Sea-surface temperature reconstruction for sediment core GeoB1023-5 ...

Sediment core GeoB 1023-5 from the eastern South Atlantic was investigated at high temporal resolution for variations of sea-surface temperature (SST) during the past 22 kyr, using the alkenone (UK'37) method. SSTs increased by 3.5°C from about 18°C during the Last Ice Age (21±2 cal kyr BP) to...

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Main Authors: Kim, Jung-Hyun, Schneider, Ralph R, Müller, Peter J, Wefer, Gerold
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2002
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.735766
https://doi.pangaea.de/10.1594/PANGAEA.735766
id ftdatacite:10.1594/pangaea.735766
record_format openpolar
spelling ftdatacite:10.1594/pangaea.735766 2024-09-15T18:23:37+00:00 Sea-surface temperature reconstruction for sediment core GeoB1023-5 ... Kim, Jung-Hyun Schneider, Ralph R Müller, Peter J Wefer, Gerold 2002 application/zip https://dx.doi.org/10.1594/pangaea.735766 https://doi.pangaea.de/10.1594/PANGAEA.735766 en eng PANGAEA https://dx.doi.org/10.1016/s0012-821x(01)00545-3 https://dx.doi.org/10.1016/s0012-821x(02)00896-8 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type M6/6 Meteor 1986 Geosciences, University of Bremen GeoB article Collection Supplementary Publication Series of Datasets 2002 ftdatacite https://doi.org/10.1594/pangaea.73576610.1016/s0012-821x(01)00545-310.1016/s0012-821x(02)00896-8 2024-07-03T13:16:23Z Sediment core GeoB 1023-5 from the eastern South Atlantic was investigated at high temporal resolution for variations of sea-surface temperature (SST) during the past 22 kyr, using the alkenone (UK'37) method. SSTs increased by 3.5°C from about 18°C during the Last Ice Age (21±2 cal kyr BP) to about 21.5°C at 14.5 cal kyr BP. This warming trend associated with the deglaciation phase was followed by a cooling event with lowest SSTs near 20°C, persisting for about 1000 years between 13 and 12 cal kyr BP. The SSTs then continued to increase to about 22.5°C at the Holocene climatic optimum at 7 cal kyr BP, and decreased again during the Late Holocene to a core-top value of 19.8°C that is comparable to modern annual mean SST values. When compared with alkenone SST records from the eastern North Atlantic, our SST record indicates continuous warming throughout the deglaciation phase in the Benguela Current, while its northern counterpart, the Canary Current, experienced prominent cooling during 'Heinrich Event 1' ... : Supplement to: Kim, Jung-Hyun; Schneider, Ralph R; Müller, Peter J; Wefer, Gerold (2002): Interhemispheric comparison of deglacial sea-surface temperature patterns in Atlantic eastern boundary currents. Earth and Planetary Science Letters, 194(3-4), 383-393 ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
M6/6
Meteor 1986
Geosciences, University of Bremen GeoB
spellingShingle Gravity corer Kiel type
M6/6
Meteor 1986
Geosciences, University of Bremen GeoB
Kim, Jung-Hyun
Schneider, Ralph R
Müller, Peter J
Wefer, Gerold
Sea-surface temperature reconstruction for sediment core GeoB1023-5 ...
topic_facet Gravity corer Kiel type
M6/6
Meteor 1986
Geosciences, University of Bremen GeoB
description Sediment core GeoB 1023-5 from the eastern South Atlantic was investigated at high temporal resolution for variations of sea-surface temperature (SST) during the past 22 kyr, using the alkenone (UK'37) method. SSTs increased by 3.5°C from about 18°C during the Last Ice Age (21±2 cal kyr BP) to about 21.5°C at 14.5 cal kyr BP. This warming trend associated with the deglaciation phase was followed by a cooling event with lowest SSTs near 20°C, persisting for about 1000 years between 13 and 12 cal kyr BP. The SSTs then continued to increase to about 22.5°C at the Holocene climatic optimum at 7 cal kyr BP, and decreased again during the Late Holocene to a core-top value of 19.8°C that is comparable to modern annual mean SST values. When compared with alkenone SST records from the eastern North Atlantic, our SST record indicates continuous warming throughout the deglaciation phase in the Benguela Current, while its northern counterpart, the Canary Current, experienced prominent cooling during 'Heinrich Event 1' ... : Supplement to: Kim, Jung-Hyun; Schneider, Ralph R; Müller, Peter J; Wefer, Gerold (2002): Interhemispheric comparison of deglacial sea-surface temperature patterns in Atlantic eastern boundary currents. Earth and Planetary Science Letters, 194(3-4), 383-393 ...
format Article in Journal/Newspaper
author Kim, Jung-Hyun
Schneider, Ralph R
Müller, Peter J
Wefer, Gerold
author_facet Kim, Jung-Hyun
Schneider, Ralph R
Müller, Peter J
Wefer, Gerold
author_sort Kim, Jung-Hyun
title Sea-surface temperature reconstruction for sediment core GeoB1023-5 ...
title_short Sea-surface temperature reconstruction for sediment core GeoB1023-5 ...
title_full Sea-surface temperature reconstruction for sediment core GeoB1023-5 ...
title_fullStr Sea-surface temperature reconstruction for sediment core GeoB1023-5 ...
title_full_unstemmed Sea-surface temperature reconstruction for sediment core GeoB1023-5 ...
title_sort sea-surface temperature reconstruction for sediment core geob1023-5 ...
publisher PANGAEA
publishDate 2002
url https://dx.doi.org/10.1594/pangaea.735766
https://doi.pangaea.de/10.1594/PANGAEA.735766
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1016/s0012-821x(01)00545-3
https://dx.doi.org/10.1016/s0012-821x(02)00896-8
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.73576610.1016/s0012-821x(01)00545-310.1016/s0012-821x(02)00896-8
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