Stable isotope (δ13C and δ18O) of Plio/Pleistocene benthic foraminifers (Uvigerina spp., Uvigerina peregrina) of piston core SO213_08-2

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Hauptverfasser: Nürnberg, Dirk, Gehre, Nadine, Fessler, Sebastian
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2025
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author Nürnberg, Dirk
Gehre, Nadine
Fessler, Sebastian
author_facet Nürnberg, Dirk
Gehre, Nadine
Fessler, Sebastian
collection Datos científicos de ciencias marinas y ambientales
contents Sediment cores from the South Pacific (Chile Fracture Zone) obtained during RV SONNE cruise SO213 (SOPATRA) in December 2011 allow us to reconstruct lateral changes in the subpolar gyres in the pelagic South Pacific over the last ~3.3 million years. This dataset comprises benthic stable carbon (δ13C) and oxygen isotope (δ18O) data from piston core SO213_08-2, which was recovered from the South Pacific (37°29.47 S 95°20.61 W) from 2172 m water depth. Measurements were performed on the benthic foraminiferal species Uvigerina spp. and Uvigerina peregrina. Sampling and analytical studies were carried out from 0.365–9.965 m core depth at ~8 cm spatial resolution. The isotope analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV carbonate preparation device.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_983373
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Stable isotope (δ13C and δ18O) of Plio/Pleistocene benthic foraminifers (Uvigerina spp., Uvigerina peregrina) of piston core SO213_08-2
Nürnberg, Dirk
Gehre, Nadine
Fessler, Sebastian
AGE; Benthic foraminiferal stable isotopes; DEPTH, sediment/rock; Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV; Paleoceanography; Plio-Pleistocene; SO213/1; SO213/1_8-2TC; Sonne; SOPATRA; South Pacific; Species; TC; Trigger corer; Uvigerina spp., δ13C; Uvigerina spp., δ18O; X-ray fluorescence (XRF)
Sediment cores from the South Pacific (Chile Fracture Zone) obtained during RV SONNE cruise SO213 (SOPATRA) in December 2011 allow us to reconstruct lateral changes in the subpolar gyres in the pelagic South Pacific over the last ~3.3 million years. This dataset comprises benthic stable carbon (δ13C) and oxygen isotope (δ18O) data from piston core SO213_08-2, which was recovered from the South Pacific (37°29.47 S 95°20.61 W) from 2172 m water depth. Measurements were performed on the benthic foraminiferal species Uvigerina spp. and Uvigerina peregrina. Sampling and analytical studies were carried out from 0.365–9.965 m core depth at ~8 cm spatial resolution. The isotope analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV carbonate preparation device.
title Stable isotope (δ13C and δ18O) of Plio/Pleistocene benthic foraminifers (Uvigerina spp., Uvigerina peregrina) of piston core SO213_08-2
topic AGE; Benthic foraminiferal stable isotopes; DEPTH, sediment/rock; Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV; Paleoceanography; Plio-Pleistocene; SO213/1; SO213/1_8-2TC; Sonne; SOPATRA; South Pacific; Species; TC; Trigger corer; Uvigerina spp., δ13C; Uvigerina spp., δ18O; X-ray fluorescence (XRF)
url https://doi.org/10.1594/PANGAEA.983373