ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Data  (422,627)
  • Other Sources  (635,327)
Collection
Language
Years
  • 1
    Publication Date: 2024-06-18
    Description: Der Bereich des Meßtischblattes 6311 Lauterecken im Saar-Nahe-Gebiet (SW-Deutschland) wurde anhand einer geologischen, ingenieurgeologischen, hydrogeologischen und morphologischen Untersuchung einer Stabilitätsanalyse der Hänge und Böschungen unterzogen, die durch die Verwertung klimatologischer Daten vervollständigt wurde. Das Ergebnis liegt in einer Stabilitätskarte sowie in einer Analyse der gesammelten Daten vor. Soweit die Untersuchung des Modellgebietes von ca. 130 km21 Größe (etwa 5% der Fläche des Saar-Nahe-Gebietes) eine Antwort zuläßt, sind Hänge und Böschungen im sedimentären Rotliegenden des Saar-Nahe-Gebietes bereits ab 7° Hangneigung potentiell rutschgefährdet. Das rutschgefährdete Areal umfaßt etwa 10% der untersuchten Fläche. Ca. 2,6% wurden von Massenbewegungen betroffen. Kriechen und Gleiten sind die häufigsten Arten der Massenbewegungen. Die beteiligten stratigraphischen Einheiten sind neben den Deckschichten die Quirnbacher, Jeckenbacher und Lautereckener Schichten des Unteren Rotliegenden. Künstliche Böschungs-, An- und Einschnitte in den für das Unterrotliegende charakteristischen Wechsellagerungen von Ton-, Schluff- und Sandsteinen, stellen ein permanentes Stabilitätsproblem dar.
    Description: Abstract: This report deals with the analysis of stability of slopes which occur on the map of Lauterecken, Saar-Nahe-area, SW-Germany. A geological, engineering geological, hydrogeological and morphological study was made, additionally, climatological data were taken into account; the results of it are analyzed and plotted in a stability map. Conclusions: Taking the regarded territory of approximately 130 km2 (about 5% of the area of the Saar-Nahe-area), it can be stated that slopes in the Saar-Nahe-area are potential landslide areas, if the inclination of the slopes is 7° or more. Within an area of 10% landslides are probable to take place. Within 2,6% mass movements happened or are going on. Creep and sliding are the most abundant forms of mass movements. Slope instability occours preferentially in weathered rocks, Quirnbach beds, Jeckenbach beds and Lauterecken beds of the Lower Permian. Steep roadcuts occurring in alternating sandstone and siltstone beds are very likely to cause stability problems.
    Description: research
    Keywords: ddc:550 ; Rutschungen ; Saar-Nahe-Becken ; TK 6311 ; Rotliegend
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2024-06-18
    Description: Trotz der am 2. August 1518 erlassenen Bergordnung kam es in den Folgejahren immer wieder zu Auseinandersetzungen zwischen den Bergleuten und den Bergbeamten. Hintergrund waren neben der wachsenden Korruption auch Betrug, Misswirtschaft und Machtmissbrauch der Bergbeamten, dem durch den rasant wachsenden Bergbau Tür und Tor geöffnet war. Mutmaßlich inspiriert durch die Bauernkriege kam es am 20. Mai 1525 zu einem Aufstand der Bergleuten in Joachimsthal. Nach der raschen Beilegung der Auseinandersetzung wurde zu der weiterhin gültigen Bergordnung vom 2. August 1518 eine Ergänzung mit 35 Artikeln erlassen.
    Description: source
    Keywords: Graf Stefan Schlick zu Passaun ; Alexander Burggraf von Leisnig ; Rudolf II. von Bünau ; Apel IV. Vitzthum ; Urban Osan ; Anton Römhelt ; Hans Hausmann ; Joachimsthal/Jáchymov ; Freiberg ; Annaberg ; Falkenau/Sokolow
    Language: German
    Type: doc-type:book , updatedVersion
    Format: 14
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    facet.materialart.
    Unknown
    Kraatz, Berlin
    In:  SUB Göttingen | KART B 140:3162, KART H 140:Kreuz
    Publication Date: 2024-06-18
    Description: Geologische Karte 1: 25 000 mit Erläuterungen. Digitalisat des FID GEO (Fachinformationsdienst Geowissenschaften), erstellt durch das GDZ (Göttinger Digitalisierungszentrum), Karte aus dem Bestand der SUB Göttingen. Koordinaten Vorlage: Nullmeridian Ferro E 033 40 - 033 50 / N 052 54 - 052 48.
