Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1 ...

A sediment core from the western tropical Atlantic covering the last 21,000 yr has been analysed for centennial scale reconstruction of sea surface temperature (SST) and ice volume-corrected oxygen isotopic composition of sea water (delta18O(ivc-sw)) using Mg / Ca and delta18O of the shallow dwellin...

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Main Authors: Weldeab, Syee, Schneider, Ralph R, Kölling, Martin
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2006
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.738284
https://doi.pangaea.de/10.1594/PANGAEA.738284
id ftdatacite:10.1594/pangaea.738284
record_format openpolar
spelling ftdatacite:10.1594/pangaea.738284 2024-09-15T17:47:45+00:00 Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1 ... Weldeab, Syee Schneider, Ralph R Kölling, Martin 2006 application/zip https://dx.doi.org/10.1594/pangaea.738284 https://doi.pangaea.de/10.1594/PANGAEA.738284 en eng PANGAEA https://dx.doi.org/10.1016/j.epsl.2005.11.012 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type JOPSII-6 M34/4 Victor Hensen Meteor 1986 Center for Marine Environmental Sciences MARUM Geosciences, University of Bremen GeoB article Collection Supplementary Publication Series of Datasets 2006 ftdatacite https://doi.org/10.1594/pangaea.73828410.1016/j.epsl.2005.11.012 2024-07-03T13:10:33Z A sediment core from the western tropical Atlantic covering the last 21,000 yr has been analysed for centennial scale reconstruction of sea surface temperature (SST) and ice volume-corrected oxygen isotopic composition of sea water (delta18O(ivc-sw)) using Mg / Ca and delta18O of the shallow dwelling planktonic foraminifer Globigerinoides ruber (white). At a period between 15.5 and 17.5 kyr BP, the Mg / Ca SST and delta18O(ivc-sw), a proxy for sea surface salinity (SSS), reveals a warming of around 2.5 °C along with an increase in salinity. A second period of pronounced warming and SSS increase occurred between 11.6 and 13.5 kyr BP. Within age model uncertainties, both warming intervals were synchronous with air temperature increase over Antarctica and ice retreat in the southern South Atlantic and terminated with abrupt centennial scale SSS decrease and slight SST cooling in conjunction with interglacial reactivation of the meridional overturning circulation (MOC). We suggest that during these warm ... : Supplement to: Weldeab, Syee; Schneider, Ralph R; Kölling, Martin (2006): Deglacial sea surface temperature and salinity increase in the western tropical Atlantic in synchrony with high latitude climate instabilities. Earth and Planetary Science Letters, 241, 699-706 ... Article in Journal/Newspaper Antarc* Antarctica DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
JOPSII-6
M34/4
Victor Hensen
Meteor 1986
Center for Marine Environmental Sciences MARUM
Geosciences, University of Bremen GeoB
spellingShingle Gravity corer Kiel type
JOPSII-6
M34/4
Victor Hensen
Meteor 1986
Center for Marine Environmental Sciences MARUM
Geosciences, University of Bremen GeoB
Weldeab, Syee
Schneider, Ralph R
Kölling, Martin
Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1 ...
topic_facet Gravity corer Kiel type
JOPSII-6
M34/4
Victor Hensen
Meteor 1986
Center for Marine Environmental Sciences MARUM
Geosciences, University of Bremen GeoB
description A sediment core from the western tropical Atlantic covering the last 21,000 yr has been analysed for centennial scale reconstruction of sea surface temperature (SST) and ice volume-corrected oxygen isotopic composition of sea water (delta18O(ivc-sw)) using Mg / Ca and delta18O of the shallow dwelling planktonic foraminifer Globigerinoides ruber (white). At a period between 15.5 and 17.5 kyr BP, the Mg / Ca SST and delta18O(ivc-sw), a proxy for sea surface salinity (SSS), reveals a warming of around 2.5 °C along with an increase in salinity. A second period of pronounced warming and SSS increase occurred between 11.6 and 13.5 kyr BP. Within age model uncertainties, both warming intervals were synchronous with air temperature increase over Antarctica and ice retreat in the southern South Atlantic and terminated with abrupt centennial scale SSS decrease and slight SST cooling in conjunction with interglacial reactivation of the meridional overturning circulation (MOC). We suggest that during these warm ... : Supplement to: Weldeab, Syee; Schneider, Ralph R; Kölling, Martin (2006): Deglacial sea surface temperature and salinity increase in the western tropical Atlantic in synchrony with high latitude climate instabilities. Earth and Planetary Science Letters, 241, 699-706 ...
format Article in Journal/Newspaper
author Weldeab, Syee
Schneider, Ralph R
Kölling, Martin
author_facet Weldeab, Syee
Schneider, Ralph R
Kölling, Martin
author_sort Weldeab, Syee
title Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1 ...
title_short Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1 ...
title_full Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1 ...
title_fullStr Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1 ...
title_full_unstemmed Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1 ...
title_sort sea surface temperature and salinity reconstruction of sediment core geob3129-1 ...
publisher PANGAEA
publishDate 2006
url https://dx.doi.org/10.1594/pangaea.738284
https://doi.pangaea.de/10.1594/PANGAEA.738284
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation https://dx.doi.org/10.1016/j.epsl.2005.11.012
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.73828410.1016/j.epsl.2005.11.012
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