Planktonic foraminifera record and SST reconstruction for the last 130 ka in the Western South Atlantic ...

This work reconstructs Late Quaternary paleoceanographic changes in the western South Atlantic Ocean based on sedimentary core GL-77, recovered from the lower continental slope in the Campos basin, offshore SE Brazil. The studied interval comprises the last 130 ka. Changes in sea surface temperature...

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Main Authors: Petró, Sandro Monticelli, Pivel, Maria Alejandra G, Coimbra, Joao Carlos, Mizusaki, A M P
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2015
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.856128
https://doi.pangaea.de/10.1594/PANGAEA.856128
id ftdatacite:10.1594/pangaea.856128
record_format openpolar
spelling ftdatacite:10.1594/pangaea.856128 2024-09-15T18:30:56+00:00 Planktonic foraminifera record and SST reconstruction for the last 130 ka in the Western South Atlantic ... Petró, Sandro Monticelli Pivel, Maria Alejandra G Coimbra, Joao Carlos Mizusaki, A M P 2015 application/zip https://dx.doi.org/10.1594/pangaea.856128 https://doi.pangaea.de/10.1594/PANGAEA.856128 en eng PANGAEA https://dx.doi.org/10.4072/rbp.2016.1.01 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer article Collection Supplementary Publication Series of Datasets 2015 ftdatacite https://doi.org/10.1594/pangaea.85612810.4072/rbp.2016.1.01 2024-08-01T10:53:32Z This work reconstructs Late Quaternary paleoceanographic changes in the western South Atlantic Ocean based on sedimentary core GL-77, recovered from the lower continental slope in the Campos basin, offshore SE Brazil. The studied interval comprises the last 130 ka. Changes in sea surface temperature (SST) and paleoproductivity were estimated using the total planktonic foraminiferal fauna and oxygen isotope analyses. The age model was based on the oxygen isotope record, biostratigraphic datums and AMS 14C dating. It was observed that the Pleistocene/Holocene transition occurs within Globorotalia menardii Biozone Y, and is not coeval with the base of Biozone Z. The range between summer and winter SST estimates is larger during the glacial period compared to interglacials. Three peaks of low SST around 70, 50 - 45 and 20 ka coincided with periods of enhanced SE trade winds. Despite faunal differences between the last interglacial (MIS 5e) and the Holocene, our SST estimates suggest that SSTs did not differ ... : Supplement to: Petró, Sandro Monticelli; Pivel, Maria Alejandra G; Coimbra, Joao Carlos; Mizusaki, A M P (2016): Paleoceanographic changes through the last 130 ka in the Western South Atlantic based on planktonic foraminifera. Revista Brasileira de Paleontologia, 19(1), 3-14 ... Article in Journal/Newspaper Planktonic foraminifera South Atlantic Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer
spellingShingle Gravity corer
Petró, Sandro Monticelli
Pivel, Maria Alejandra G
Coimbra, Joao Carlos
Mizusaki, A M P
Planktonic foraminifera record and SST reconstruction for the last 130 ka in the Western South Atlantic ...
topic_facet Gravity corer
description This work reconstructs Late Quaternary paleoceanographic changes in the western South Atlantic Ocean based on sedimentary core GL-77, recovered from the lower continental slope in the Campos basin, offshore SE Brazil. The studied interval comprises the last 130 ka. Changes in sea surface temperature (SST) and paleoproductivity were estimated using the total planktonic foraminiferal fauna and oxygen isotope analyses. The age model was based on the oxygen isotope record, biostratigraphic datums and AMS 14C dating. It was observed that the Pleistocene/Holocene transition occurs within Globorotalia menardii Biozone Y, and is not coeval with the base of Biozone Z. The range between summer and winter SST estimates is larger during the glacial period compared to interglacials. Three peaks of low SST around 70, 50 - 45 and 20 ka coincided with periods of enhanced SE trade winds. Despite faunal differences between the last interglacial (MIS 5e) and the Holocene, our SST estimates suggest that SSTs did not differ ... : Supplement to: Petró, Sandro Monticelli; Pivel, Maria Alejandra G; Coimbra, Joao Carlos; Mizusaki, A M P (2016): Paleoceanographic changes through the last 130 ka in the Western South Atlantic based on planktonic foraminifera. Revista Brasileira de Paleontologia, 19(1), 3-14 ...
format Article in Journal/Newspaper
author Petró, Sandro Monticelli
Pivel, Maria Alejandra G
Coimbra, Joao Carlos
Mizusaki, A M P
author_facet Petró, Sandro Monticelli
Pivel, Maria Alejandra G
Coimbra, Joao Carlos
Mizusaki, A M P
author_sort Petró, Sandro Monticelli
title Planktonic foraminifera record and SST reconstruction for the last 130 ka in the Western South Atlantic ...
title_short Planktonic foraminifera record and SST reconstruction for the last 130 ka in the Western South Atlantic ...
title_full Planktonic foraminifera record and SST reconstruction for the last 130 ka in the Western South Atlantic ...
title_fullStr Planktonic foraminifera record and SST reconstruction for the last 130 ka in the Western South Atlantic ...
title_full_unstemmed Planktonic foraminifera record and SST reconstruction for the last 130 ka in the Western South Atlantic ...
title_sort planktonic foraminifera record and sst reconstruction for the last 130 ka in the western south atlantic ...
publisher PANGAEA
publishDate 2015
url https://dx.doi.org/10.1594/pangaea.856128
https://doi.pangaea.de/10.1594/PANGAEA.856128
genre Planktonic foraminifera
South Atlantic Ocean
genre_facet Planktonic foraminifera
South Atlantic Ocean
op_relation https://dx.doi.org/10.4072/rbp.2016.1.01
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.85612810.4072/rbp.2016.1.01
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