    Description: map
    Description: DFG, SUB Göttingen
    Keywords: ddc:554.3 ; ddc:912 ; Geologische Karte
    Language: German
    Type: doc-type:carthographicMaterial
    Format: 78
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2024-06-18
    Description: Die biostratigraphische Aussagekraft organischwandiger Dinoflagella- tenzysten in Rupel-Sedimenten (Unter-Oligozän) des Mainzer Beckens wird anhand von Material aus fünf Kernbohrungen aus verschiedenen Ablagerungsräumen untersucht. Die Abfolge vom oberen Foraminiferenmergel bis in den unteren Schleichsand lässt sich durch das Aussetzen von Wetzeliella gochtii, Rhombodinium draco, Phtanoperidinium amomum, P. comatum, W. symmetrica und Enneadocysta pectiniformis in vier Abschnitte gliedern. Ein Vergleich mit Dinoflagellatenzysten-Zonierungen für den nordwesteuropäischen Raum ergibt die größten Übereinstimmungen mit der Zonierung von Köthe (1990). Dies weist auf eine enge paläozeanographische Verbindung zwischen dem Mainzer Becken und dem nordwestdeutschen Tertiärbecken zur Zeit des Rupels hin.
    Description: Abstract: The biostratigraphic significance of organic-walled dinoflagellate cysts from Rupelian (Lower Oligocene) sediments of the Mainz Basin (Southwest Germany) is investigated. The study material is derived from five boreholes drilled in different depo- sitional environments. The investigated succession can be subdivided into four intervals based on the last appearance data of Wetzeliella gochtii, Rhombodinium draco, Phtanope- ridinium amomum, P. comatum, W. symmetrica, and Enneadocysta pectiniformis. A comparison of dinoflagellate cyst ranges in the Mainz Basin with zonations from the Northwest European Tertiary Basin yields highest agreement with the zonation of Köthe (1990) which has been established for northern Germany. This indicates a close palae- oceanographic connection between the Mainz Basin and the Northwest European Tertiary Basin during Rupelian times.
    Description: research
    Keywords: ddc:560.47 ; Mainzer Becken ; Biostratigraphie ; Dinoflagellaten ; Oligozän
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2024-06-18
    Description: In verschiedenen Hanglagen der Ortsgemeinde Essenheim in Rheinhessen (Rheinland-Pfalz) ist der Untergrund rutschgefährdet oder es sind fossile Rutschungen vorhanden. In einer dieser Hanglagen wurde die Erweiterung des Baugebietes „Domherrngärten" geplant. In der Folge dessen war zu klären, unter welchen Randbedingungen die Bebauung realisiert werden kann. Hierzu wurden in mehreren Kampagnen der geologische Untergrund mit Kernbohrungen untersucht und Inklinometermessstellen zur Beobachtung von Hangbewegungen eingerichtet. Die Untersuchungsergebnisse wurden im Rahmen einer Bachelorarbeit zur Durchführung von Standsicherheitsberechnungen genutzt. Auf der Basis aller Untersuchungsergebnisse werden Vorsorgemaßnahmen für die Bebauung in einem rutschgefährdetem Hang aufgezeigt.
    Description: Abstract: Various slopes in the village Essenheim in Rhinehessen/ Rhineland-Pala- tinate are prone to landslides. The planed extension of the building area „Domherrngärten II" is part of such an area. In succession it had to be discussed under which circumstances construction is possible. To analyze the geological features core drillings with rock sampling were executed as well as inclinometers (measurements to detect motion of the slope). The taken data was used in a Bachelor thesis to evaluate the slope stability. On the base of all results references for building on instable slopes are given.
