Determination of millennial-scale climate variability based on alkenones in the western Atlantic Ocean ...

High-resolution records of alkenone-derived sea surface temperatures and elemental Ti/Ca ratios from a sediment core retrieved off northeastern Brazil (4° S) reveal short-term climate variability throughout the past 63,000 a. Large pulses of terrigenous sediment discharge, caused by increased precip...

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Main Authors: Jaeschke, Andrea, Rühlemann, Carsten, Arz, Helge Wolfgang, Heil, Gerrit M N, Lohmann, Gerrit
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2007
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.667499
https://doi.pangaea.de/10.1594/PANGAEA.667499
id ftdatacite:10.1594/pangaea.667499
record_format openpolar
spelling ftdatacite:10.1594/pangaea.667499 2024-09-15T17:47:50+00:00 Determination of millennial-scale climate variability based on alkenones in the western Atlantic Ocean ... Jaeschke, Andrea Rühlemann, Carsten Arz, Helge Wolfgang Heil, Gerrit M N Lohmann, Gerrit 2007 application/zip https://dx.doi.org/10.1594/pangaea.667499 https://doi.pangaea.de/10.1594/PANGAEA.667499 en eng PANGAEA https://dx.doi.org/10.1029/2006pa001391 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type M34/4 Meteor 1986 Geosciences, University of Bremen GeoB article Collection Supplementary Publication Series of Datasets 2007 ftdatacite https://doi.org/10.1594/pangaea.66749910.1029/2006pa001391 2024-07-03T13:10:33Z High-resolution records of alkenone-derived sea surface temperatures and elemental Ti/Ca ratios from a sediment core retrieved off northeastern Brazil (4° S) reveal short-term climate variability throughout the past 63,000 a. Large pulses of terrigenous sediment discharge, caused by increased precipitation in the Brazilian hinterland, coincide with Heinrich events and the Younger Dryas period. Terrigenous input maxima related to Heinrich events H6–H2 are characterized by rapid cooling of surface water ranging between 0.5 and 2° C. This signature is consistent with a climate model experiment where a reduction of the Atlantic meridional overturning circulation (AMOC) and related North Atlantic cooling causes intensification of NE trade winds and a southward movement of the Intertropical Convergence Zone, resulting in enhanced precipitation off northeastern Brazil. During deglaciation the surface temperature evolution at the core site predominantly followed the Antarctic warming trend, including a cooling, ... : Supplement to: Jaeschke, Andrea; Rühlemann, Carsten; Arz, Helge Wolfgang; Heil, Gerrit M N; Lohmann, Gerrit (2007): Coupling of millennial-scale changes in sea surface temperature and precipitation off northeastern Brazil with high-latitude climate shifts during the last glacial period. Paleoceanography, 22(4), PA4206 ... Article in Journal/Newspaper Antarc* Antarctic North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
M34/4
Meteor 1986
Geosciences, University of Bremen GeoB
spellingShingle Gravity corer Kiel type
M34/4
Meteor 1986
Geosciences, University of Bremen GeoB
Jaeschke, Andrea
Rühlemann, Carsten
Arz, Helge Wolfgang
Heil, Gerrit M N
Lohmann, Gerrit
Determination of millennial-scale climate variability based on alkenones in the western Atlantic Ocean ...
topic_facet Gravity corer Kiel type
M34/4
Meteor 1986
Geosciences, University of Bremen GeoB
description High-resolution records of alkenone-derived sea surface temperatures and elemental Ti/Ca ratios from a sediment core retrieved off northeastern Brazil (4° S) reveal short-term climate variability throughout the past 63,000 a. Large pulses of terrigenous sediment discharge, caused by increased precipitation in the Brazilian hinterland, coincide with Heinrich events and the Younger Dryas period. Terrigenous input maxima related to Heinrich events H6–H2 are characterized by rapid cooling of surface water ranging between 0.5 and 2° C. This signature is consistent with a climate model experiment where a reduction of the Atlantic meridional overturning circulation (AMOC) and related North Atlantic cooling causes intensification of NE trade winds and a southward movement of the Intertropical Convergence Zone, resulting in enhanced precipitation off northeastern Brazil. During deglaciation the surface temperature evolution at the core site predominantly followed the Antarctic warming trend, including a cooling, ... : Supplement to: Jaeschke, Andrea; Rühlemann, Carsten; Arz, Helge Wolfgang; Heil, Gerrit M N; Lohmann, Gerrit (2007): Coupling of millennial-scale changes in sea surface temperature and precipitation off northeastern Brazil with high-latitude climate shifts during the last glacial period. Paleoceanography, 22(4), PA4206 ...
format Article in Journal/Newspaper
author Jaeschke, Andrea
Rühlemann, Carsten
Arz, Helge Wolfgang
Heil, Gerrit M N
Lohmann, Gerrit
author_facet Jaeschke, Andrea
Rühlemann, Carsten
Arz, Helge Wolfgang
Heil, Gerrit M N
Lohmann, Gerrit
author_sort Jaeschke, Andrea
title Determination of millennial-scale climate variability based on alkenones in the western Atlantic Ocean ...
title_short Determination of millennial-scale climate variability based on alkenones in the western Atlantic Ocean ...
title_full Determination of millennial-scale climate variability based on alkenones in the western Atlantic Ocean ...
title_fullStr Determination of millennial-scale climate variability based on alkenones in the western Atlantic Ocean ...
title_full_unstemmed Determination of millennial-scale climate variability based on alkenones in the western Atlantic Ocean ...
title_sort determination of millennial-scale climate variability based on alkenones in the western atlantic ocean ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.667499
https://doi.pangaea.de/10.1594/PANGAEA.667499
genre Antarc*
Antarctic
North Atlantic
genre_facet Antarc*
Antarctic
North Atlantic
op_relation https://dx.doi.org/10.1029/2006pa001391
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.66749910.1029/2006pa001391
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