary fluxes, assuming steady state, was 0.065 mol Si/m**2/yr. This is in good agreement with the mean annual opal flux determined from sediment trap samples, averaged over the last decade (0.062 mol Si/m**2/yr). Thus ca. 12% of the opal flux delivered to the seafloor get preserved in the sediments. A simple comparison between the sedimentation rate and the dissolution rate in the uppermost 5.5 cm of the sediment column suggests that there should be no accumulation of opal in PAP sediments. However, by combining the BENGAL high sampling frequency with our experimental results on BSi dissolution, we conclude that non-steady state processes associated with the seasonal deposition of fresh biogenic particles may well play a fundamental role in the preservation of BSi in these sediments. This comes about though the way seasonal variability affects the quality of the biogenic matter reaching the seafloor. Hence it influences the intrinsic dissolution properties of the opal at the seafloor and also the part played by non-local mixing events by ensuring the rapid transport of BSi particles deep into the sediment to where saturation is reached.
    Keywords: 12925-008; 12926-002; 12930-040; 12930-045; 12930-075; 12930-082; 12930-087; 13077-018; 13077-021; 13077-035; 13077-057; 13078-019; 13200-012; 13200-024; 13200-026; 13200-032; 13200-059; 13200-074; 13201-005; 13368-040; 362; 54301-002; 54301-010; 54301-023; ALBEX lander; Bengal; BENGAL; Benthic Biology and Geochemistry of a North-eastern Atlantic Abyssal Locality; CH135; Challenger; D222/1; D222/2; D226; D229; D231; D236; DI236_11-1; Discovery (1962); GBGL; GBGL-01; GBGL-02; Göteborg lander; M36/6; M36/6_MC33; M42/2; M42/2_365; M42/2_367; M42/2_377-6; M42/2_381; M42/2_397-1; M42/2_422; M42/2_425; M42/2_432-1; M42/2_433; M42/2_MC2; M42/2_MC28; M42/2_MC30; M42/2_MC32; M42/2_MC34; M42/2_MC5; M42/2_MC9; MCB57; MCS; Meteor (1986); MUC; MultiCorer; MultiCorer, small; MultiCorer Barnett pattern (12-57); NIOZL
    Type: Dataset
    Format: application/zip, 33 datasets
    Location Call Number Expected Availability
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  • 60
    facet.materialart.
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    PANGAEA
    In:  Supplement to: Heinz, Petra; Hemleben, Christoph (2003): Regional and seasonal variations of recent benthic deep-sea foraminifera in the Arabian Sea. Deep Sea Research Part I: Oceanographic Research Papers, 50(3), 435-447, https://doi.org/10.1016/S0967-0637(03)00014-1
    Publication Date: 2024-04-18
    Description: Assemblages of living deep-sea benthic foraminifera, their densities, vertical distribution pattern, and diversity, were investigated in the intermonsoon period after the northeast monsoon in the Arabian Sea in spring 1997. Foraminiferal numbers show a distinct gradient from north to south, with a maximum of 623 foraminifera in 50 cm**3 at the northern site. High percentages of small foraminifera were found in the western and northern part of the Arabian Sea. Most stations show a typical vertical distribution with a maximum in the first centimeter and decreasing numbers with increasing sediment depths. But at the central station, high densities can be found even in deeper sediment layers. Diversity is very high at the northern and western sites, but reduced at the central and southern stations. Data and faunal assemblages were compared with studies carried out in 1995. A principal component analysis of intermonsoon assemblages shows that the living benthic foraminifera can be characterized by five principal component communities. Dominant communities influencing each site differ strongly between the two years. In spring 1997, stations in the north, west and central Arabian Sea were dominated by opportunistic species, indicating the influence of fresh sedimentation pulses or enhanced organic carbon fluxes after the northeast monsoon.
    Keywords: 30#3, SAST; 58#3, CAST; 70#3, NAST; 88#3, WAST; 90#2, WAST-T; BIGSET; BIGSET-1; Biogeochemical Fluxes of Matter and Energy in the Deep Sea; Central Arabian Sediment Trap; MUC; MultiCorer; Northern Arabian Sediment Trap; SO118; SO118_MC-18; SO118_MC-35; SO118_MC-43; SO118_MC-51; SO118_MC-52; Sonne; Southern Arabian Sediment Trap; Western Arabian Sediment Trap; Western Arabian Sediment Trap-Kuppe
    Type: Dataset
    Format: application/zip, 30 datasets
    Location Call Number Expected Availability
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  • 61
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Heinz, Petra; Hemleben, Christoph (2006): Foraminiferal response to the Northeast Monsoon in the western and southern Arabian Sea. Marine Micropaleontology, 58(2), 103-113, https://doi.org/10.1016/j.marmicro.2005.10.001
    Publication Date: 2024-04-18
    Description: Sediments from the western and southern part of the Arabian Sea were collected periodically in the spring intermonsoon between March and May 1997 and additionally at the end of the Northeast Monsoon in February 1998. Assemblages of Rose Bengal stained, living deep-sea benthic foraminifera, their densities, vertical distribution pattern, and diversity were analysed after the Northeast Monsoon and short-time changes were recorded. In the western Arabian Sea, foraminiferal numbers increased steadily between March and the beginning of May, especially in the smaller size classes (30-63 µm, 63-125 µm). At the same time, the deepening of the foraminiferal living horizon, variable diversity and rapid variations between dominant foraminiferal communities were observed. We interpret these observations as the time-dependent response of benthic foraminifera to enhanced organic carbon fluxes during and after the Northeast Monsoon. In the southern Arabian Sea, constant low foraminiferal abundances during time, no distinctive change in the vertical distribution, reduced diversity, and more stable foraminiferal communities were noticed, which indicates no or little influence of the Northeast Monsoon to benthic foraminifera in this region.
