A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World
Autor(a) principal: | |
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Data de Publicação: | 2022 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | http://hdl.handle.net/10400.1/18825 |
Resumo: | In order to better understand interglacial climate variability within the 41 kyr world, we produced high-resolution climate records for interglacial Marine Isotope Stage (MIS) 47 (1424-1452 ka) at IODP Site U1387 (36 degrees 48 ' N, 7 degrees 43 ' W) on the southern Portuguese margin. Using benthic and planktonic foraminifera stable isotope records, U-37(k') sea-surface temperature (SST), and plankton assemblage data we investigated Mediterranean Outflow Water (MOW) and surface water conditions. The MOW-level records indicate a poorly ventilated and sluggish bottom current during the MIS 48/MIS 47 transition in association with the insolation maximum, whereas a well-ventilated MOW formed a contourite layer during the second insolation maximum. The benthic delta O-18 record shows a fairly abrupt change during the deglaciation of MIS 48, while the surface waters experienced a terminal stadial event that was associated with initial cooling and freshening followed by stepwise warming until interglacial SST was reached at 1450 ka. Interglacial conditions with SST of 24 degrees C or higher persisted until 1427 ka, although warm SST prevailed into MIS 46. The persistent and prolonged warmth is attributed to a northward expansion of the subtropical gyre during MIS 47 as reflected by the dominance of subtropical-tropical planktonic foraminifera species and the presence of warm water coccolithophores taxa. |
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A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr WorldInterglacial climateIODP Site U1387Sea surface temperaturesTerminal stadial evenSubtropical gyreMediterranean Outflow WaterPlanktonic foraminiferaCoccolithophoresStable isotopesIn order to better understand interglacial climate variability within the 41 kyr world, we produced high-resolution climate records for interglacial Marine Isotope Stage (MIS) 47 (1424-1452 ka) at IODP Site U1387 (36 degrees 48 ' N, 7 degrees 43 ' W) on the southern Portuguese margin. Using benthic and planktonic foraminifera stable isotope records, U-37(k') sea-surface temperature (SST), and plankton assemblage data we investigated Mediterranean Outflow Water (MOW) and surface water conditions. The MOW-level records indicate a poorly ventilated and sluggish bottom current during the MIS 48/MIS 47 transition in association with the insolation maximum, whereas a well-ventilated MOW formed a contourite layer during the second insolation maximum. The benthic delta O-18 record shows a fairly abrupt change during the deglaciation of MIS 48, while the surface waters experienced a terminal stadial event that was associated with initial cooling and freshening followed by stepwise warming until interglacial SST was reached at 1450 ka. Interglacial conditions with SST of 24 degrees C or higher persisted until 1427 ka, although warm SST prevailed into MIS 46. The persistent and prolonged warmth is attributed to a northward expansion of the subtropical gyre during MIS 47 as reflected by the dominance of subtropical-tropical planktonic foraminifera species and the presence of warm water coccolithophores taxa.LA/P/0101/2020LA/P/0101/2020POCI-01-0145-FEDER-022157MDPISapientiaVoelker, AntjeRodrigues, TeresaTrotta, SamantaMarino, MariaKuhnert, Henning2023-01-17T10:25:23Z20222022-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.1/18825eng10.3390/atmos130913782073-4433info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2023-07-24T10:31:11Zoai:sapientia.ualg.pt:10400.1/18825Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T20:08:32.839793Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World |
title |
A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World |
spellingShingle |
A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World Voelker, Antje Interglacial climate IODP Site U1387 Sea surface temperatures Terminal stadial even Subtropical gyre Mediterranean Outflow Water Planktonic foraminifera Coccolithophores Stable isotopes |
title_short |
A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World |
title_full |
A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World |
title_fullStr |
A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World |
title_full_unstemmed |
A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World |
title_sort |
A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World |
author |
Voelker, Antje |
author_facet |
Voelker, Antje Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning |
author_role |
author |
author2 |
Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning |
author2_role |
author author author author |
dc.contributor.none.fl_str_mv |
Sapientia |
dc.contributor.author.fl_str_mv |
Voelker, Antje Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning |
dc.subject.por.fl_str_mv |
Interglacial climate IODP Site U1387 Sea surface temperatures Terminal stadial even Subtropical gyre Mediterranean Outflow Water Planktonic foraminifera Coccolithophores Stable isotopes |
topic |
Interglacial climate IODP Site U1387 Sea surface temperatures Terminal stadial even Subtropical gyre Mediterranean Outflow Water Planktonic foraminifera Coccolithophores Stable isotopes |
description |
In order to better understand interglacial climate variability within the 41 kyr world, we produced high-resolution climate records for interglacial Marine Isotope Stage (MIS) 47 (1424-1452 ka) at IODP Site U1387 (36 degrees 48 ' N, 7 degrees 43 ' W) on the southern Portuguese margin. Using benthic and planktonic foraminifera stable isotope records, U-37(k') sea-surface temperature (SST), and plankton assemblage data we investigated Mediterranean Outflow Water (MOW) and surface water conditions. The MOW-level records indicate a poorly ventilated and sluggish bottom current during the MIS 48/MIS 47 transition in association with the insolation maximum, whereas a well-ventilated MOW formed a contourite layer during the second insolation maximum. The benthic delta O-18 record shows a fairly abrupt change during the deglaciation of MIS 48, while the surface waters experienced a terminal stadial event that was associated with initial cooling and freshening followed by stepwise warming until interglacial SST was reached at 1450 ka. Interglacial conditions with SST of 24 degrees C or higher persisted until 1427 ka, although warm SST prevailed into MIS 46. The persistent and prolonged warmth is attributed to a northward expansion of the subtropical gyre during MIS 47 as reflected by the dominance of subtropical-tropical planktonic foraminifera species and the presence of warm water coccolithophores taxa. |
publishDate |
2022 |
dc.date.none.fl_str_mv |
2022 2022-01-01T00:00:00Z 2023-01-17T10:25:23Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10400.1/18825 |
url |
http://hdl.handle.net/10400.1/18825 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.3390/atmos13091378 2073-4433 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
MDPI |
publisher.none.fl_str_mv |
MDPI |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
instname_str |
Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
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1799133331512623104 |