Opal and barium records of six sediment cores for the last 400 ka ...
Records of biogenic opal and barium were measured in sediment cores at the Antarctic continental margin in the area of the Weddell, Lazarev and Cosmonaut seas. These records provide a qualitative and quantitative tool to estimate changes in palaeoproductivity over the last 400 ka. The stratigraphy o...
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ftdatacite:10.1594/pangaea.728665 2024-04-28T08:01:35+00:00 Opal and barium records of six sediment cores for the last 400 ka ... Bonn, Wolfgang J Gingele, Franz Grobe, Hannes Mackensen, Andreas Fütterer, Dieter K 1998 application/zip https://dx.doi.org/10.1594/pangaea.728665 https://doi.pangaea.de/10.1594/PANGAEA.728665 en eng PANGAEA https://dx.doi.org/10.1016/s0031-0182(97)00144-2 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type ANT-IV/3 ANT-V/4 ANT-VI/3 ANT-VIII/6 ANT-IX/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS article Supplementary Publication Series of Datasets Collection 1998 ftdatacite https://doi.org/10.1594/pangaea.72866510.1016/s0031-0182(97)00144-2 2024-04-02T09:30:57Z Records of biogenic opal and barium were measured in sediment cores at the Antarctic continental margin in the area of the Weddell, Lazarev and Cosmonaut seas. These records provide a qualitative and quantitative tool to estimate changes in palaeoproductivity over the last 400 ka. The stratigraphy of the investigated cores is calibrated to a lithostratigraphy, adjusted to a stable isotope record from the eastern Weddell Sea, which is supported by a Th-dating method. We present evidence that interglacial productivity along the Antarctic continental margin is twice as high compared to subantarctic sites near South Orkney. A glacial/interglacial pattern with high productivity during peak warm stages can be observed back to 400 ka. High interglacial productivity is linked to a reduced sea-ice coverage, which is regulated by the heat flux introduced by North Atlantic Deep Water (NADW) to the Antarctic Ocean. Generally, good correlations between the barium and opal records of the sediment cores indicate that ... : Supplement to: Bonn, Wolfgang J; Gingele, Franz; Grobe, Hannes; Mackensen, Andreas; Fütterer, Dieter K (1998): Palaeoproductivity at the Antarctic continental margin: opal and barium records for the last 400 ka. Palaeogeography, Palaeoclimatology, Palaeoecology, 139(3-4), 195-211 ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Ocean NADW North Atlantic Deep Water North Atlantic Sea ice Weddell Sea DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Gravity corer Kiel type ANT-IV/3 ANT-V/4 ANT-VI/3 ANT-VIII/6 ANT-IX/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS |
spellingShingle |
Gravity corer Kiel type ANT-IV/3 ANT-V/4 ANT-VI/3 ANT-VIII/6 ANT-IX/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS Bonn, Wolfgang J Gingele, Franz Grobe, Hannes Mackensen, Andreas Fütterer, Dieter K Opal and barium records of six sediment cores for the last 400 ka ... |
topic_facet |
Gravity corer Kiel type ANT-IV/3 ANT-V/4 ANT-VI/3 ANT-VIII/6 ANT-IX/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS |
description |
Records of biogenic opal and barium were measured in sediment cores at the Antarctic continental margin in the area of the Weddell, Lazarev and Cosmonaut seas. These records provide a qualitative and quantitative tool to estimate changes in palaeoproductivity over the last 400 ka. The stratigraphy of the investigated cores is calibrated to a lithostratigraphy, adjusted to a stable isotope record from the eastern Weddell Sea, which is supported by a Th-dating method. We present evidence that interglacial productivity along the Antarctic continental margin is twice as high compared to subantarctic sites near South Orkney. A glacial/interglacial pattern with high productivity during peak warm stages can be observed back to 400 ka. High interglacial productivity is linked to a reduced sea-ice coverage, which is regulated by the heat flux introduced by North Atlantic Deep Water (NADW) to the Antarctic Ocean. Generally, good correlations between the barium and opal records of the sediment cores indicate that ... : Supplement to: Bonn, Wolfgang J; Gingele, Franz; Grobe, Hannes; Mackensen, Andreas; Fütterer, Dieter K (1998): Palaeoproductivity at the Antarctic continental margin: opal and barium records for the last 400 ka. Palaeogeography, Palaeoclimatology, Palaeoecology, 139(3-4), 195-211 ... |
format |
Article in Journal/Newspaper |
author |
Bonn, Wolfgang J Gingele, Franz Grobe, Hannes Mackensen, Andreas Fütterer, Dieter K |
author_facet |
Bonn, Wolfgang J Gingele, Franz Grobe, Hannes Mackensen, Andreas Fütterer, Dieter K |
author_sort |
Bonn, Wolfgang J |
title |
Opal and barium records of six sediment cores for the last 400 ka ... |
title_short |
Opal and barium records of six sediment cores for the last 400 ka ... |
title_full |
Opal and barium records of six sediment cores for the last 400 ka ... |
title_fullStr |
Opal and barium records of six sediment cores for the last 400 ka ... |
title_full_unstemmed |
Opal and barium records of six sediment cores for the last 400 ka ... |
title_sort |
opal and barium records of six sediment cores for the last 400 ka ... |
publisher |
PANGAEA |
publishDate |
1998 |
url |
https://dx.doi.org/10.1594/pangaea.728665 https://doi.pangaea.de/10.1594/PANGAEA.728665 |
genre |
Antarc* Antarctic Antarctic Ocean NADW North Atlantic Deep Water North Atlantic Sea ice Weddell Sea |
genre_facet |
Antarc* Antarctic Antarctic Ocean NADW North Atlantic Deep Water North Atlantic Sea ice Weddell Sea |
op_relation |
https://dx.doi.org/10.1016/s0031-0182(97)00144-2 |
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.72866510.1016/s0031-0182(97)00144-2 |
_version_ |
1797573266017091584 |