    Keywords: 19#4; 2#2; 23/25; 24/03; 32; 4#2; 7/30; 7#4; Arabian Sea; BIGSET; BIGSET-1; BIGSET-2/JGOFS-IN-4; Biogeochemical Fluxes of Matter and Energy in the Deep Sea; JGOFS-IN-1; JGOFS-IN-2; MUC; MultiCorer; SO117; SO117_MC464; SO117_MC468; SO117_MC469; SO118; SO118_MC-02; SO118_MC-04; SO119; SO119_MC501; SO129; SO129_MC-03; SO129_MC-09; SO129_MC-14; Sonne; Southern Arabian Sediment Trap; Western Arabian Sediment Trap; Western Arabian Sediment Trap-Kuppe; Western Arabian Sediment Trap Plain; Western Arabian Sediment Trap Top
    Type: Dataset
    Format: application/zip, 52 datasets
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  • 62
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    PANGAEA
    In:  Supplement to: Pfannkuche, Olaf; Soltwedel, Thomas (1998): Small benthic size classes along the N.W. European Continental Margin: spatial and temporal variability in activity and biomass. Progress in Oceanography, 42(1-4), 189-207, https://doi.org/10.1016/S0079-6611(98)00034-2
    Publication Date: 2024-04-18
    Description: In the context of the European OMEX Programme this investigation focused on gradients in the biomass and activity of the small benthic size spectrum along a transect across the Goban Spur from the outer Celtic Sea into Porcupine Abyssal Plain. The effects of food pulses (seasonal, episodic) on this part of the benthic size spectrum were investigated. Sediments sampled during eight expeditions at different seasons covering a range from 200 m to 4800 m water depth were assayed with biochemical bulk measurements: determinations of chloroplastic pigment equivalents (CPE), the sum of chlorophyll a and its breakdown products, provide information concerning the input of phytodetrital matter to the seafloor; phospholipids were analyzed to estimate the total biomass of small benthic organisms (including bacteria, fungi, flagellata, protozoa and small metazoan meiofauna). A new term 'small size class biomass' (SSCB) is introduced for the biomass of the smallest size classes of sediment-inhabiting organisms; the reduction of fluorescein-di-acetate (FDA) was determined to evaluate the potential activity of ester-cleaving bacterial exoenzymes in the sediment samples. At all stations benthic biomass was predominantly composed of the small size spectrum (90% on the shelf; 97–98% in the bathyal and abyssal parts of the transect). Small size class biomass (integrated over a 10 cm sediment column) ranged from 8 g C/m**2 on the shelf to 2.1 g C/m**2 on the adjacent Porcupine Abyssal Plain, exponentially decreasing with increasing water depth. However, a correlation between water depth and SSCB, macrofauna biomass as well as metazoan meiofauna biomass exhibited a significantly flatter slope for the small size classes in comparison to the larger organisms. CPE values indicated a pronounced seasonal cycle on the shelf and upper slope with twin peaks of phytodetrital deposition in mid spring and late summer. The deeper stations seem to receive a single annual flux maximum in late summer. SSCB and heterotrophic activity are significantly correlated to the amount of sediment-bound pigments. Seasonality in pigment concentrations is clearly followed by SSCB and activity. In contrast to macro- and megafauna which integrate over larger periods (months/years), the small benthic size classes, namely bacteria and foraminifera, proved to be the most reactive potential of the benthic communities to any perturbations on short time scales (days/weeks). The small size classes, therefore, occupy a key role in early diagenetic processes.
    Keywords: 425; 426; 427; 428; 429; 430; 431; 434; 435; 79401; ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Goban Spur; M27/1; M27/1_79401; M30/1; M30/1_MC24; M30/1_MC25; M30/1_MC26; M30/1_MC27; M30/1_MC28; M30/1_MC29; M30/1_MC30; M30/1_MC31; M30/1_MC32; M30/1_MC33; Meteor (1986); MUC; MultiCorer; NE Atlantic; Porcupine Abyssal Plain
    Type: Dataset
    Format: application/zip, 11 datasets
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  • 63
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    PANGAEA
    In:  Supplement to: Pfannkuche, Olaf; Boetius, Antje; Lundgreen, Ulrich; Lochte, Karin; Thiel, Hjalmar (1999): Responses of deep-sea benthos to sedimentation patterns in the North-East Atlantic in 1992. Deep Sea Research Part I: Oceanographic Research Papers, 46(4), 573-596, https://doi.org/10.1016/S0967-0637(98)00081-8
    Publication Date: 2024-04-18
    Description: In an extended deep-sea study the response of the benthic community to seasonally varying sedimentation rates of organic matter were investigated at a fixed abyssal site in the NE Atlantic (BIOTRANS station or JGOFS station L2 at 47°N-20°W, water depth 〉4500 m) on four legs of METEOR expedition 21 between March and August 1992. The vertical flux at 3500 m depth and temporal variations in the chloroplastic pigment concentration, a measure of phytodetritus deposition, and of total adenylates and total phospholipids, measures of benthic biomass, and of activity of hydrolytic enzymes were observed. The flux patterns in moored sediment traps of total chlorophyll, POC and total flux showed an early sedimentation peak in March/April 1992, followed by low fluxes in May and intermediate ones from June to August. Thus 1992 differed from other years, in which one large flux peak after the spring phytoplankton bloom was observed. Unusually high concentrations of chloroplastic pigments were consistently observed in March 1992, reflecting the early sedimentation input. At the same time biomass of small benthic organisms (bacteria to meiobenthos) and activity of hydrolytic enzymes were higher compared to values from March 1985 and from the following months in 1992. In May and August 1992 pigment concentrations and biomass and activity parameters in the sediment were lower than during previously observed depositions of phytodetrital matter in summer. The data imply that the deep ocean benthic community reacts to small sedimentation events with transient increases in metabolic activity and only small biomass production. The coupling between pelagic and benthic processes is so close that interannual variability in surface water production is "mirrored" by deep-sea benthic processes.
