A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World

Detalhes bibliográficos
Autor(a) principal: Voelker, Antje
Data de Publicação: 2022
Outros Autores: Rodrigues, Teresa, Trotta, Samanta, Marino, Maria, Kuhnert, Henning
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.
id RCAP_82844b9b665f36a79c21a7afa0cf3b94
oai_identifier_str oai:sapientia.ualg.pt:10400.1/18825
network_acronym_str RCAP
network_name_str Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
repository_id_str 7160
spelling 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
_version_ 1799133331512623104