    Description: research
    Keywords: ddc:624.151 ; Mainzer Becken ; Rutschungen ; Ingenieurgeologie ; TK 6014
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: McIntyre, Katherine; Ravelo, Ana Christina; Delaney, Margaret Lois (1999): North Atlantic intermediate waters in the Late Pliocene to Early Pleistocene. Paleoceanography, 14(3), 324-335, https://doi.org/10.1029/1998PA900005
    Publication Date: 2024-06-18
    Description: We generated benthic isotope records from Ocean Drilling Program (ODP) site 981 on the Feni drift (2173 m water depth) and from ODP site 983 on the Gardar drift (1983 m water depth) to examine the interaction between North Atlantic Deep Water (NADW) and Glacial North Atlantic Intermediate Water (GNAIW) formation from 2.0 to 1.4 Ma. We find NADW at both sites during interglacial periods, and a mix of NADW and Southern Ocean water at the Feini drift during most glacial periods. Prior to 1.7 Ma we find no evidence ofr GNAIW at the Gardar drift site. Instead, glacial Gardar drift delta13C values are as low or lower than values for all other sites in the North Atlantic and reflect continued glacial overflow from the Nordic seas. After 1.7 Ma Gardar drift delta13C values increase and suggest that there was GNAIW at the Gardar drift site during some glacial intervals. Overall, we find that NADW and GNAIW production changed around 1.7 Ma in concert with changes in sea surface temperature and salinity and in the Earth's obliquity cycle.
    Keywords: 162-981; 162-983; COMPCORE; Composite Core; Joides Resolution; Leg162; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: McIntyre, Katherine; Ravelo, Ana Christina; Delaney, Margaret Lois; Anderson, Linda Davis; Johannessen, Truls (1997): Ground truthing the Cd/Ca-carbon isotope relationship in foraminifera of the Greenland-Iceland-Norwegian Seas. Marine Geology, 140(1-2), 61-73, https://doi.org/10.1016/S0025-3227(97)00004-2
    Publication Date: 2024-06-18
    Description: In order to examine whether the paleoceanographic nutrient proxies, d13C and cadmium/calcium in foraminiferal calcite, are well coupled to nutrients in the region of North Atlantic Deep Water formation, we present da ta from two transects of the Greenland-Iceland-Norwegian Seas. Along Transect A (74.3°N, 18.3°E to 75.0°N, 12.5°W, 15 stations), we measured phosphate and Cd concentrations of modern surface sea water. Along Transect B (64.5°N, 0.7°W to 70.4°N, 18.2°W, 14 stations) we measured Cd/Ca ratios and d13C of the planktonic foraminifera Neogloboquadrina pachyderma sinistral in core top sediments. Our results indicate that Cd and phosphate both vary with surface water mass and are well correlated along Transect A. Our planktonic foraminiferal d13C data indicate similar nutrient variation with water mass along Transect B. Our Cd/Ca data hint at the same type of nutrient variability, but interpretations are hampered by low values close to the detection limit of this technique and therefore relatively large error bars. We also measured Cd and phosphate concentrations in water depth profiles at three sites along Transect A and the d13C of the benthic foraminifera Cibicidoides wuellerstorfi along Transect B. Modern sea water depth profiles along Transect A have nutrient depletions at the surface and then constant values at depths greater than 100 meters. The d13C of planktonic and benthic foraminifera from Transect B plotted versus depth also reflect surface nutrient depletion and deep nutrient enrichment as seen at Transect A, with a small difference between intermediate and deep waters. Overall we see no evidence for decoupling of Cd/Ca ratio and d13C in foraminiferal calcite from water column nutrient concentrations along these transects in a region of North Atlantic Deep Water formation.
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Barth, Aaron M; Clark, Peter U; Bill, Nicholas S; He, Feng; Pisias, Nicklas G (2018): Climate evolution across the Mid-Brunhes Transition. Climate of the Past, 14(12), 2071-2087, https://doi.org/10.5194/cp-14-2071-2018
    Publication Date: 2024-06-18
    Description: The Mid-Brunhes Transition (MBT) began ∼430ka with an increase in the amplitude of the 100-kyr climate cycles of the past 800,000 years. The MBT has been identified in ice-core records, which indicate interglaciations became warmer with higher atmospheric CO2 levels after the MBT, and benthic oxygen isotope (δ18O) records, which suggest that post-MBT interglaciations had higher sea levels than pre-MBT interglaciations. It remains unclear, however, whether the MBT was a globally synchronous phenomenon that included other components of the climate system. Here we further characterize changes in the climate system across the MBT through statistical analyses of ice-core and δ18O records as well as sea-surface temperature, benthic carbon isotope, and dust accumulation records. Our results demonstrate that the MBT was a global event with a significant increase in climate variance in most components of the climate system assessed here. However, our results indicate that the onset of high-amplitude variability in temperature, atmospheric CO2, and sea level at ∼430ka was preceded by changes in the carbon cycle, ice sheets, and monsoon strength during MIS 14 and 13.