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Biotrans; Iceland Basin; JGOFS; Joint Global Ocean Flux Study; M21/1; M21/1_MC373; M21/1_MC375; M21/1_MC376; M21/1_MC378; M21/1_MC379; M21/1_MC380; M21/1_MC381; M21/1_MC382; M21/1_MC383; M21/1_MC386; M21/1_MC387; M21/1_MC388; M21/1_MC389; M21/1_MC390; M21/1_MC391; M21/2; M21/2_MC394; M21/2_MC395; M21/2_MC396; M21/2_MC398; M21/2_MC399; M21/2_MC400; M21/3; M21/3_MC401; M21/3_MC402; M21/3_MC403; M21/3_MC404; M21/3_MC405; M21/3_MC407; M21/3_MC408; M21/3_MC409; M21/3_MC415; M21/3_MC416; M21/3_MC417; M21/6; M21/6_MC424; M21/6_MC426; M21/6_MC434; M21/6_MC435; M21/6_MC439; M21/6_MC446; M21/6_MC447; M21/6_MC448; M21/6_MC452; M21/6_MC454; M21/6_MC456; M27/2; M27/2_MC358; M27/2_MC469; M27/2_MC470; M27/2_MC471; M27/2_MC472; Madeira Basin; Meteor (1986); MUC; MultiCorer
    Type: Dataset
    Format: application/zip, 66 datasets
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  • 64
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    PANGAEA
    In:  Supplement to: Teichert, Barbara M A; Eisenhauer, Anton; Bohrmann, Gerhard; Haase-Schramm, Alexandra; Bock, Barbara; Linke, Peter (2003): U/Th systematics and ages of authigenic carbonates from Hydrate Ridge, Cascadia Margin: Recorders of fluid flow variations. Geochimica et Cosmochimica Acta, 67(20), 3845-3857, https://doi.org/10.1016/S0016-7037(03)00128-5
    Publication Date: 2024-04-18
    Description: Uranium (U) concentrations and activity ratios (d234U) of authigenic carbonates are sensitive recorders of different fluid compositions at submarine seeps of hydrocarbon-rich fluids ("cold seeps") at Hydrate Ridge, off the coast of Oregon, USA. The low U concentrations (mean: 1.3 ± 0.4 µg/g) and high 234U values (165-317 per mil) of gas hydrate carbonates reflect the influence of sedimentary pore water indicating that these carbonates were formed under reducing conditions below or at the seafloor. Their 230Th/234U ages span a time interval from 0.8 to 6.4 ka and cluster around 1.2 and 4.7 ka. In contrast, chemoherm carbonates precipitate from marine bottom water marked by relatively high U concentrations (mean: 5.2 ± 0.8 µg/g) and a mean d234U ratio of 166 ± 3 per mil. Their U isotopes reflect the d234U ratios of the bottom water being enriched in 234U relative to normal seawater. Simple mass balance calculations based on U concentrations and their corresponding d234U ratios reveal a contribution of about 11% of sedimentary pore water to the bottom water. From the U pore water flux and the reconstructed U pore water concentration a mean flow rate of about 147 ± 68 cm/a can be estimated. 230Th/234U ages of chemoherm carbonates range from 7.3 to 267.6 ka. 230Th/234U ages of two chemoherms (Alvin and SE-Knoll chemoherm) correspond to time intervals of low sealevel stands in marine isotope stages (MIS) 2, 4, 5, 6, 7 and 8. This observation indicates that fluid flow at cold seep sites sensitively reflects pressure changes of the hydraulic head in the sediments. The d18OPDB ratios of the chemoherm carbonates support the hypothesis of precipitation during glacial times. Deviations of the chemoherm d18O values from the marine d18O record can be interpreted as to reflect temporally and spatially varying bottom water and/or vent fluid temperatures during carbonate precipitation between 2.6 and 8.6°C.
    Keywords: 3424-4-A; 3428-6-A; 3429-3-A; 36/4TV-G; AT3-35B; Atlantis (1997); Bottom water sampler; BWS; Gravity corer (Kiel type); HYDROTRACE; Manipulator arm; Multicorer with television; Ocean Floor Observation System; OFOS; OFOS-6; Oregon Vent; Remote operated vehicle; ROV; ROV_MA; SL; SO109/1; SO109/1_36-4; SO143_21-2; SO143_221-2; SO143_222; SO143_55-2; SO143_55-5; SO143_56-1; SO143_60-1; SO143/1b; SO143/3; SO148/1; SO148/1_26; SO148/1_565-7; SO148/1_566-1; SO148/1_570-1; SO148/2; SO148/2_570-9; SO148/2_571-1; SO148/2_571-2; SO148/2_571-3; Sonne; TECFLUX I; TECFLUX II; Television-Grab; TVG; TVMUC
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 65
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    PANGAEA
    In:  Supplement to: Stumpf, Roland; Frank, Martin; Schönfeld, Joachim; Haley, Brian A (2010): Late Quaternary variability of Mediterranean Outflow Water from radiogenic Nd and Pb isotopes. Quaternary Science Reviews, 29(19-20), 2462-2472, https://doi.org/10.1016/j.quascirev.2010.06.021
    Publication Date: 2024-04-18
    Description: Mediterranean Outflow Water (MOW) is characterised by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m in the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. We used high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese coatings of sediments in three gravity cores at 577, 1745 and 1974 m water depth in the Gulf of Cadiz and along the Portuguese margin complemented by a selection of surface sediments to reconstruct the extent and pathways of MOWover the past 23 000 years. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station. In contrast, the Pb isotope records show significant and systematic variations, which provide evidence for a significantly different pattern of the MOW pathways between 20 000 and 12 000 years ago compared with the subsequent period of time.
