Temperature reconstruction of sediment cores from the northeastern Arabian Sea ...

In order to reconstruct the monsoonal variability during the late Holocene we investigated a complete, annually laminated sediment record from the oxygen minimum zone (OMZ) off Pakistan for oxygen isotopes of planktic foraminifera and alkenone-derived sea surface temperatures (SST). Significant SST...

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Main Authors: Doose-Rolinski, Heidi, Rogalla, U, Scheeder, Georg, Lückge, Andreas, von Rad, Ulrich
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.735717
https://doi.pangaea.de/10.1594/PANGAEA.735717
id ftdatacite:10.1594/pangaea.735717
record_format openpolar
spelling ftdatacite:10.1594/pangaea.735717 2024-09-15T18:09:51+00:00 Temperature reconstruction of sediment cores from the northeastern Arabian Sea ... Doose-Rolinski, Heidi Rogalla, U Scheeder, Georg Lückge, Andreas von Rad, Ulrich 2001 application/zip https://dx.doi.org/10.1594/pangaea.735717 https://doi.pangaea.de/10.1594/PANGAEA.735717 en eng PANGAEA https://dx.doi.org/10.1029/2000pa000511 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Box corer Reineck Kasten corer SO90 Sonne article Collection Supplementary Publication Series of Datasets 2001 ftdatacite https://doi.org/10.1594/pangaea.73571710.1029/2000pa000511 2024-07-03T13:16:23Z In order to reconstruct the monsoonal variability during the late Holocene we investigated a complete, annually laminated sediment record from the oxygen minimum zone (OMZ) off Pakistan for oxygen isotopes of planktic foraminifera and alkenone-derived sea surface temperatures (SST). Significant SST changes of up to 3°C which cannot be explained by changes in the alkenone-producing coccolithophorid species (inferred from the Gephyrocapsa oceanica / Emiliania huxleyi ratio) suggest that SST changes are driven by changes in the monsoon strength. Our high-(decadal)-resolution data indicate that the late Holocene in the northeastern Arabian Sea was not characterized by a stable uniform climate, as inferred from the Greenland ice cores, but by variations in the dominance of the SW monsoon conditions with significant effects on temperatures. Highest SST fluctuations of up to 3.0°C and 2.5°C were observed for the time interval from 4600 to 3300 years B.P. and during the past 500 years. The significant, short-term ... : Supplement to: Doose-Rolinski, Heidi; Rogalla, U; Scheeder, Georg; Lückge, Andreas; von Rad, Ulrich (2001): High resolution temperature and evaporation changes during the late Holocene in the northeastern Arabian Sea. Paleoceanography, 16(4), 358-367 ... Article in Journal/Newspaper Greenland Greenland ice cores DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Box corer Reineck
Kasten corer
SO90
Sonne
spellingShingle Box corer Reineck
Kasten corer
SO90
Sonne
Doose-Rolinski, Heidi
Rogalla, U
Scheeder, Georg
Lückge, Andreas
von Rad, Ulrich
Temperature reconstruction of sediment cores from the northeastern Arabian Sea ...
topic_facet Box corer Reineck
Kasten corer
SO90
Sonne
description In order to reconstruct the monsoonal variability during the late Holocene we investigated a complete, annually laminated sediment record from the oxygen minimum zone (OMZ) off Pakistan for oxygen isotopes of planktic foraminifera and alkenone-derived sea surface temperatures (SST). Significant SST changes of up to 3°C which cannot be explained by changes in the alkenone-producing coccolithophorid species (inferred from the Gephyrocapsa oceanica / Emiliania huxleyi ratio) suggest that SST changes are driven by changes in the monsoon strength. Our high-(decadal)-resolution data indicate that the late Holocene in the northeastern Arabian Sea was not characterized by a stable uniform climate, as inferred from the Greenland ice cores, but by variations in the dominance of the SW monsoon conditions with significant effects on temperatures. Highest SST fluctuations of up to 3.0°C and 2.5°C were observed for the time interval from 4600 to 3300 years B.P. and during the past 500 years. The significant, short-term ... : Supplement to: Doose-Rolinski, Heidi; Rogalla, U; Scheeder, Georg; Lückge, Andreas; von Rad, Ulrich (2001): High resolution temperature and evaporation changes during the late Holocene in the northeastern Arabian Sea. Paleoceanography, 16(4), 358-367 ...
format Article in Journal/Newspaper
author Doose-Rolinski, Heidi
Rogalla, U
Scheeder, Georg
Lückge, Andreas
von Rad, Ulrich
author_facet Doose-Rolinski, Heidi
Rogalla, U
Scheeder, Georg
Lückge, Andreas
von Rad, Ulrich
author_sort Doose-Rolinski, Heidi
title Temperature reconstruction of sediment cores from the northeastern Arabian Sea ...
title_short Temperature reconstruction of sediment cores from the northeastern Arabian Sea ...
title_full Temperature reconstruction of sediment cores from the northeastern Arabian Sea ...
title_fullStr Temperature reconstruction of sediment cores from the northeastern Arabian Sea ...
title_full_unstemmed Temperature reconstruction of sediment cores from the northeastern Arabian Sea ...
title_sort temperature reconstruction of sediment cores from the northeastern arabian sea ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.735717
https://doi.pangaea.de/10.1594/PANGAEA.735717
genre Greenland
Greenland ice cores
genre_facet Greenland
Greenland ice cores
op_relation https://dx.doi.org/10.1029/2000pa000511
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.73571710.1029/2000pa000511
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