Age models and foraminifera assemblages from sediment profiles of the North Atlantic ...

Based on foraminiferal transfer-functions, the distribution patterns of early Holocene sea- surface temperatures (SST) were studied, using the information from 154 deep-sea sediment cores (92 Atlantic, 62 Indian Ocean and Western Pacific). For our reconstruction, we employed a uniform high-resolutio...

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Main Author: Schulz, Hartmut
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1995
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.877864
https://doi.pangaea.de/10.1594/PANGAEA.877864
id ftdatacite:10.1594/pangaea.877864
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spelling ftdatacite:10.1594/pangaea.877864 2024-09-15T18:23:30+00:00 Age models and foraminifera assemblages from sediment profiles of the North Atlantic ... Schulz, Hartmut 1995 application/zip https://dx.doi.org/10.1594/pangaea.877864 https://doi.pangaea.de/10.1594/PANGAEA.877864 en eng PANGAEA https://dx.doi.org/10.2312/reports-gpi.1995.73 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG article Collection Supplementary Publication Series of Datasets 1995 ftdatacite https://doi.org/10.1594/pangaea.87786410.2312/reports-gpi.1995.73 2024-08-01T11:01:20Z Based on foraminiferal transfer-functions, the distribution patterns of early Holocene sea- surface temperatures (SST) were studied, using the information from 154 deep-sea sediment cores (92 Atlantic, 62 Indian Ocean and Western Pacific). For our reconstruction, we employed a uniform high-resolution, AMS 14C-calibrated d18O-chronology, converted to a calendar timescale, and the new SIMMAX-Transfer-Technique in the Atlantic Oceans (Pflaumann et al. in press).The short-term SST fluctuations during the last 30,000 years are not directly related to the relatively slow changes in insolation during this period, reaching maximum seasonal deviations from modern values at approximaterly 11,000 years B.P. Although seasonal changes in solar radiation must have triggered global warming to the modern, interglacial mode, there is little evidence for linear warming and heat transport by ocean currents.The SIMMAX-temperature estimates indicate an early and rapid warming in the Equatorial Atlantic, as well as in the eastern ... : Supplement to: Schulz, Hartmut (1995): Meeresoberflächentemperaturen vor 10.000 Jahren - Auswirkungen des frühholozänen Insolationsmaximums = Sea-surface temperatures 10,000 years B.P. - consequences of the early Holocene insolation maximum. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 73, 156 pp ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
spellingShingle Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
Schulz, Hartmut
Age models and foraminifera assemblages from sediment profiles of the North Atlantic ...
topic_facet Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
description Based on foraminiferal transfer-functions, the distribution patterns of early Holocene sea- surface temperatures (SST) were studied, using the information from 154 deep-sea sediment cores (92 Atlantic, 62 Indian Ocean and Western Pacific). For our reconstruction, we employed a uniform high-resolution, AMS 14C-calibrated d18O-chronology, converted to a calendar timescale, and the new SIMMAX-Transfer-Technique in the Atlantic Oceans (Pflaumann et al. in press).The short-term SST fluctuations during the last 30,000 years are not directly related to the relatively slow changes in insolation during this period, reaching maximum seasonal deviations from modern values at approximaterly 11,000 years B.P. Although seasonal changes in solar radiation must have triggered global warming to the modern, interglacial mode, there is little evidence for linear warming and heat transport by ocean currents.The SIMMAX-temperature estimates indicate an early and rapid warming in the Equatorial Atlantic, as well as in the eastern ... : Supplement to: Schulz, Hartmut (1995): Meeresoberflächentemperaturen vor 10.000 Jahren - Auswirkungen des frühholozänen Insolationsmaximums = Sea-surface temperatures 10,000 years B.P. - consequences of the early Holocene insolation maximum. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 73, 156 pp ...
format Article in Journal/Newspaper
author Schulz, Hartmut
author_facet Schulz, Hartmut
author_sort Schulz, Hartmut
title Age models and foraminifera assemblages from sediment profiles of the North Atlantic ...
title_short Age models and foraminifera assemblages from sediment profiles of the North Atlantic ...
title_full Age models and foraminifera assemblages from sediment profiles of the North Atlantic ...
title_fullStr Age models and foraminifera assemblages from sediment profiles of the North Atlantic ...
title_full_unstemmed Age models and foraminifera assemblages from sediment profiles of the North Atlantic ...
title_sort age models and foraminifera assemblages from sediment profiles of the north atlantic ...
publisher PANGAEA
publishDate 1995
url https://dx.doi.org/10.1594/pangaea.877864
https://doi.pangaea.de/10.1594/PANGAEA.877864
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.2312/reports-gpi.1995.73
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.87786410.2312/reports-gpi.1995.73
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