    Keywords: BC; Box corer; GC; GC10; GC22; GC45; Gravity corer; Gravity corer (Kiel type); Gulf of Cádiz, Atlantic Ocean; LV044-316; M39/1; M39/1_08-3; M39/1_36-4; M39/1_58-2; M39008-3; M39058-2; Maria S. Merian; Meteor (1986); MSM01/3; MSM01/3_139; MSM01/3_161; MSM01/3_168; MSM01/3_183; MSM01/3_190-2; MSM01/3_237-1; MSM01/3_240; MSM01/3_331; MUC; MUC11; MUC2; MUC4; MUC6; MUC9; MultiCorer; PALEO 1; Portuguese Margin; POS287; POS287_08-1B; POS287_14-1B; POS287_26-1B; Poseidon; SL
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 66
    Publication Date: 2024-04-18
    Description: The ADEPD project compiled biological and biogeochemical data from a range of international and national deep sea projects in the information system PANGAEA. Diverse data sets were brought together in an uniform data format and are made available to a wider public. More than one hundred biogeochemical variables and 114,000 published and unpublished data sets were compiled in the last two years in PANGAEA. A new and very simple approach to the data base via the world wide web was implemented. Now for the first time a large deep sea data base is easily accessible for the general public on: http://www.pangaea.de/Projects/ADEPD.
    Keywords: 323; 326; 329; ADEPD; ANT-IV/1a; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; BIO-CFluxStation256; BIO-CFluxStation265; BIO-CFluxStation290; BIO-CFluxStation298; BIO-CFluxStation303; BIO-CFluxStation304; BIO-CFluxStation305; BIO-CFluxStation313; BIO-CFluxStation314; BIO-CFluxStation316; BIO-CFluxStation319; BIO-CFluxStation327; Biotrans; Cape Verde Basin; Giant box corer; GKG; Goban Spur; Iceland Basin; M10/4; M10/4_MC220; M10/4_MC221; M10/4_MC225; M10/4_MC226; M10/4_MC230; M10/4_MC232; M10/4_MC234; M10/4_MC237; M10/4_MC238; M10/4_MC240; M10/4_MC242; M10/4_MC243; M10/4_MC250; M10/4_MC253; M10/4_MC255; M10/4_MC257; M10/4_MC260; M10/4_MC261; M10/4_MC262; M10/4_MC263; M10/4_MC264; M10/4_MC265; M10/4_MC266; M12/3; M12/3_MC301; M12/3_MC302; M12/3_MC305; M12/3_MC307; M12/3_MC309; M12/3_MC311; M12/3_MC313; M12/3_MC315; M12/3_MC316; M12/3_MC317; M12/3_MC319; M12/3_MC320; M12/3_MC321; M12/3_MC323; M12/3_MC325; M21/6; M21/6_MC419; M21/6_MC422; M21/6_MC423; M21/6_MC424; M21/6_MC426; M21/6_MC434; M21/6_MC435; M21/6_MC439; M21/6_MC441; M21/6_MC442; M21/6_MC446; M21/6_MC447; M21/6_MC448; M21/6_MC452; M21/6_MC454; M21/6_MC456; M3; M3/1_KG1113; M3/1_KG1133; M3/1_KG1135; M3/1_KG1138; M3/1_KG1143; M3/1_MC40; M3/1_MC41; M3/1_MC44; M3/1_MC47; M3/1_MC48; M3/1_MC52; M3/1_MC55; M3/1_MC59; M3/1_MC60; M3/1_MC63; M3/1_MC68; M53; M53_155-4; M53_158-4; M53_162-4; M53_164-4; M53_166-4; M53_168-1; M53_169-2; M53_170-1; M53_173-2; M53_KG-804; M53_KG-808; M53_KG-812; M53_KG-816; M53_KG-820; M53_KG-822; M53_KG-824; M53_KG-827; M53_KG-833; M6/3; M6/3_MC128; M6/3_MC130; M6/7; M6/7_MC135; M6/7_MC141; M6/7_MC142; M6/7_MC144; M6/7_MC145; M6/7_MC147; M6/7_MC148; M6/7_MC153; M6/7_MC155; M6/7_MC157; M6/7_MC158; M6/7_MC159; M6/7_MC161; M6/7_MC162; M6/7_MC166; M6/7_MC170; M69; M69_KG1046; M69_KG1047; M69_KG1048; M69_KG1049; M69_KG1050; M69_KG1051; M69_KG1052; M69_KG1053; M69_MC10; M70; M70_KG1055; M70_KG1057; M70_KG1059; M70_KG1063; M70_KG1064; M70_KG1067; M70_KG1070; M70_KG1073; M70_KG1075; M70_KG1076; M70_KG1078; M70_KG1081; M70_KG1084; M70_MC11; M70_MC12; M70_MC13; M70_MC14; M70_MC15; M70_MC16; M70_MC17; M70_MC18; M70_MC19; M70_MC20; M70_MC21; M70_MC22; M70_MC23; M70_MC24; Meteor (1964); Meteor (1986); MUC; MultiCorer; NOAMP II; NOAMP III; NOAMP IV; North Atlantic Ocean; Northeast Atlantic; off West Africa; Polarstern; Porcupine Abyssal Plain; PS08_KG1088; PS08_KG1101; PS08_KG1103; PS08_KG1107; PS08_MC25; PS08_MC27; PS08_MC28; PS08_MC31; PS08_MC33; PS08_MC35; PS08_MC37; PS08_MC39; PS08 NOAMP; Sierra Leone Basin; SO31; SO31_KG1031; SO31_KG1033; SO31_KG1036; SO31_KG1038; SO31_KG1042; SO31_MC04; SO31_MC05; SO31_MC06; SO31_MC07; SO31_MC08; SO31_MC09; Sonne
    Type: Dataset
    Format: application/zip, 396 datasets
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  • 67
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-310_042; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 492 data points
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  • 68
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-311_043; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 720 data points
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  • 69
    Publication Date: 2024-04-18
    Keywords: 35#3; BIGSET-1; Biogeochemical flux in the deep sea; Calculated from weight/volume; DEPTH, sediment/rock; GEOMARFLUX; Gravity corer (Kiel type); Ion selective probe; Oxidation reduction (RedOx) potential; pH; Porosity; SL; SO118; SO118_SL-01; Sonne; Southern Arabian Sediment Trap
    Type: Dataset
    Format: text/tab-separated-values, 51 data points
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  • 70
    Publication Date: 2024-04-18
    Keywords: 53#2; Aluminium; Barium; BIGSET-1; Biogeochemical flux in the deep sea; Cadmium; Calcium; Calculated from weight/volume; Carbon, organic, total; Copper; DEPTH, sediment/rock; Element analyser CHN; GEOMARFLUX; Graphite furnace atomic absorption spectrometer (GF-AAS); Gravity corer (Kiel type); Inductively coupled plasma atomic emission spectroscope (ICP-AES); Ion selective probe; Iron; Lead; Magnesium; Manganese; Oxidation reduction (RedOx) potential; pH; Porosity; Silicate; SL; SO118; SO118_SL-02; Sonne; Titanium; Western Arabian Sediment Trap
    Type: Dataset
    Format: text/tab-separated-values, 525 data points
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  • 71
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-315_048; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 72
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-315_049; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 596 data points
