Age determination of three sediment cores from the Eurasian continental margin ...

Sediment cores located along the Eurasian continental margin (Arctic Ocean) have been studied to reconstruct the environmental changes in terms of waxing and waning of the Barents/Kara Sea ice-sheets, Atlantic water inflow, and sea-ice distribution over the last 150 kyr. The stratigraphy of the core...

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Main Authors: Knies, Jochen, Nowaczyk, Norbert R, Müller, Claudia, Vogt, Christoph, Stein, Ruediger
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2000
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.762326
https://doi.pangaea.de/10.1594/PANGAEA.762326
id ftdatacite:10.1594/pangaea.762326
record_format openpolar
spelling ftdatacite:10.1594/pangaea.762326 2024-09-15T17:53:27+00:00 Age determination of three sediment cores from the Eurasian continental margin ... Knies, Jochen Nowaczyk, Norbert R Müller, Claudia Vogt, Christoph Stein, Ruediger 2000 application/zip https://dx.doi.org/10.1594/pangaea.762326 https://doi.pangaea.de/10.1594/PANGAEA.762326 en eng PANGAEA https://dx.doi.org/10.1016/s0025-3227(99)00106-1 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type Kasten corer ARK-VIII/2 ARK-XI/1 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2000 ftdatacite https://doi.org/10.1594/pangaea.76232610.1016/s0025-3227(99)00106-1 2024-07-03T13:10:33Z Sediment cores located along the Eurasian continental margin (Arctic Ocean) have been studied to reconstruct the environmental changes in terms of waxing and waning of the Barents/Kara Sea ice-sheets, Atlantic water inflow, and sea-ice distribution over the last 150 kyr. The stratigraphy of the cores is based on stable oxygen isotopes, AMS 14C, and paleomagnetic data. We studied variations in marine and terrigenous input by a multiproxy approach, involving direct comparison of sedimentological and organo-geochemical data. Extensive episodes of northern Barents Sea ice-sheet growth during marine isotope stages (MIS) 6 and 2 have been supported by, at least, subsurface Atlantic water inflow, moisture-bearing storms, low summer insolation, and minimal calving of ice. Ice advance during MIS 4 was probably restricted to the shallow shelf. Between MIS 4 and MIS 2, large ice-sheet fluctuations correspond to contemporary Laurentide surging events and indicate short-term climatic changes in the Arctic Ocean as has ... : Supplement to: Knies, Jochen; Nowaczyk, Norbert R; Müller, Claudia; Vogt, Christoph; Stein, Ruediger (2000): A multiproxy approach to reconstruct the environmental changes along the Eurasian continental margin over the last 150 000 years. Marine Geology, 163(1-4), 317-344 ... Article in Journal/Newspaper Arctic Ocean Barents Sea Ice Sheet Kara Sea Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
Kasten corer
ARK-VIII/2
ARK-XI/1
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Gravity corer Kiel type
Kasten corer
ARK-VIII/2
ARK-XI/1
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Knies, Jochen
Nowaczyk, Norbert R
Müller, Claudia
Vogt, Christoph
Stein, Ruediger
Age determination of three sediment cores from the Eurasian continental margin ...
topic_facet Gravity corer Kiel type
Kasten corer
ARK-VIII/2
ARK-XI/1
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Sediment cores located along the Eurasian continental margin (Arctic Ocean) have been studied to reconstruct the environmental changes in terms of waxing and waning of the Barents/Kara Sea ice-sheets, Atlantic water inflow, and sea-ice distribution over the last 150 kyr. The stratigraphy of the cores is based on stable oxygen isotopes, AMS 14C, and paleomagnetic data. We studied variations in marine and terrigenous input by a multiproxy approach, involving direct comparison of sedimentological and organo-geochemical data. Extensive episodes of northern Barents Sea ice-sheet growth during marine isotope stages (MIS) 6 and 2 have been supported by, at least, subsurface Atlantic water inflow, moisture-bearing storms, low summer insolation, and minimal calving of ice. Ice advance during MIS 4 was probably restricted to the shallow shelf. Between MIS 4 and MIS 2, large ice-sheet fluctuations correspond to contemporary Laurentide surging events and indicate short-term climatic changes in the Arctic Ocean as has ... : Supplement to: Knies, Jochen; Nowaczyk, Norbert R; Müller, Claudia; Vogt, Christoph; Stein, Ruediger (2000): A multiproxy approach to reconstruct the environmental changes along the Eurasian continental margin over the last 150 000 years. Marine Geology, 163(1-4), 317-344 ...
format Article in Journal/Newspaper
author Knies, Jochen
Nowaczyk, Norbert R
Müller, Claudia
Vogt, Christoph
Stein, Ruediger
author_facet Knies, Jochen
Nowaczyk, Norbert R
Müller, Claudia
Vogt, Christoph
Stein, Ruediger
author_sort Knies, Jochen
title Age determination of three sediment cores from the Eurasian continental margin ...
title_short Age determination of three sediment cores from the Eurasian continental margin ...
title_full Age determination of three sediment cores from the Eurasian continental margin ...
title_fullStr Age determination of three sediment cores from the Eurasian continental margin ...
title_full_unstemmed Age determination of three sediment cores from the Eurasian continental margin ...
title_sort age determination of three sediment cores from the eurasian continental margin ...
publisher PANGAEA
publishDate 2000
url https://dx.doi.org/10.1594/pangaea.762326
https://doi.pangaea.de/10.1594/PANGAEA.762326
genre Arctic Ocean
Barents Sea
Ice Sheet
Kara Sea
Sea ice
genre_facet Arctic Ocean
Barents Sea
Ice Sheet
Kara Sea
Sea ice
op_relation https://dx.doi.org/10.1016/s0025-3227(99)00106-1
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.76232610.1016/s0025-3227(99)00106-1
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