Sediment record of the last 1.8 Ma in the Amundsen Sea

Fuente: PANGAEA
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Autori principali: Hillenbrand, Claus-Dieter, Fütterer, Dieter K, Grobe, Hannes, Frederichs, Thomas
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2002
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author Hillenbrand, Claus-Dieter
Fütterer, Dieter K
Grobe, Hannes
Frederichs, Thomas
author_facet Hillenbrand, Claus-Dieter
Fütterer, Dieter K
Grobe, Hannes
Frederichs, Thomas
collection Datos científicos de ciencias marinas y ambientales
contents Records of glaciomarine deposition recovered from the West Antarctic continental margin in the Amundsen Sea allow the reconstruction of the behaviour of the West Antarctic Ice Sheet (WAIS) in response to the natural climatic changes of the last 1.8 million years. Contents of gravel-sized and lithogenic components represent the input and redeposition of glaciogenic debris, whereas variations in the proportions of the calcareous sediment fraction reflect palaeoproductivity changes. All proxies, which are regarded as sensitive to a WAIS collapse, changed markedly during the global climatic cycles, but do not confirm a complete disintegration of the WAIS during the Pleistocene.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_711660
institution PANGAEA
language en
publishDate 2002
publisher PANGAEA
record_format pangaea
spellingShingle Sediment record of the last 1.8 Ma in the Amundsen Sea
Hillenbrand, Claus-Dieter
Fütterer, Dieter K
Grobe, Hannes
Frederichs, Thomas
Adelaide Island; Amundsen Sea; Antarctic Peninsula; ANT-VI/2; ANT-XI/3; Anvers Island; Argentine Islands; AWI_Paleo; Bellingshausen Sea; Giant box corer; GKG; Gravity corer (Kiel type); Marguerite Bay; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS12; PS12/185; PS12/186; PS12/193; PS12/194; PS12/195; PS12/196; PS12/199; PS12/200; PS1554-1; PS1555-1; PS1557-1; PS1558-1; PS1559-1; PS1560-1; PS1563-1; PS1564-1; PS2522-1; PS2524-1; PS2525-1; PS2526-1; PS2527-1; PS2528-1; PS2529-1; PS2531-1; PS2532-2; PS2533-1; PS2534-2; PS2537-1; PS2538-1; PS2539-2; PS2540-1; PS2541-2; PS2542-1; PS2543-3; PS2544-1; PS2545-1; PS2546-1; PS2547-2; PS2547-3; PS2548-2; PS2550-2; PS2551-1; PS2553-2; PS2556-1; PS29; PS29/010; PS29/012; PS29/016; PS29/018; PS29/021; PS29/022; PS29/024; PS29/033; PS29/039; PS29/040; PS29/042; PS29/045; PS29/046; PS29/047; PS29/048; PS29/049; PS29/050; PS29/051; PS29/054; PS29/057; PS29/062; PS29/063; PS29/064; PS29/066; PS29/067; PS29/070; PS29/075; Silicon Cycling in the World Ocean; SINOPS; SL
Records of glaciomarine deposition recovered from the West Antarctic continental margin in the Amundsen Sea allow the reconstruction of the behaviour of the West Antarctic Ice Sheet (WAIS) in response to the natural climatic changes of the last 1.8 million years. Contents of gravel-sized and lithogenic components represent the input and redeposition of glaciogenic debris, whereas variations in the proportions of the calcareous sediment fraction reflect palaeoproductivity changes. All proxies, which are regarded as sensitive to a WAIS collapse, changed markedly during the global climatic cycles, but do not confirm a complete disintegration of the WAIS during the Pleistocene.
title Sediment record of the last 1.8 Ma in the Amundsen Sea
topic Adelaide Island; Amundsen Sea; Antarctic Peninsula; ANT-VI/2; ANT-XI/3; Anvers Island; Argentine Islands; AWI_Paleo; Bellingshausen Sea; Giant box corer; GKG; Gravity corer (Kiel type); Marguerite Bay; MUC; MultiCorer; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS12; PS12/185; PS12/186; PS12/193; PS12/194; PS12/195; PS12/196; PS12/199; PS12/200; PS1554-1; PS1555-1; PS1557-1; PS1558-1; PS1559-1; PS1560-1; PS1563-1; PS1564-1; PS2522-1; PS2524-1; PS2525-1; PS2526-1; PS2527-1; PS2528-1; PS2529-1; PS2531-1; PS2532-2; PS2533-1; PS2534-2; PS2537-1; PS2538-1; PS2539-2; PS2540-1; PS2541-2; PS2542-1; PS2543-3; PS2544-1; PS2545-1; PS2546-1; PS2547-2; PS2547-3; PS2548-2; PS2550-2; PS2551-1; PS2553-2; PS2556-1; PS29; PS29/010; PS29/012; PS29/016; PS29/018; PS29/021; PS29/022; PS29/024; PS29/033; PS29/039; PS29/040; PS29/042; PS29/045; PS29/046; PS29/047; PS29/048; PS29/049; PS29/050; PS29/051; PS29/054; PS29/057; PS29/062; PS29/063; PS29/064; PS29/066; PS29/067; PS29/070; PS29/075; Silicon Cycling in the World Ocean; SINOPS; SL
url https://doi.org/10.1594/PANGAEA.711660