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  • 73
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-317_052; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2572 data points
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  • 74
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-320_057; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1992 data points
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  • 75
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-325_067; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 7136 data points
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  • 76
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-326_069; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 7272 data points
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  • 77
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-328_073; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 4944 data points
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  • 78
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    In:  Supplement to: Caballero-Gill, Rocio P; Herbert, Timothy D; Dowsett, Harry J (2019): 100‐kyr Paced Climate Change in the Pliocene Warm Period, Southwest Pacific. Paleoceanography and Paleoclimatology, 34(4), 524-545, https://doi.org/10.1029/2018PA003496
    Publication Date: 2024-04-18
    Description: The mid to late Pliocene (~4.2-2.8 Ma.) represents an experiment in climate sensitivity to orbital pacing in which nearly all continental ice was confined to the Southern Hemisphere. Most studies have emphasized the dominant role of obliquity in determining changes in ice volume and temperature at this time, although most records come from the Northern Hemisphere, instead of the hemisphere where the bulk of ice resided. We present the first orbitally-resolved, mid to late Pliocene Southern Hemisphere paired records of surface and subsurface variability from two deep ocean archives from the Southwest Pacific Ocean (Sites 594 and 1125). These records indicate dominance of low frequencies centered at ~100 kyr for this time period. Because these signatures extend coherently and synchronously from mid-depth water properties (δ13C, δ18O of benthic foraminifera), which have their chemistry set in the subantarctic belt, to the surface (alkenone-derived surface temperature estimates, color reflectance, and magnetic susceptibility), we infer the fingerprint of the ~100 kyr cycles must have extended over a large region of the Southern Hemisphere. We propose that nonlinearities in climate response to precessional forcing- most likely through ice sheet and/or carbon cycle behavior- generated the observed low frequency. A review of published mid to late Pliocene time series suggests the ~100 kyr pacing may be a widespread phenomenon and that major circa-100 kyr excursions in Pliocene climate were an important overlay to the underlying 41 kyr glacial-interglacial rhythm. These results caution against uncritical use of existing Pliocene isotopic templates to construct high-resolution age models.
    Keywords: benthic foraminifera stable isotopes; Deep Sea Drilling Project; DSDP; DSDP 594; mid-late Pliocene; Ocean Drilling Program; ODP; ODP 1125; Southwest Pacific; Uk'37 sst and C37total
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 79
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    Unknown
    PANGAEA
    In:  Supplement to: Cornils, Astrid; Sieger, Rainer; Mizdalski, Elke; Schumacher, Stefanie; Grobe, Hannes; Schnack-Schiel, Sigrid B (2018): Copepod species abundance from the Southern Ocean and other regions (1980 - 2005) - a legacy. Earth System Science Data, 10, 1457-1471, https://doi.org/10.5194/essd-10-1457-2018
    Publication Date: 2024-04-18
    Description: This data collection originates from the efforts of Sigrid Schnack-Schiel (1946–2016), a zooplankton ecologist with great expertise in life cycle strategies of Antarctic calanoid copepods, who also investigated zooplankton communities in tropical and subtropical marine environments. Here, we present 33 data sets with abundances of planktonic copepods from 20 expeditions to the Southern Ocean (Weddell Sea, Scotia Sea, Amundsen Sea, Bellingshausen Sea, Antarctic Peninsula), one expedition to the Magellan region, one latitudinal transect in the eastern Atlantic Ocean, one expedition to the Great Meteor Bank, and one expedition to the northern Red Sea and Gulf of Aqaba as part of her scientific legacy. A total of 349 stations from 1980 to 2005 were archived. During most expeditions depth-stratified samples were taken with a Hydrobios multinet with five or nine nets, thus allowing inter-comparability between the different expeditions. A Nansen or a Bongo net was deployed only during four cruises. Maximum sampling depth varied greatly among stations due to different bottom depths. However, during 11 cruises to the Southern Ocean the maximum sampling depth was restricted to 1000m, even at locations with greater bottom depths. In the eastern Atlantic Ocean (PS63) sampling depth was restricted to the upper 300m.
    Keywords: AWI_BPP; Bentho-Pelagic Processes @ AWI
    Type: Dataset
    Format: application/zip, 33 datasets
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  • 80
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    Unknown
    PANGAEA
    In:  Supplement to: Seiter, Katherina; Hensen, Christian; Schröter, Jürgen; Zabel, Matthias (2004): Organic carbon content in surface sediments-defining regional provinces. Deep Sea Research Part I: Oceanographic Research Papers, 51(12), 2001-2026, https://doi.org/10.1016/j.dsr.2004.06.014
    Publication Date: 2024-04-18
    Description: Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (〈5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.
