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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Sedimentology 52 (2005), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: RADIUS is a newly developed particle-size measurement technique, based on evaluation of digital images of thin sections. Analyses are performed with sub-millimetre sample resolution and are thus designed to work on a single lamina of laminated sediments. The method covers grain sizes from medium silt to coarse sand. The application contains pattern-recognition modules that allow the detection of typical particle distributions of loess, organic detritus, turbidites and tephra layers. Cutting and hiding effects of particles on thin sections are corrected by empirical correction matrices. The calculated analysis results are compared with manually counted and measured samples to calibrate the application settings. The method can be applied to all fine-grained clastic sediments, particularly to laminated lake sediments.
    Type of Medium: Electronic Resource
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  • 2
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    PANGAEA
    In:  Supplement to: Seelos, Klemens; Sirocko, Frank (2006): Abrupt cooling events at the very end of the last interglacial. In: Sirocko, F, Claussen, M, Litt, T & Sanchez-Goñi, M F(eds.): The climate of past interglacials; Developments in Quaternary Science, Elsevier, Amsterdam, 207-230, https://doi.org/10.1016/S1571-0866(07)80039-X
    Publication Date: 2023-05-12
    Description: A comparison of a last interglacial annually laminated and varve counted maar lake record from the Eifel/Germany, with a laminated lake sediment record from Northern Germany shows, that high resolution cores can be correlated across central Europe by dust/loess content, if the resolution of grain size data is on the order of decades/centuries. Phases of widespread dust dispersal are the same as the cold events in the Greenland ice and North Atlantic sea surface temperature patterns. The first occurrence of dust in Northern Germany and in the Eifel is during the Late Eemian Aridity Pulse (LEAP, Sirocko et al. 2005) which is called C26 in ocean records (McManus, same vol.). This cold and arid event occurred exactly at the time of the last glacial inception at 118 kyr. Vegetation change in Northern Germany and the Eifel is out of phase after the LEAP. A taiga/tundra vegetation charcterizes Northern Germany between the LEAP and C24, whereas at the same time a Carpinus dominated temperate forest spread in the Eifel region, comparable to the Carpinus dominated forests in France (Sánchez Goñi et al., 2005). A drastic cooling, associated with widespread aridity, came with the C24 cold event, when the vegetation of central Europe changed to a tundra or shrub tundra.
    Keywords: DRILL; Drilling/drill rig; Ei2; Eigelbach Trockenmaar, Eifel, Germany; ELSA_Ei2; Rederstall, Schleswig-Holstein, Germany; RS1
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-01-14
    Keywords: AGE; DRILL; Drilling/drill rig; Rederstall, Schleswig-Holstein, Germany; RS1; Size fraction 0.063-0.020 mm, coarse silt
    Type: Dataset
    Format: text/tab-separated-values, 9378 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-01-23
    Keywords: AGE; DRILL; Drilling/drill rig; Ei2; Eigelbach Trockenmaar, Eifel, Germany; ELSA_Ei2; Size fraction 0.063-0.020 mm, coarse silt
    Type: Dataset
    Format: text/tab-separated-values, 10000 data points
    Location Call Number Limitation Availability
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  • 5
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    PANGAEA
    In:  Supplement to: Sprenk, Daniela; Weber, Michael E; Kuhn, Gerhard; Wennrich, Volker; Hartmann, Thomas; Seelos, Klemens (2014): Seasonal changes in glacial polynya activity inferred from Weddell Sea varves. Climate of the Past, 10(3), 1239-1251, https://doi.org/10.5194/cp-10-1239-2014
    Publication Date: 2023-06-27
    Description: The Weddell Sea and the associated Filchner-Rønne Ice Shelf constitute key regions for global bottomwater production today. However, little is known about bottom-water production under different climate and icesheet conditions. Therefore, we studied core PS1795, which consists primarily of fine-grained siliciclastic varves that were deposited on contourite ridges in the southeastern Weddell Sea during the Last Glacial Maximum (LGM). We conducted high-resolution X-ray fluorescence (XRF) analysis and grain-size measurements with the RADIUS tool (Seelos and Sirocko, 2005, doi:10.1111/j.1365-3091.2005.00715.x) using thin sections to characterize the two seasonal components of the varves at sub-mm resolution to distinguish the seasonal components of the varves. Bright layers contain coarser grains that can mainly be identified as quartz in the medium-to-coarse silt grain size. They also contain higher amounts of Si, Zr, Ca, and Sr, as well as more ice-rafted debris (IRD). Dark layers, on the other hand, contain finer particles such as mica and clay minerals from the chlorite and illite groups. In addition, Fe, Ti, Rb, and K are elevated. Based on these findings as well as on previous analyses on neighbouring cores, we propose a model of enhanced thermohaline convection in front of a grounded ice sheet that is supported by seasonally variable coastal polynya activity during the LGM. Accordingly, katabatic (i.e. offshore blowing) winds removed sea ice from the ice edge, leading to coastal polynya formation. We suggest that glacial processes were similar to today with stronger katabatic winds and enhanced coastal polynya activity during the winter season. Under these conditions, lighter coarser-grained layers are likely glacial winter deposits, when brine rejection was increased, leading to enhanced bottom-water formation and increased sediment transport. Vice versa, darker finer-grained layers were then deposited during less windier season, mainly during summer, when coastal polynya activity was likely reduced.
