Investigations on sediment core Co1010 from Rauer Group, Antarctica ...

The Rauer Group is an archipelago in Prydz Bay, East Antarctica. The ice-free islands and the surrounding shallow marine areas provide valuable archives for the reconstruction of the late Pleistocene and Holocene environmental and climatic history of the region. Two sediment records from two marine...

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Main Authors: Berg, Sonja, Wagner, Bernd, Cremer, Holger, Leng, Melanie J, Melles, Martin
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.745306
https://doi.pangaea.de/10.1594/PANGAEA.745306
id ftdatacite:10.1594/pangaea.745306
record_format openpolar
spelling ftdatacite:10.1594/pangaea.745306 2024-09-15T17:42:35+00:00 Investigations on sediment core Co1010 from Rauer Group, Antarctica ... Berg, Sonja Wagner, Bernd Cremer, Holger Leng, Melanie J Melles, Martin 2010 application/zip https://dx.doi.org/10.1594/pangaea.745306 https://doi.pangaea.de/10.1594/PANGAEA.745306 en eng PANGAEA https://dx.doi.org/10.1016/j.palaeo.2010.08.002 https://dx.doi.org/10.1017/s0954102009001886 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core ANT-XXIII/9 Polarstern Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 article Collection Supplementary Publication Series of Datasets 2010 ftdatacite https://doi.org/10.1594/pangaea.74530610.1016/j.palaeo.2010.08.00210.1017/s0954102009001886 2024-07-03T13:10:33Z The Rauer Group is an archipelago in Prydz Bay, East Antarctica. The ice-free islands and the surrounding shallow marine areas provide valuable archives for the reconstruction of the late Pleistocene and Holocene environmental and climatic history of the region. Two sediment records from two marine inlets of Rauer Group have been studied for their sedimentological, geochemical, and biological characteristics. Radiocarbon ages from one of the inlets indicate ice-free conditions within the last glacial cycle, probably during the second half of Marine Isotope Stage 3. Subsequent ice sheet coverage of Rauer Group during the Last Glacial Maxiumum (LGM) can be inferred from a till layer recovered in one of the basins. The inlets became ice-free prior to 11,200 cal yr BP, when biogenic sedimentation started. Deglacial processes in the catchments, however, influenced the inlets until ~9200 cal. yr BP as evidenced by the input of minerogenic material. Marine productivity under relatively open water conditions ... : Supplement to: Berg, Sonja; Wagner, Bernd; Cremer, Holger; Leng, Melanie J; Melles, Martin (2010): Late Quaternary environmental and climate history of Rauer Group, East Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 297, 201-213 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Prydz Bay Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
ANT-XXIII/9
Polarstern
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
spellingShingle Composite Core
ANT-XXIII/9
Polarstern
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
Berg, Sonja
Wagner, Bernd
Cremer, Holger
Leng, Melanie J
Melles, Martin
Investigations on sediment core Co1010 from Rauer Group, Antarctica ...
topic_facet Composite Core
ANT-XXIII/9
Polarstern
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158
description The Rauer Group is an archipelago in Prydz Bay, East Antarctica. The ice-free islands and the surrounding shallow marine areas provide valuable archives for the reconstruction of the late Pleistocene and Holocene environmental and climatic history of the region. Two sediment records from two marine inlets of Rauer Group have been studied for their sedimentological, geochemical, and biological characteristics. Radiocarbon ages from one of the inlets indicate ice-free conditions within the last glacial cycle, probably during the second half of Marine Isotope Stage 3. Subsequent ice sheet coverage of Rauer Group during the Last Glacial Maxiumum (LGM) can be inferred from a till layer recovered in one of the basins. The inlets became ice-free prior to 11,200 cal yr BP, when biogenic sedimentation started. Deglacial processes in the catchments, however, influenced the inlets until ~9200 cal. yr BP as evidenced by the input of minerogenic material. Marine productivity under relatively open water conditions ... : Supplement to: Berg, Sonja; Wagner, Bernd; Cremer, Holger; Leng, Melanie J; Melles, Martin (2010): Late Quaternary environmental and climate history of Rauer Group, East Antarctica. Palaeogeography, Palaeoclimatology, Palaeoecology, 297, 201-213 ...
format Article in Journal/Newspaper
author Berg, Sonja
Wagner, Bernd
Cremer, Holger
Leng, Melanie J
Melles, Martin
author_facet Berg, Sonja
Wagner, Bernd
Cremer, Holger
Leng, Melanie J
Melles, Martin
author_sort Berg, Sonja
title Investigations on sediment core Co1010 from Rauer Group, Antarctica ...
title_short Investigations on sediment core Co1010 from Rauer Group, Antarctica ...
title_full Investigations on sediment core Co1010 from Rauer Group, Antarctica ...
title_fullStr Investigations on sediment core Co1010 from Rauer Group, Antarctica ...
title_full_unstemmed Investigations on sediment core Co1010 from Rauer Group, Antarctica ...
title_sort investigations on sediment core co1010 from rauer group, antarctica ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.745306
https://doi.pangaea.de/10.1594/PANGAEA.745306
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Prydz Bay
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Prydz Bay
Sea ice
op_relation https://dx.doi.org/10.1016/j.palaeo.2010.08.002
https://dx.doi.org/10.1017/s0954102009001886
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.74530610.1016/j.palaeo.2010.08.00210.1017/s0954102009001886
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