Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition
Sea-ice is believed to be an important control on climatic changes through the Mid-Pleistocene Transition (MPT; 0.6–1.2 Ma). However, the low resolution/short timescale of existing reconstructions prevents a full evaluation of these dynamics. Here, diatom assemblages from the Bering Sea are used to...
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Elsevier
2021
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Online Access: | http://nora.nerc.ac.uk/id/eprint/530149/ https://nora.nerc.ac.uk/id/eprint/530149/1/1-s2.0-S0277379121001256-main.pdf https://doi.org/10.1016/j.quascirev.2021.106918 |
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ftnerc:oai:nora.nerc.ac.uk:530149 2023-05-15T15:43:13+02:00 Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition Worne, Savannah Stroynowski, Zuzia Kender, Sev Swann, George E.A. 2021-05-01 text http://nora.nerc.ac.uk/id/eprint/530149/ https://nora.nerc.ac.uk/id/eprint/530149/1/1-s2.0-S0277379121001256-main.pdf https://doi.org/10.1016/j.quascirev.2021.106918 en eng Elsevier https://nora.nerc.ac.uk/id/eprint/530149/1/1-s2.0-S0277379121001256-main.pdf Worne, Savannah; Stroynowski, Zuzia; Kender, Sev; Swann, George E.A. 2021 Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition. Quaternary Science Reviews, 259, 106918. https://doi.org/10.1016/j.quascirev.2021.106918 <https://doi.org/10.1016/j.quascirev.2021.106918> cc_by_4 CC-BY Publication - Article PeerReviewed 2021 ftnerc https://doi.org/10.1016/j.quascirev.2021.106918 2023-02-04T19:52:01Z Sea-ice is believed to be an important control on climatic changes through the Mid-Pleistocene Transition (MPT; 0.6–1.2 Ma). However, the low resolution/short timescale of existing reconstructions prevents a full evaluation of these dynamics. Here, diatom assemblages from the Bering Sea are used to investigate sea-ice evolution on millennial timescales. We find that sea-ice was primarily controlled by ice-sheet/sea level fluctuations that modulated warm water flow into the Bering Sea. Facilitated by an amplified Walker circulation, sea-ice expansion began at ∼1.05 Ma with a step-increase during the 900 kyr event. Maximal pack ice was simultaneous with glacial maxima, suggesting sea-ice was responding to, rather than modulating ice-sheet dynamics, as proposed by the sea-ice switch hypothesis. Significant pack ice, coupled with Bering Strait closure at 0.9 Ma, indicates that brine rejection played an integral role in the glacial expansion/deglacial collapse of intermediate waters during the MPT, regulating subarctic ocean-atmospheric exchanges of CO2. Article in Journal/Newspaper Bering Sea Bering Strait Ice Sheet Sea ice Subarctic Natural Environment Research Council: NERC Open Research Archive Bering Sea Bering Strait Quaternary Science Reviews 259 106918 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
description |
Sea-ice is believed to be an important control on climatic changes through the Mid-Pleistocene Transition (MPT; 0.6–1.2 Ma). However, the low resolution/short timescale of existing reconstructions prevents a full evaluation of these dynamics. Here, diatom assemblages from the Bering Sea are used to investigate sea-ice evolution on millennial timescales. We find that sea-ice was primarily controlled by ice-sheet/sea level fluctuations that modulated warm water flow into the Bering Sea. Facilitated by an amplified Walker circulation, sea-ice expansion began at ∼1.05 Ma with a step-increase during the 900 kyr event. Maximal pack ice was simultaneous with glacial maxima, suggesting sea-ice was responding to, rather than modulating ice-sheet dynamics, as proposed by the sea-ice switch hypothesis. Significant pack ice, coupled with Bering Strait closure at 0.9 Ma, indicates that brine rejection played an integral role in the glacial expansion/deglacial collapse of intermediate waters during the MPT, regulating subarctic ocean-atmospheric exchanges of CO2. |
format |
Article in Journal/Newspaper |
author |
Worne, Savannah Stroynowski, Zuzia Kender, Sev Swann, George E.A. |
spellingShingle |
Worne, Savannah Stroynowski, Zuzia Kender, Sev Swann, George E.A. Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition |
author_facet |
Worne, Savannah Stroynowski, Zuzia Kender, Sev Swann, George E.A. |
author_sort |
Worne, Savannah |
title |
Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition |
title_short |
Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition |
title_full |
Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition |
title_fullStr |
Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition |
title_full_unstemmed |
Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition |
title_sort |
sea-ice response to climate change in the bering sea during the mid-pleistocene transition |
publisher |
Elsevier |
publishDate |
2021 |
url |
http://nora.nerc.ac.uk/id/eprint/530149/ https://nora.nerc.ac.uk/id/eprint/530149/1/1-s2.0-S0277379121001256-main.pdf https://doi.org/10.1016/j.quascirev.2021.106918 |
geographic |
Bering Sea Bering Strait |
geographic_facet |
Bering Sea Bering Strait |
genre |
Bering Sea Bering Strait Ice Sheet Sea ice Subarctic |
genre_facet |
Bering Sea Bering Strait Ice Sheet Sea ice Subarctic |
op_relation |
https://nora.nerc.ac.uk/id/eprint/530149/1/1-s2.0-S0277379121001256-main.pdf Worne, Savannah; Stroynowski, Zuzia; Kender, Sev; Swann, George E.A. 2021 Sea-ice response to climate change in the Bering Sea during the Mid-Pleistocene Transition. Quaternary Science Reviews, 259, 106918. https://doi.org/10.1016/j.quascirev.2021.106918 <https://doi.org/10.1016/j.quascirev.2021.106918> |
op_rights |
cc_by_4 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1016/j.quascirev.2021.106918 |
container_title |
Quaternary Science Reviews |
container_volume |
259 |
container_start_page |
106918 |
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1766377271720935424 |