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dc.contributor.authorStewart, Joseph A.
dc.contributor.authorLi, Tao
dc.contributor.authorSpooner, Peter T.
dc.contributor.authorBurke, Andrea
dc.contributor.authorChen, Tianyu
dc.contributor.authorRoberts, Jenny
dc.contributor.authorRae, James W. B.
dc.contributor.authorPeck, Victoria
dc.contributor.authorKender, Sev
dc.contributor.authorLiu, Qian
dc.contributor.authorRobinson, Laura F.
dc.date.accessioned2021-10-21T09:30:07Z
dc.date.available2021-10-21T09:30:07Z
dc.date.issued2021-10-19
dc.identifier.citationStewart , J A , Li , T , Spooner , P T , Burke , A , Chen , T , Roberts , J , Rae , J W B , Peck , V , Kender , S , Liu , Q & Robinson , L F 2021 , ' Productivity and dissolved oxygen controls on the Southern Ocean deep‐sea benthos during the Antarctic Cold Reversal ' , Paleoceanography and Paleoclimatology , vol. 36 , no. 10 , e2021PA004288 . https://doi.org/10.1029/2021pa004288en
dc.identifier.issn2572-4517
dc.identifier.otherPURE: 276340463
dc.identifier.otherPURE UUID: efd1f50e-9e8c-47a3-bbfc-2eea5b794cc1
dc.identifier.otherJisc: 171b6985a2284670b667a1ebddfddb5e
dc.identifier.otherORCID: /0000-0002-3754-1498/work/101958899
dc.identifier.otherORCID: /0000-0003-3904-2526/work/101958902
dc.identifier.otherScopus: 85118216649
dc.identifier.otherWOS: 000711966000008
dc.identifier.urihttp://hdl.handle.net/10023/24176
dc.descriptionFunding was provided by an Antarctic Bursary awarded to J.A.S., ERC and NERC grants awarded to L.F.R. (278705, NE/S001743/1, NE/R005117/1) and L.F.R. and J.W.B.R. (NE/N003861/1).en
dc.description.abstractThe Antarctic Cold Reversal (ACR; 14.7 to 13 thousand years ago; ka) phase of the last deglaciation saw a pause in the rise of atmospheric CO2 and Antarctic temperature, that contrasted with warming in the North. A re-expansion of sea ice and a northward shift in the position of the westerly winds in the Southern Ocean are well-documented, but the response of deep-sea biota and the primary drivers of habitat viability remain unclear. Here we present a new perspective on ecological changes in the deglacial Southern Ocean, including multi-faunal benthic assemblage (foraminifera and cold-water corals) and coral geochemical data (Ba/Ca and δ11B) from the Drake Passage. Our records show that, during the ACR, peak abundances of thick-walled benthic foraminifera Uvigerina bifurcata and corals are observed at shallow depths in the sub-Antarctic (∼300 m), while coral populations at greater depths and further south diminished. Our ecological and geochemical data indicate that habitat shifts were dictated by (i) a northward migration of food supply (primary production) into the Subantarctic Zone and (ii) poorly oxygenated seawater at depth during this Antarctic cooling interval.
dc.format.extent17
dc.language.isoeng
dc.relation.ispartofPaleoceanography and Paleoclimatologyen
dc.rightsCopyright © 2021. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.en
dc.subjectCoralen
dc.subjectForaminiferaen
dc.subjectDrake Passageen
dc.subjectDeglacialen
dc.subjectGC Oceanographyen
dc.subjectDASen
dc.subject.lccGCen
dc.titleProductivity and dissolved oxygen controls on the Southern Ocean deep‐sea benthos during the Antarctic Cold Reversalen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.School of Earth & Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.St Andrews Isotope Geochemistryen
dc.contributor.institutionUniversity of St Andrews.Centre for Energy Ethicsen
dc.identifier.doihttps://doi.org/10.1029/2021pa004288
dc.description.statusPeer revieweden


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