Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years

G.M. Ganssen; F.J.C. Peeters; B. Metcalfe; P. Anand; S.J.A. Jung; D. Kroon; G.J.A. Brummer

doi:10.5194/cpd-6-2795-2010

Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years

G.M. Ganssen, F.J.C. Peeters, B. Metcalfe, P. Anand, S.J.A. Jung, D. Kroon, G.J.A. Brummer

Earth and Climate

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Abstract

The oxygen isotopic composition of planktonic foraminifera tests is one of the widest used geochemical tools to reconstruct past changes of physical parameters of the upper ocean. It is common practice to analyze multiple individuals from a mono-specific population and assume that the outcome reflects a mean value of the environmental conditions during calcification of the analyzed individuals. Here we present the oxygen isotope composition of individual specimens of the surface-dwelling species Globigerinoides ruber and Globigerina bulloides from sediment cores in the Western Arabian Sea off Somalia, inferred as indicators of past seasonal ranges in temperature. Combining the δ

Original language	English
Pages (from-to)	1337-1349
Number of pages	13
Journal	Climate of the Past
Volume	7
Issue number	4
DOIs	https://doi.org/10.5194/cpd-6-2795-2010 https://doi.org/10.5194/cp-7-1337-2011
Publication status	Published - 8 Dec 2011

Bibliographical note

First published in: Climate of the Past Discussions (issn 1814-9340), 6 (2010), pag.2795-2814

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title = "Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years",

abstract = "The oxygen isotopic composition of planktonic foraminifera tests is one of the widest used geochemical tools to reconstruct past changes of physical parameters of the upper ocean. It is common practice to analyze multiple individuals from a mono-specific population and assume that the outcome reflects a mean value of the environmental conditions during calcification of the analyzed individuals. Here we present the oxygen isotope composition of individual specimens of the surface-dwelling species Globigerinoides ruber and Globigerina bulloides from sediment cores in the Western Arabian Sea off Somalia, inferred as indicators of past seasonal ranges in temperature. Combining the δ",

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AU - Ganssen, G.M.

AU - Peeters, F.J.C.

AU - Metcalfe, B.

AU - Anand, P.

AU - Jung, S.J.A.

AU - Kroon, D.

AU - Brummer, G.J.A.

N1 - First published in: Climate of the Past Discussions (issn 1814-9340), 6 (2010), pag.2795-2814

PY - 2011/12/8

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N2 - The oxygen isotopic composition of planktonic foraminifera tests is one of the widest used geochemical tools to reconstruct past changes of physical parameters of the upper ocean. It is common practice to analyze multiple individuals from a mono-specific population and assume that the outcome reflects a mean value of the environmental conditions during calcification of the analyzed individuals. Here we present the oxygen isotope composition of individual specimens of the surface-dwelling species Globigerinoides ruber and Globigerina bulloides from sediment cores in the Western Arabian Sea off Somalia, inferred as indicators of past seasonal ranges in temperature. Combining the δ

AB - The oxygen isotopic composition of planktonic foraminifera tests is one of the widest used geochemical tools to reconstruct past changes of physical parameters of the upper ocean. It is common practice to analyze multiple individuals from a mono-specific population and assume that the outcome reflects a mean value of the environmental conditions during calcification of the analyzed individuals. Here we present the oxygen isotope composition of individual specimens of the surface-dwelling species Globigerinoides ruber and Globigerina bulloides from sediment cores in the Western Arabian Sea off Somalia, inferred as indicators of past seasonal ranges in temperature. Combining the δ

U2 - 10.5194/cpd-6-2795-2010

DO - 10.5194/cpd-6-2795-2010

M3 - Article

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EP - 1349

JO - Climate of the Past

JF - Climate of the Past

SN - 1814-9324

IS - 4

ER -

Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years

Abstract

Bibliographical note

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