Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition
The Mid-Brunhes Transition (MBT) saw an increase in the amplitude of glacial cycles expressed in ice core and deep ocean records from about 400 ka, but its influence on high-latitude climates is not fully understood. The Arctic Ocean is thought to have warmed and exhibited reduced sea ice, but littl...
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ftcopernicus:oai:publications.copernicus.org:jm77943 2023-05-15T14:59:08+02:00 Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition Kender, Sev Aturamu, Adeyinka Zalasiewicz, Jan Kaminski, Michael A. Williams, Mark 2019-12-03 application/pdf https://doi.org/10.5194/jm-38-177-2019 https://jm.copernicus.org/articles/38/177/2019/ eng eng doi:10.5194/jm-38-177-2019 https://jm.copernicus.org/articles/38/177/2019/ eISSN: 2041-4978 Text 2019 ftcopernicus https://doi.org/10.5194/jm-38-177-2019 2020-07-20T16:22:33Z The Mid-Brunhes Transition (MBT) saw an increase in the amplitude of glacial cycles expressed in ice core and deep ocean records from about 400 ka, but its influence on high-latitude climates is not fully understood. The Arctic Ocean is thought to have warmed and exhibited reduced sea ice, but little is known of sea ice marginal locations such as the Bering Sea. The Bering Sea is the link between the Arctic and Pacific Ocean and is an area of high productivity and CO 2 ventilation; it hosts a pronounced oxygen minimum zone (OMZ) and is thought to be the location of Glacial North Pacific Intermediate Water (GNPIW) formation in the Pleistocene. To understand palaeoceanographic change in the region, we analysed benthic foraminiferal faunas from Bowers Ridge (Site U1342, 800 m of water depth) over the past 600 kyr, as they are uniquely well preserved and sensitive to changes in deep and surface ocean conditions. We identified and imaged 71 taxa and provide a full taxonomy. Foraminiferal preservation is markedly higher during glacials, indicating the presence of less corrosive GNPIW. The most abundant species are Bulimina exilis , Takayanagia delicata , Alabaminella weddellensis , Gyroidina sp. 2, Cassidulina laevigata , Islandiella norcrossi , and Uvigerina bifurcata , consistent with broadly high net primary production throughout the last 600 kyr. Correspondence analysis shows that the most significant Assemblage 1 comprises B. exilis , T. delicata , Bolivina spissa , and Brizalina , which occur sporadically within intervals of laminated, biogenic-rich sediment, mostly during glacials and also some deglacials, and are interpreted as indicating very high productivity. Other assemblages contain the phytodetritivore species A. weddellensis , I. norcrossi , and C. laevigata , indicative of seasonal phytoplankton blooms. Before the MBT, more numerous intervals of the very high-productivity Assemblage 1 and A. weddellensis occur, which we suggest reflect a time of more sea-ice-related seasonal stratification and ice edge blooms. Our inference of a decrease in sea ice meltwater stratification influence in the central Bering Sea after the MBT is consistent with records showing that the Arctic and Pacific Ocean warmed during glacials and suggests that high-latitude productivity and sea ice changes were an important feature of this climate event. Text Arctic Arctic Ocean Bering Sea Foraminifera* ice core Phytoplankton Sea ice Copernicus Publications: E-Journals Arctic Arctic Ocean Bering Sea Bowers ENVELOPE(164.083,164.083,-85.000,-85.000) Pacific Journal of Micropalaeontology 38 2 177 187 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
The Mid-Brunhes Transition (MBT) saw an increase in the amplitude of glacial cycles expressed in ice core and deep ocean records from about 400 ka, but its influence on high-latitude climates is not fully understood. The Arctic Ocean is thought to have warmed and exhibited reduced sea ice, but little is known of sea ice marginal locations such as the Bering Sea. The Bering Sea is the link between the Arctic and Pacific Ocean and is an area of high productivity and CO 2 ventilation; it hosts a pronounced oxygen minimum zone (OMZ) and is thought to be the location of Glacial North Pacific Intermediate Water (GNPIW) formation in the Pleistocene. To understand palaeoceanographic change in the region, we analysed benthic foraminiferal faunas from Bowers Ridge (Site U1342, 800 m of water depth) over the past 600 kyr, as they are uniquely well preserved and sensitive to changes in deep and surface ocean conditions. We identified and imaged 71 taxa and provide a full taxonomy. Foraminiferal preservation is markedly higher during glacials, indicating the presence of less corrosive GNPIW. The most abundant species are Bulimina exilis , Takayanagia delicata , Alabaminella weddellensis , Gyroidina sp. 2, Cassidulina laevigata , Islandiella norcrossi , and Uvigerina bifurcata , consistent with broadly high net primary production throughout the last 600 kyr. Correspondence analysis shows that the most significant Assemblage 1 comprises B. exilis , T. delicata , Bolivina spissa , and Brizalina , which occur sporadically within intervals of laminated, biogenic-rich sediment, mostly during glacials and also some deglacials, and are interpreted as indicating very high productivity. Other assemblages contain the phytodetritivore species A. weddellensis , I. norcrossi , and C. laevigata , indicative of seasonal phytoplankton blooms. Before the MBT, more numerous intervals of the very high-productivity Assemblage 1 and A. weddellensis occur, which we suggest reflect a time of more sea-ice-related seasonal stratification and ice edge blooms. Our inference of a decrease in sea ice meltwater stratification influence in the central Bering Sea after the MBT is consistent with records showing that the Arctic and Pacific Ocean warmed during glacials and suggests that high-latitude productivity and sea ice changes were an important feature of this climate event. |
format |
Text |
author |
Kender, Sev Aturamu, Adeyinka Zalasiewicz, Jan Kaminski, Michael A. Williams, Mark |
spellingShingle |
Kender, Sev Aturamu, Adeyinka Zalasiewicz, Jan Kaminski, Michael A. Williams, Mark Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition |
author_facet |
Kender, Sev Aturamu, Adeyinka Zalasiewicz, Jan Kaminski, Michael A. Williams, Mark |
author_sort |
Kender, Sev |
title |
Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition |
title_short |
Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition |
title_full |
Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition |
title_fullStr |
Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition |
title_full_unstemmed |
Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition |
title_sort |
benthic foraminifera indicate glacial north pacific intermediate water and reduced primary productivity over bowers ridge, bering sea, since the mid-brunhes transition |
publishDate |
2019 |
url |
https://doi.org/10.5194/jm-38-177-2019 https://jm.copernicus.org/articles/38/177/2019/ |
long_lat |
ENVELOPE(164.083,164.083,-85.000,-85.000) |
geographic |
Arctic Arctic Ocean Bering Sea Bowers Pacific |
geographic_facet |
Arctic Arctic Ocean Bering Sea Bowers Pacific |
genre |
Arctic Arctic Ocean Bering Sea Foraminifera* ice core Phytoplankton Sea ice |
genre_facet |
Arctic Arctic Ocean Bering Sea Foraminifera* ice core Phytoplankton Sea ice |
op_source |
eISSN: 2041-4978 |
op_relation |
doi:10.5194/jm-38-177-2019 https://jm.copernicus.org/articles/38/177/2019/ |
op_doi |
https://doi.org/10.5194/jm-38-177-2019 |
container_title |
Journal of Micropalaeontology |
container_volume |
38 |
container_issue |
2 |
container_start_page |
177 |
op_container_end_page |
187 |
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1766331268717346816 |