Planktonic isotope record and clay mineralogy of sediment core PS2138-1 ...
Improved multiparameter records from the northern Barents Sea margin show two prominent freshwater pulses into the Arctic Ocean during MIS 5 that significantly disturbed the regional oceanic regime and probably affected global climate. Both pulses are associated with major iceberg-rafted debris (IRD...
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Online Access: | https://dx.doi.org/10.1594/pangaea.736919 https://doi.pangaea.de/10.1594/PANGAEA.736919 |
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ftdatacite:10.1594/pangaea.736919 2024-09-15T17:53:12+00:00 Planktonic isotope record and clay mineralogy of sediment core PS2138-1 ... Knies, Jochen Vogt, Christoph 2003 application/zip https://dx.doi.org/10.1594/pangaea.736919 https://doi.pangaea.de/10.1594/PANGAEA.736919 en eng PANGAEA https://dx.doi.org/10.1016/j.yqres.2003.07.008 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type ARK-VIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 2003 ftdatacite https://doi.org/10.1594/pangaea.73691910.1016/j.yqres.2003.07.008 2024-08-01T08:58:27Z Improved multiparameter records from the northern Barents Sea margin show two prominent freshwater pulses into the Arctic Ocean during MIS 5 that significantly disturbed the regional oceanic regime and probably affected global climate. Both pulses are associated with major iceberg-rafted debris (IRD) events, revealing intensive iceberg/sea ice melting. The older meltwater pulse occurred near the MIS 5/6 boundary (~131,000 yr ago); its ~2000 year duration and high IRD input accompanied by high illite content suggest a collapse of large-scale Saalian Glaciation in the Arctic Ocean. Movement of this meltwater with the Transpolar Drift current into the Fram Strait probably promoted freshening of Nordic Seas surface water, which may have increased sea-ice formation and significantly reduced deep-water formation. A second pulse of freshwater occurred within MIS 5a (~77,000 yr ago); its high smectite content and relatively short duration is possibly consistent with sudden discharge of Early Weichselian ice-dammed ... : Supplement to: Knies, Jochen; Vogt, Christoph (2003): Freshwater pulses in the eastern Arctic Ocean during Saalian and Early Weichselian ice-sheet collapse. Quaternary Research, 60(3), 243-251 ... Article in Journal/Newspaper Arctic Ocean Barents Sea Fram Strait Ice Sheet Iceberg* Nordic Seas Sea ice DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Gravity corer Kiel type ARK-VIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
spellingShingle |
Gravity corer Kiel type ARK-VIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN Knies, Jochen Vogt, Christoph Planktonic isotope record and clay mineralogy of sediment core PS2138-1 ... |
topic_facet |
Gravity corer Kiel type ARK-VIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
description |
Improved multiparameter records from the northern Barents Sea margin show two prominent freshwater pulses into the Arctic Ocean during MIS 5 that significantly disturbed the regional oceanic regime and probably affected global climate. Both pulses are associated with major iceberg-rafted debris (IRD) events, revealing intensive iceberg/sea ice melting. The older meltwater pulse occurred near the MIS 5/6 boundary (~131,000 yr ago); its ~2000 year duration and high IRD input accompanied by high illite content suggest a collapse of large-scale Saalian Glaciation in the Arctic Ocean. Movement of this meltwater with the Transpolar Drift current into the Fram Strait probably promoted freshening of Nordic Seas surface water, which may have increased sea-ice formation and significantly reduced deep-water formation. A second pulse of freshwater occurred within MIS 5a (~77,000 yr ago); its high smectite content and relatively short duration is possibly consistent with sudden discharge of Early Weichselian ice-dammed ... : Supplement to: Knies, Jochen; Vogt, Christoph (2003): Freshwater pulses in the eastern Arctic Ocean during Saalian and Early Weichselian ice-sheet collapse. Quaternary Research, 60(3), 243-251 ... |
format |
Article in Journal/Newspaper |
author |
Knies, Jochen Vogt, Christoph |
author_facet |
Knies, Jochen Vogt, Christoph |
author_sort |
Knies, Jochen |
title |
Planktonic isotope record and clay mineralogy of sediment core PS2138-1 ... |
title_short |
Planktonic isotope record and clay mineralogy of sediment core PS2138-1 ... |
title_full |
Planktonic isotope record and clay mineralogy of sediment core PS2138-1 ... |
title_fullStr |
Planktonic isotope record and clay mineralogy of sediment core PS2138-1 ... |
title_full_unstemmed |
Planktonic isotope record and clay mineralogy of sediment core PS2138-1 ... |
title_sort |
planktonic isotope record and clay mineralogy of sediment core ps2138-1 ... |
publisher |
PANGAEA |
publishDate |
2003 |
url |
https://dx.doi.org/10.1594/pangaea.736919 https://doi.pangaea.de/10.1594/PANGAEA.736919 |
genre |
Arctic Ocean Barents Sea Fram Strait Ice Sheet Iceberg* Nordic Seas Sea ice |
genre_facet |
Arctic Ocean Barents Sea Fram Strait Ice Sheet Iceberg* Nordic Seas Sea ice |
op_relation |
https://dx.doi.org/10.1016/j.yqres.2003.07.008 |
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.73691910.1016/j.yqres.2003.07.008 |
_version_ |
1810295202707931136 |