Calculated seawater d18O record of the deep thermocline (Globorotalia truncatulinoides) corrected for global ice volume from 2.5 to 1 Ma

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Autores principales: Raddatz, Jacek, Zeeden, Christian, Kniest, Jorit, Nürnberg, Dirk
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2025
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author Raddatz, Jacek
Zeeden, Christian
Kniest, Jorit
Nürnberg, Dirk
author_facet Raddatz, Jacek
Zeeden, Christian
Kniest, Jorit
Nürnberg, Dirk
collection Datos científicos de ciencias marinas y ambientales
contents Measured stable oxygen isotopes measured on a surface dwelling (G.ruber) and deep dwelling foraminifera (G truncatulinoides) from a sediment core in the tropical Pacific retrieved during research cruise SO-225 to the Manihiki Plateau. Oxygen isotopes ratios of this dataset have been combined with previously published temperature reconstruction using Mg/Ca ratios (Raddatz et al. 2017, Raddatz et al 2019) to calculate the d18O of seawater through time (2.5 to 1.0 Ma) of the sea surface and deep thermocline. We also provide a surface and deep thermocline d18O-seawater record that has been correct for global ice volume using the modelled ice sheet evolution through the Quaternary by Bintanja and Van de Wal (2008).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_984810
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Calculated seawater d18O record of the deep thermocline (Globorotalia truncatulinoides) corrected for global ice volume from 2.5 to 1 Ma
Raddatz, Jacek
Zeeden, Christian
Kniest, Jorit
Nürnberg, Dirk
AGE; Globorotalia truncatulinoides, δ18O; MANIHIKI II; Manihiki Plateau; PC; Piston corer; Planktonic foraminifera; SO225; SO225_53-3; Sonne; South Pacific Ocean; West Pacific Warm Pool
Measured stable oxygen isotopes measured on a surface dwelling (G.ruber) and deep dwelling foraminifera (G truncatulinoides) from a sediment core in the tropical Pacific retrieved during research cruise SO-225 to the Manihiki Plateau. Oxygen isotopes ratios of this dataset have been combined with previously published temperature reconstruction using Mg/Ca ratios (Raddatz et al. 2017, Raddatz et al 2019) to calculate the d18O of seawater through time (2.5 to 1.0 Ma) of the sea surface and deep thermocline. We also provide a surface and deep thermocline d18O-seawater record that has been correct for global ice volume using the modelled ice sheet evolution through the Quaternary by Bintanja and Van de Wal (2008).
title Calculated seawater d18O record of the deep thermocline (Globorotalia truncatulinoides) corrected for global ice volume from 2.5 to 1 Ma
topic AGE; Globorotalia truncatulinoides, δ18O; MANIHIKI II; Manihiki Plateau; PC; Piston corer; Planktonic foraminifera; SO225; SO225_53-3; Sonne; South Pacific Ocean; West Pacific Warm Pool
url https://doi.org/10.1594/PANGAEA.984810