    Keywords: 0010PG; 0029PG; 0036PG; 0038PG; 01_BC1; 01BOX; 01BOXC; 01BOXG; 02_BC5; 02BOX; 02BOXC; 02BOXG; 03_BC4; 03BOX; 03BOXG; 03MULC; 04_BC4; 04BOX; 04BOXG; 04MULC; 05_BC5; 05BOX; 05BOXG; 05MULC; 06_BC5; 06BOX; 06BOXG; 06MT28_2; 06MULC; 07_BC4; 07BOX; 07BOXG; 07MULC; 08_BC5; 08BOX; 08BOXG; 08MULC; 09_BC1; 09BOX; 09BOXG; 09MULC; 10_BC4; 10103-1B; 10103-8K; 108-663; 108-663A; 108-664; 108-664B; 10BOX; 11_BC8; 110#1, M31/3-110.1_MC2; 11B; 11BC39; 11BOX; 12B; 12BC47-2; 12BOX; 13B; 13BCP56; 13BOX; 14B; 14BOX; 159-959; 159-959C; 159-962; 159-962B; 15B; 167-1011; 167-1018; 167-1019; 167-1020; 167-1021; 16B; 179KG; 17B; 17 m-Lake; 185KG; 186KG; 188KG; 193KG; 194KG; 1BC1-2; 200227; 200228; 200229; 200230; 200231; 201MX; 202KG; 204KG; 209KG; 210MX; 212KG; 215KG; 216KG; 234KG; 236KG; 24#1; 243K; 252KG; 255KG; 26-258A; 264KG; 27#2; 280K; 290KG; 292KG; 2BC5-1; 30#3, SAST; 30#4; 3-14; 371; 373; 375; 376; 377; 379; 380; 381; 382; 383; 386; 388; 39#1; 4#2; 403; 406; 41; 414; 415; 416; 423; 424; 428; 429; 431; 432; 433; 434; 4399-1; 440; 4403-1; 4411-1; 4414-1; 4418-1; 442; 443; 444; 449; 451; 452; 453; 455; 460; 49-407; 4B; 4BC14-2; 4IMP11; 50#4; 53#1; 58#3, CAST; 581, NAST; 5B; 6#2; 603; 637; 641; 655; 655, EAST; 661, EAST; 669; 67#2; 6B; 6BC20-2; 70#1; 76#2; 76#3; 7B; 8-73; 88#1; 8B; 8BC27-3; 92#1; 92#3; 9B; 9BC26; A_EN179-BC1; A_EN179-BC2; A_EN179-BC3; A_EN179-BC4; A_EN179-BC5; A_EN179-BC7; A_EN187-BC1; A_EN187-BC10; A_EN187-BC11; A_EN187-BC3; A_EN187-BC4; A_EN187-BC5; A_EN187-BC6; A_EN187-BC8; A_EN187-BC9; A-10-VG; A-15-VG; A-16-BG; A-17-BG; A-19-VG; A-1-VG; A-20-BG; A-21; A-23-VG; A-24; A-25-BG; A-262; A-27-VG; A-28-BG; A-29-BG; A-30; A-31-VG; A-32; A-33-BG; A-34-BG; A-36-BG; A-37-BG; A-38; A-39; A-40-BG; A-41-BG; A-6-BG; A-7-BG; A84-01; A84-02; A84-03; A84-04; A84-05; A84-06; A84-07; A84-08; A84-09; A84-11; A84-12; A84-13; A84-14; A84-15; A84-17; A84-18; A84-19; A84-21; A84-22; A84-23; A84-24; A84-25; A84-26; A84-27; A84-28; A-8-BG; A-9; Achterwasser; ADEPDCruises; ADS; Agadir Canyon; Agulhas Basin; AK1-10; AK1-12; AK11-880; AK11-882; AK11-918; AK11-927; AK11-928; AK11-929; AK11-981; AK1-2; AK1-3; AK1-5; AK3-100; AK3-101,2; AK3-108; AK3-130; AK3-136; AK3-137; AK3-138; AK3-140; AK3-141; AK3-142; AK3-143; AK3-144; AK3-145; AK3-147; AK3-150,3; AK3-151; AK3-152; AK3-153; AK3-157; AK3-158; AK3-159; AK3-160; AK3-161; AK3-163; AK3-166; AK3-167; AK3-168; AK3-170,2; AK3-171; AK3-175; AK3-185; AK3-203; AK3-205; AK3-208; AK3-209; AK3-210; AK3-51; AK3-52; AK3-53,2; AK3-53,3; AK3-54; AK3-55; AK3-56; AK3-59,2; AK3-87,2; AK3-95; AK3-97; AK3-98; AK3-99; AK40-4306; AK40-4323; AK40-4324; AK40-4333; AK40-4334; AK43-4834; AK43-4877; AK43-4878; AK43-4879; AK43-4880; AK43-4881; AK43-4882; AK43-4889; AK43-4890; AK43-4891; AK43-4896; AK43-4898; AK43-4899; AK43-4900; AK43-4901; AK43-4902; AK43-4903; AK43-4904; AK43-4905; AK43-4907; AK43-4910; AK43-4912; AK43-4923; AK43-4925; AK43-4926; AK43-4928; AK43-4929; AK43-4931; AK43-4933; AK43-4934; AK43-4935; AK43-4936; AK43-4938; AK43-4940; AK43-4943; AK43-4945; AK43-4946; AK43-4949; AK43-4952; AK43-4955; AK43-4956; AK5-327,1; AK5-328,2; AK5-332,2; AK5-333,2; AK5-337,2; AK5-340,2; AK5-345; AK5-351; AK5-352,2; AK5-356; AK5-362; AK5-366,2; AK5-375; AK5-376,2; AK5-377,2; AK5-378; AK5-400,2; AK5-402; AK5-403; AK5-405; AK5-414; AK5-416,2; AK5-419; AK5-421,2; AK6-431-1; AK6-431-2; AK6-435; AK6-436; AK6-439; AK6-440; AK6-441-1; AK6-441-3; AK6-441-6a; AK6-441-7; AK6-441-9; AK6-443-9; Akademik Boris Petrov; Akademik Kurchatov; Akademik Nikolaj Strakhov; Akademik Sergey Vavilov; AKU1; AKU11; AKU3; AKU40; AKU43; AKU5; AKU6; AL63; Alexander von Humboldt; Alkor (1990); ALV76; Alv-ADS; Alv-DOS-1; Alv-DOS-2; Alv-DS-1; Alv-DWD; Alvin; Amazon Fan; Amazon Shelf/Fan; Amundsen Basin; Amundsen Sea; Andromeda; Angola Basin; Angola Benguela Front; Angola Diapir Field; ANIRO; ANIRO-611; ANIRO-613; ANIRO-636; ANIRO-641; ANIRO-645; ANIRO-654; ANIRO-657; ANS2; ANS2-1; ANS2-10; ANS2-11; ANS2-12; ANS2-13; ANS2-14; ANS2-15; ANS2-18; ANS2-19; ANS2-2; ANS2-22; ANS2-23; ANS2-24; ANS2-26; ANS2-27; ANS2-3; ANS2-4; ANS2-5; ANS2-6; ANS2-7; ANS2-8; ANS2-9; Antarctic Ocean; ANT-I/2; ANT-II/3; ANT-II/4; ANT-III/3; ANTIPROD; ANT-IV/1c; ANT-IV/3; ANT-IV/4; ANT-IX/3; ANT-IX/4; ANT-V/4; ANT-VI/3; ANT-VIII/3; ANT-VIII/5; ANT-VIII/6; ANT-X/2; ANT-X/4; ANT-XI/2; ANT-XI/3; ANT-XIV/3; AOS94_1; AOS94_12; AOS94_13; AOS94_16; AOS94_17; AOS94_19; AOS94_21; AOS94_23; AOS94_24; AOS94_25; AOS94_26; AOS94_28; AOS94_30; AOS94_31; AOS94_32; AOS94_33; AOS94_6; AOS94_7; AOS94_8; APSARA4; Arabian