    Keywords: ANT-VIII/5; AWI_Paleo; Gravity corer (Kiel type); Lyddan Island; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS16; PS16/425; PS1795-2; SL
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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  • 6
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    PANGAEA
    In:  Supplement to: Sirocko, Frank; Seelos, Klemens; Schaber, Katja; Rein, Bert; Dreher, Frank; Diehl, Markus; Lehne, Rouwen; Jäger, Knut; Krbetschek, Matthias R; Degering, Detlev (2005): A late eemian aridity pulse in central Europe during the last glacial inception. Nature, 436, 833-836, https://doi.org/10.1038/nature03905
    Publication Date: 2023-06-27
    Description: Investigating the processes that led to the end of the last interglacial period is relevant for understanding how our ongoing interglacial will end, which has been a matter of much debate. A recent ice core from Greenland demonstrates climate cooling from 122,000 years ago driven by orbitally controlled insolation, with glacial inception at 118,000 years ago. Here we present an annually resolved, layer-counted record of varve thickness, quartz grain size and pollen assemblages from a maar lake in the Eifel (Germany), which documents a late Eemian aridity pulse lasting 468 years with dust storms, aridity, bushfire and a decline of thermophilous trees at the time of glacial inception. We interpret the decrease in both precipitation and temperature as an indication of a close link of this extreme climate event to a sudden southward shift of the position of the North Atlantic drift, the ocean current that brings warm surface waters to the northern European region. The late Eemian aridity pulse occurred at a 65° N July insolation of 416 W/m**2, close to today's value of 428 W/m**2, and may therefore be relevant for the interpretation of present-day climate variability.
    Keywords: DRILL; Drilling/drill rig; Ei2; Eifel Laminated Sediment Archive; Eigelbach Trockenmaar, Eifel, Germany; ELSA; ELSA_Ei2; ELSA_HL2; HL2; Westlich Hoher List, Trockenmaar, Eifel, Germany
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 7
    Publication Date: 2023-06-27
    Keywords: ANT-VIII/5; AWI_Paleo; Carbon, inorganic, total; Carbon, organic, total; DEPTH, sediment/rock; Element analyser CHN, LECO; Gravity corer (Kiel type); Lyddan Island; Nitrogen, total; Opal, auto analysis (Müller & Schneider, 1993); Opal, biogenic silica; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS16; PS16/425; PS1795-2; SL; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 900 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2023-06-27
    Keywords: ANT-VIII/5; AWI_Paleo; Calcium, area, total counts; DEPTH, sediment/rock; Gravity corer (Kiel type); Iron, area, total counts; Lyddan Island; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; Potassium, area, total counts; PS16; PS16/425; PS1795-2; Silicon, area, total counts; SL; Titanium, area, total counts; X-ray fluorescence ITRAX core scanner
    Type: Dataset
    Format: text/tab-separated-values, 25425 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2023-06-27
    Keywords: AGE; DRILL; Drilling/drill rig; ELSA_HL2; HL2; RADIUS thin section detection; Size fraction 0.063-0.020 mm, coarse silt; Westlich Hoher List, Trockenmaar, Eifel, Germany
    Type: Dataset
    Format: text/tab-separated-values, 8686 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Sirocko, Frank; Dietrich, Stephan; Veres, Daniel; Grootes, Pieter Meiert; Schaber-Mohr, Katja; Seelos, Klemens; Nadeau, Marie-Josée; Kromer, Bernd; Rothacker, Leo; Röhner, Marieke; Krbetschek, Matthias R; Appleby, Peter G; Hambach, Ulrich; Rolf, Christian; Sudo, Masafumi; Grim, Stephanie (2013): Multi-proxy dating of Holocene maar lakes and Pleistocene dry maar sediments in the Eifel, Germany. Quaternary Science Reviews, 62, 56-76, https://doi.org/10.1016/j.quascirev.2012.09.011
    Publication Date: 2023-12-02
    Description: During the last twelve years the ELSA Project (Eifel Laminated Sediment Archive) at Mainz University has drilled a total of about 52 cores from 27 maar lakes and filled-in maar basins in the Eifel/Germany. Dating has been completed for the Holocene cores using 6 different methods (210Pb and 137Cs activities, palynostratigraphy, event markers, varve counting, 14C). In general, the different methods consistently complement one another within error margins. Event correlation was used for relating typical lithological changes with historically known events such as the two major Holocene flood events at 1342 AD and ca 800 BC. Dating of MIS2?MIS3 core sections is based on greyscale tuning, radiocarbon and OSL dating, magnetostratigraphy and tephrochronology. The lithological changes in the sediment cores demonstrate a sequence of events similar to the North Atlantic rapid climate variability of the Last Glacial Cycle. The warmest of the MIS3 interstadials was GI14, when a forest with abundant spruce covered the Eifel area from 55 to 48 ka BP, i.e. during a time when also other climate archives in Europe suggested very warm conditions. The forest of this 'Early Stage 3 warm phase' developed subsequently into a steppe with scattered birch and pine, and finally into a glacial desert at around 25 ka BP. Evidence for Mono Lake and Laschamp geomagnetic excursions is found in two long cores. Several large eruptions during Middle and Late Pleistocene (Ulmener Maar - 11,000 varve years BP, Laacher See - 12,900 varve years BP, Mosenberg volcanoes/Meerfelder Maar 41-45 cal ka BP, Dümpel Maar 116 ka BP, Glees Maar - 151 ka BP) produced distinct ash-layers crucial for inter-core and inter-site correlations. The oldest investigated maar of the Eifel is 40Ar/39Ar dated to the time older than 520 ka BP.
    Keywords: AGE; Eifel Laminated Sediment Archive; ELSA; Probability
    Type: Dataset
    Format: text/tab-separated-values, 625 data points
    Location Call Number Limitation Availability
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