A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World
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. Usin...
Published in: | Atmosphere |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
MDPI
2022
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Subjects: | |
Online Access: | http://hdl.handle.net/10400.1/18825 https://doi.org/10.3390/atmos13091378 |
_version_ | 1821685942439641088 |
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author | Voelker, Antje Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning |
author_facet | Voelker, Antje Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning |
author_sort | Voelker, Antje |
collection | Universidade do Algarve: Sapienta |
container_issue | 9 |
container_start_page | 1378 |
container_title | Atmosphere |
container_volume | 13 |
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. info:eu-repo/semantics/publishedVersion |
format | Article in Journal/Newspaper |
genre | Planktonic foraminifera |
genre_facet | Planktonic foraminifera |
id | ftunivalgarve:oai:sapientia.ualg.pt:10400.1/18825 |
institution | Open Polar |
language | English |
op_collection_id | ftunivalgarve |
op_doi | https://doi.org/10.3390/atmos13091378 |
op_relation | info:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDB%2F04326%2F2020/PT info:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDP%2F04326%2F2020/PT LA/P/0101/2020 info:eu-repo/grantAgreement/FCT/9471 - RIDTI/PTDC%2FCTA-GEO%2F29897%2F2017/PT info:eu-repo/grantAgreement/FCT/3599-PPCDT/PTDC%2FMAR-PRO%2F3761%2F2012/PT POCI-01-0145-FEDER-022157 http://hdl.handle.net/10400.1/18825 doi:10.3390/atmos13091378 2073-4433 |
op_rights | openAccess http://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm | CC-BY |
publishDate | 2022 |
publisher | MDPI |
record_format | openpolar |
spelling | ftunivalgarve:oai:sapientia.ualg.pt:10400.1/18825 2025-01-17T00:20:49+00:00 A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World Voelker, Antje Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning 2022 http://hdl.handle.net/10400.1/18825 https://doi.org/10.3390/atmos13091378 eng eng MDPI info:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDB%2F04326%2F2020/PT info:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDP%2F04326%2F2020/PT LA/P/0101/2020 info:eu-repo/grantAgreement/FCT/9471 - RIDTI/PTDC%2FCTA-GEO%2F29897%2F2017/PT info:eu-repo/grantAgreement/FCT/3599-PPCDT/PTDC%2FMAR-PRO%2F3761%2F2012/PT POCI-01-0145-FEDER-022157 http://hdl.handle.net/10400.1/18825 doi:10.3390/atmos13091378 2073-4433 openAccess http://creativecommons.org/licenses/by/4.0/ CC-BY Interglacial climate IODP Site U1387 Sea surface temperatures Terminal stadial even Subtropical gyre Mediterranean Outflow Water Planktonic foraminifera Coccolithophores Stable isotopes article 2022 ftunivalgarve https://doi.org/10.3390/atmos13091378 2023-01-25T01:02:53Z 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. info:eu-repo/semantics/publishedVersion Article in Journal/Newspaper Planktonic foraminifera Universidade do Algarve: Sapienta Atmosphere 13 9 1378 |
spellingShingle | Interglacial climate IODP Site U1387 Sea surface temperatures Terminal stadial even Subtropical gyre Mediterranean Outflow Water Planktonic foraminifera Coccolithophores Stable isotopes Voelker, Antje Rodrigues, Teresa Trotta, Samanta Marino, Maria Kuhnert, Henning 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 |
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_short | A southern Portuguese Margin Perspective of Marine Isotope Stage 47—An interglacial in the 41 kyr World |
title_sort | southern portuguese margin perspective of marine isotope stage 47—an interglacial in the 41 kyr world |
topic | Interglacial climate IODP Site U1387 Sea surface temperatures Terminal stadial even Subtropical gyre Mediterranean Outflow Water Planktonic foraminifera Coccolithophores Stable isotopes |
topic_facet | Interglacial climate IODP Site U1387 Sea surface temperatures Terminal stadial even Subtropical gyre Mediterranean Outflow Water Planktonic foraminifera Coccolithophores Stable isotopes |
url | http://hdl.handle.net/10400.1/18825 https://doi.org/10.3390/atmos13091378 |