Sea; Arctic Ocean; Argentine Basin; Argentine Islands; Argentinian Basin; Argo; ARIES; ARIES-040PG; ARIES-045PG; ARIES-048G; ARK-I/3; ARK-II/5; ARK-III/3; ARK-IV/3; ARK-IX/3; ARK-IX/4; Arkona Basin; ARK-V/2; ARK-V/3b; ARK-VI/2; ARK-VII/1; ARK-VII/3b; ARK-VIII/2; ARK-VIII/3; ARK-XI/1; Arlis Plateau; ASV11; ASV11-1006; ASV11-1006.1; ASV11-1024; ASV11-1026; ASV11-1054; ASV11-829; ASV11-830; ASV11-831; ASV11-833; ASV11-835; ASV11-837; ASV11-838; ASV11-841; ASV11-842; ASV11-844; ASV11-847; ASV11-850; ASV11-853; ASV11-855; ASV11-858; ASV11-860; ASV11-861; ASV11-863; ASV11-865; ASV11-867; ASV11-869; ASV11-873; ASV11-875; ASV11-877; ASV11-879; ASV11-880; ASV11-882; ASV11-883; ASV11-891; ASV11-892; ASV11-894; ASV11-895; ASV11-896; ASV11-897; ASV11-898; ASV11-899; ASV11-900; ASV11-901; ASV11-902; ASV11-987; ASV11-988; ASV12; ASV12_1081-GC; ASV13; ASV13_1018-G; ASV13_1088-G; ASV13_1093-G; ASV13_1094-G; ASV13_1095-G; ASV13_1096-G; ASV13_1097-G; ASV13_1098-G; ASV13_1099-G; ASV13_1101-G; ASV13_1102-G; ASV13_1103-G; ASV13_1104-G; ASV13_1105-G; ASV13_1106-GC; ASV13_1112-G; ASV13_1115-G; ASV13_1117-G; ASV13_1119-G; ASV13_1120-G; ASV13_1121-G; ASV13_1122-G; ASV13_1123-G; ASV13_1124-G; ASV13_1125-G; ASV13_1126-G; ASV13_1127-G; ASV13_1128-G; ASV13_1129-G; ASV13_1132-G; ASV13_1133-G; ASV13_1134-G; ASV13_1135-G; ASV13_1136-G; ASV13_1137-G; ASV13_1139-G; ASV13_1140-G; ASV13_1141-G; ASV13_1142-G; ASV13_1143-G; ASV13_1144-G; ASV13_1145-G; ASV13_1146-G; ASV13_1147-G; ASV13_1148-G; ASV13_1149-G; ASV13_1150-G; ASV13_1151-G; ASV13_1152-G; ASV13_1153-G; ASV13_1154-G; ASV13_1155-G; ASV13_1156-G; ASV13_1158-G; ASV13_1159-G; ASV13_1162-G; ASV13_1163-G; ASV13_1164-G; ASV13_1165-G; ASV13_1201-G; ASV13_1202-G; ATESEPP; Atka Bay; Atlantic Caribbean Margin; Atlantic Ocean; Atlantic Ridge; Aurelia; Aurelia_08_1984; Aurelia_08_1984_01_BC; Aurelia_08_1984_02_BC; Aurelia_08_1984_03_BC; Aurelia_08_1984_04_BC; Aurelia_08_1984_05_BC; Aurelia_08_1984_06_BC; Aurelia_08_1984_07_BC; Aurelia_08_1984_08_BC; Aurelia_08_1984_09_BC; Aurelia_08_1984_11_BC; Aurelia_08_1984_12_BC; Aurelia_08_1984_13_BC; Aurelia_08_1984_14_BC; Aurelia_08_1984_15_BC; Aurelia_08_1984_17_BC; Aurelia_08_1984_18_BC; Aurelia_08_1984_19_BC; Aurelia_08_1984_21_BC; Aurelia_08_1984_22_BC; Aurelia_08_1984_23_BC; Aurelia_08_1984_24_BC; Aurelia_08_1984_25_BC; Aurelia_08_1984_26_BC; Aurelia_08_1984_27_BC; Aurelia_08_1984_28_BC; Auriga; AWI Antarctic Land Expedition; AWI Arctic Land Expedition; B-10-BG; B-11-BG; B-143; B-14-VG; B-16-BG; B-17-BG; B-187; B-18-BG; B-191; B-192; B-19-VG; B-20-VG; B-24-BG; B-26-VG; B-28-BG; B-2-BG; B-33-BG; B-34-BG; B-35-BG; B-37-BG; B-41-BG; B-43-BG; B-44-BG; B-45-BG; B-46-BG; B-4-BG; B-5; B-50-BG; B-51-BG; B-59-BG; B-6; B-61-BG; B-62-BG; B-67-BG; B-69-BG; B-6-VG; B-7; B-70-BG; B-71-BG; B-75-VG; B-76-VG; B-78-BG; B-79-BG; B-7-VG; B-89-BG; B-8-VG; B-9-BG; BA84; BA84-02PC; BA84-03TW; BA84-08GC; Baltic Sea; Bannock; Bannock basin; Barents abyssal plain; Barents Sea; Basalt Sø; Basin-I_BC31; BC; BCORE1; BCORE2; BCORE3; BCORE4; BCORE6; BCORE7; BCR; Bear Island Trough; Bel1; Bel1-611; Bel1-613; Bel1-621; Bel1-636; Bel1-641; Bel1-645; Bel1-654; Bel1-657; Bel2; Bel2-1; Bel2-10; Bel2-100; Bel2-103; Bel2-107; Bel2-11; Bel2-111; Bel2-115; Bel2-12; Bel2-13; Bel2-16; Bel2-18; Bel2-19; Bel2-2; Bel2-20; Bel2-21; Bel2-22; Bel2-24; Bel2-25; Bel2-27; Bel2-28; Bel2-31; Bel2-32; Bel2-33; Bel2-35; Bel2-36; Bel2-37; Bel2-38; Bel2-39; Bel2-4; Bel2-40; Bel2-41; Bel2-42; Bel2-43; Bel2-45; Bel2-47;
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 81
    Publication Date: 2024-04-18
    Keywords: Canary Islands Azores Gibraltar Observations; CANIGO; Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1a; M42/1a-CTD-265_004; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 224 data points
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  • 82
    Publication Date: 2024-04-18
    Keywords: Canary Islands Azores Gibraltar Observations; CANIGO; Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1a; M42/1a-CTD-272_011; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 7344 data points
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  • 83
    Publication Date: 2024-04-18
    Keywords: Canary Islands Azores Gibraltar Observations; CANIGO; Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1a; M42/1a-CTD-279_015; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2560 data points
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  • 84
    Publication Date: 2024-04-18
