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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Bibliographic Details
Main Authors: Knies, Jochen, Vogt, Christoph
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.736919
https://doi.pangaea.de/10.1594/PANGAEA.736919
id ftdatacite:10.1594/pangaea.736919
record_format openpolar
spelling 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
institution 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
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