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lisiecki, Lorraine E; Raymo, Maureen E (2005): A Pliocene-Pleistocene stack of 57 globally distributed benthic d18O records. Paleoceanography, 20, PA1003, https://doi.org/10.1029/2004PA001071
    Publication Date: 2024-06-18
    Description: We present a 5.3-Myr stack (the ''LR04'' stack) of benthic d18O records from 57 globally distributed sites aligned by an automated graphic correlation algorithm. This is the first benthic delta18O stack composed of more than three records to extend beyond 850 ka, and we use its improved signal quality to identify 24 new marine isotope stages in the early Pliocene. We also present a new LR04 age model for the Pliocene-Pleistocene derived from tuning the delta18O stack to a simple ice model based on 21 June insolation at 65 N. Stacked sedimentation rates provide additional age model constraints to prevent overtuning. Despite a conservative tuning strategy, the LR04 benthic stack exhibits significant coherency with insolation in the obliquity band throughout the entire 5.3 Myr and in the precession band for more than half of the record. The LR04 stack contains significantly more variance in benthic delta18O than previously published stacks of the late Pleistocene as the result of higher resolution records, a better alignment technique, and a greater percentage of records from the Atlantic. Finally, the relative phases of the stack's 41- and 23-kyr components suggest that the precession component of delta18O from 2.7-1.6 Ma is primarily a deep-water temperature signal and that the phase of d18O precession response changed suddenly at 1.6 Ma.
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2024-06-18
    Description: The presence-absence data for macrobenthic fauna that has been collected in Mingulay Reef Complex (Scotland, UK) across 79 stations over the years 2003, 2005, 2009, 2010 and 2011. The collection of the benthic samples has been carried out using a Van-Veen grab, mainly from hard habitats (e.g. live and dead coral framework). About 60% of the macrofaunal specimens have been identified at species level using high quality taxonomic keys and advice from taxonomy experts. Most common taxonomic groups analysed here are molluscs, polychaetes, arthropods, bryozoans, anthozoans, tunicates and brachiopods. The collection of the specimens is now deposited at the National Museums of Scotland (see the attached excel file for details). The enviromental data contains information about coordinates and environmental settings at stations where macrobenthic samples mentioned above, were collected. The environmental settings that are included in the file refer to the years 2003, 2005, 2009, 2010, 2011. For more information on the environmental variables have a look in Henry et al. 2010 (doi:10.1007/s00338-009-0577-6) and Henry et al. 2013 (doi:10.5194/bg-10-2737-2013). The environmental variables included in the excel file are: type of macrohabitat (i.e. muddy sand, rubble, rock, live coral, dead framework, live & dead framework), depth (m), slope, ruggedness, broad-scale bathymetric position index, fine-scale bathymetric position index, average current speed (m/s), maximum current speed (m/s), northness, eastness, winter North Atlantic Oscillation Index (same year), winter North Atlantic Oscillation Index (previous year), annual average bottom temperature (same year), annual average bottom salinity (same year). Extraction of bathymetric (depth) and topographic data [slope, aspect, northness, eastness, ruggedness, standardised broad-scale bathymetric position index (BPI; with an inner radius of 1 cell and an outer radius of 5 cells), fine-scale BPI (with an inner radius of 1 cell and an outer radius of 3 cells)] was based on multibeam echosounder data, using the Spatial Analyst and Benthic Terrain Modeler toolboxes in ArcGIS v.10.6.1 Average and maximum current speed values (m/s) were extracted by the ArcGIS v. 10.6.1 Spatial Analyst toolbox using data generated by a high-resolution 3D ocean model created for the MRC by Moreno-Navas et al. (2014). Data for the winter NAOI (DJFM) (Hurrell et al., 2003) were downloaded from the National Center for Atmospheric Research/University Corporation for Atmospheric Research website (climatedataguide.ucar.edu; data accessed on 28/02/2019).
    Keywords: ATLAS; A Trans-Atlantic assessment and deep-water ecosystem-based spatial management plan for Europe; Climate change; continental shelf; coral reefs; Deep sea; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; Macrofauna; vulnerable marine ecosystems
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...