    Keywords: Canary Islands Azores Gibraltar Observations; CANIGO; Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1a; M42/1a-CTD-278_014; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2380 data points
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  • 85
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-314_047; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 596 data points
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  • 86
    Publication Date: 2024-04-18
    Keywords: Conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; DEPTH, water; ESTOC; European Station for Time-Series in the Ocean Canary Islands; M42/1b; M42/1b-CTD-317_053; Meteor (1986); Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 596 data points
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  • 87
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; BIGSET; Biogeochemical Fluxes of Matter and Energy in the Deep Sea; Calculated; Carbon/Nitrogen ratio; DEPTH, sediment/rock; M36/6; M36/6_368FFR; Meteor (1986); RESP; Respirometer
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 88
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; BIGSET; Biogeochemical Fluxes of Matter and Energy in the Deep Sea; Biotrans; Calculated; Carbon/Nitrogen ratio; DEPTH, sediment/rock; M36/6; M36/6_400FFRc; M36/6_FFR-3; Meteor (1986); RESP; Respirometer
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 89
    Publication Date: 2024-04-18
    Keywords: 395; ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Bacteria, biomass as carbon; Biotrans; DEPTH, sediment/rock; M36/6; M36/6_MC50; Meteor (1986); MUC; MultiCorer
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 90
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH511; Ch511_MC10#1; Ch511-10#1; Challenger; Chlorophyll pigment equivalents; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Seabight
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 91
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH511; Ch511_MC5#2; Ch511-05#2; Challenger; Chlorophyll pigment equivalents; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Seabight
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 92
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH511; Ch511_MC9#3; Ch511-09#3; Challenger; Chlorophyll pigment equivalents; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Seabight
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 93
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH512; Ch512_MC2#1; Ch512-02#1; Challenger; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Seabight; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 94
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH515; Ch515_MC4#3; Ch515-04#3; Challenger; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Abyssal Plain; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 95
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH515; Ch515_MC4#5; Ch515-04#5; Challenger; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Abyssal Plain; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 96
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH515; Ch515_MC5#1; Ch515-05#1; Challenger; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Abyssal Plain; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 97
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH515; Ch515_MC7#1; Ch515-07#1; Challenger; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Seabight; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 98
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH516; Ch516_MC15#2; Ch516-15#2; Challenger; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Seabight; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 99
    Publication Date: 2024-04-18
    Keywords: ADEPD; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; CH516; Ch516_MC15#5; Ch516-15#5; Challenger; Chlorophyll pigment equivalents; Confidence; DEPTH, sediment/rock; MUC; MultiCorer; Porcupine Seabight; Student_s t
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 100
    Publication Date: 2024-04-18
    Keywords: ADEPD; ARK-IX/4; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Chitobiase activity; DEPTH, sediment/rock; Laptev Sea; MUC; MultiCorer; Polarstern; PS2477-1; PS27; PS27/064; Quaternary Environment of the Eurasian North; QUEEN
    Type: Dataset
    Format: text/tab-separated-values, 5 data points
    Location Call Number Expected Availability
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