Age model and stable isotope record of eastern equatorial Pacific sediment cores ...

Six deep sea cores from the eastern equatorial Pacific (EEP) were analyzed for planktonic foraminifera and stable isotopes in order to reconstruct sea surface temperatures (SST) for the last 40 ka. South of the Equatorial Front the abundance of Globorotalia inflata increased, and SST decreased by &g...

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Main Authors: Martinez, Ignacio, Keigwin, Lloyd D, Barrows, Timothy T, Yokoyama, Yusuke, Southon, John
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.841739
https://doi.pangaea.de/10.1594/PANGAEA.841739
id ftdatacite:10.1594/pangaea.841739
record_format openpolar
spelling ftdatacite:10.1594/pangaea.841739 2024-09-15T18:31:03+00:00 Age model and stable isotope record of eastern equatorial Pacific sediment cores ... Martinez, Ignacio Keigwin, Lloyd D Barrows, Timothy T Yokoyama, Yusuke Southon, John 2003 application/zip https://dx.doi.org/10.1594/pangaea.841739 https://doi.pangaea.de/10.1594/PANGAEA.841739 en eng PANGAEA https://dx.doi.org/10.1029/2002pa000877 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Deep Sea Drilling Project DSDP Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2003 ftdatacite https://doi.org/10.1594/pangaea.84173910.1029/2002pa000877 2024-08-01T10:54:44Z Six deep sea cores from the eastern equatorial Pacific (EEP) were analyzed for planktonic foraminifera and stable isotopes in order to reconstruct sea surface temperatures (SST) for the last 40 ka. South of the Equatorial Front the abundance of Globorotalia inflata increased, and SST decreased by >5°C (core ODP846B), creating a stronger SST meridional gradient and advection of the Peru Current than present for the ~16-35 ka interval. A sharper SST meridional gradient forced stronger Choco jet events and a moisture increase in western Colombia, which supplied, through the San Juan River and the south-flowing equatorial and the Peru-Chile countercurrents, abundant hemipelagic quartz over the northern Peru basin (core TR163-31B). The Choco jet, and its associated mesoscale convective cells, provoked an increase in snow precipitation over the Central Cordillera of Colombia and the advance of the Murillo glacier. In synchrony with the intensified Choco jet events, the "dry island" effect over the Eastern ... : Supplement to: Martinez, Ignacio; Keigwin, Lloyd D; Barrows, Timothy T; Yokoyama, Yusuke; Southon, John (2003): La Niña-like conditions in the eastern equatorial Pacific and a stronger Choco jet in the northern Andes during the last glaciation. Paleoceanography, 18(2), 1033 ... Article in Journal/Newspaper Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
spellingShingle Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
Martinez, Ignacio
Keigwin, Lloyd D
Barrows, Timothy T
Yokoyama, Yusuke
Southon, John
Age model and stable isotope record of eastern equatorial Pacific sediment cores ...
topic_facet Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
description Six deep sea cores from the eastern equatorial Pacific (EEP) were analyzed for planktonic foraminifera and stable isotopes in order to reconstruct sea surface temperatures (SST) for the last 40 ka. South of the Equatorial Front the abundance of Globorotalia inflata increased, and SST decreased by >5°C (core ODP846B), creating a stronger SST meridional gradient and advection of the Peru Current than present for the ~16-35 ka interval. A sharper SST meridional gradient forced stronger Choco jet events and a moisture increase in western Colombia, which supplied, through the San Juan River and the south-flowing equatorial and the Peru-Chile countercurrents, abundant hemipelagic quartz over the northern Peru basin (core TR163-31B). The Choco jet, and its associated mesoscale convective cells, provoked an increase in snow precipitation over the Central Cordillera of Colombia and the advance of the Murillo glacier. In synchrony with the intensified Choco jet events, the "dry island" effect over the Eastern ... : Supplement to: Martinez, Ignacio; Keigwin, Lloyd D; Barrows, Timothy T; Yokoyama, Yusuke; Southon, John (2003): La Niña-like conditions in the eastern equatorial Pacific and a stronger Choco jet in the northern Andes during the last glaciation. Paleoceanography, 18(2), 1033 ...
format Article in Journal/Newspaper
author Martinez, Ignacio
Keigwin, Lloyd D
Barrows, Timothy T
Yokoyama, Yusuke
Southon, John
author_facet Martinez, Ignacio
Keigwin, Lloyd D
Barrows, Timothy T
Yokoyama, Yusuke
Southon, John
author_sort Martinez, Ignacio
title Age model and stable isotope record of eastern equatorial Pacific sediment cores ...
title_short Age model and stable isotope record of eastern equatorial Pacific sediment cores ...
title_full Age model and stable isotope record of eastern equatorial Pacific sediment cores ...
title_fullStr Age model and stable isotope record of eastern equatorial Pacific sediment cores ...
title_full_unstemmed Age model and stable isotope record of eastern equatorial Pacific sediment cores ...
title_sort age model and stable isotope record of eastern equatorial pacific sediment cores ...
publisher PANGAEA
publishDate 2003
url https://dx.doi.org/10.1594/pangaea.841739
https://doi.pangaea.de/10.1594/PANGAEA.841739
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://dx.doi.org/10.1029/2002pa000877
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.84173910.1029/2002pa000877
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