Benthic stable isotopes of sediment core M94-482 PC

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Autore principale: Nürnberg, Dirk
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2022
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author Nürnberg, Dirk
author_facet Nürnberg, Dirk
collection Datos científicos de ciencias marinas y ambientales
contents Proxy parameter of core M94-482 PC: Benthic stable isotopes of sediment core M94-482 PC. Isotope analyses were performed on the benthic foraminiferal species Uvigerina peregrina. Sedimentological and logging data as well as the foraminiferal analyses were performed on piston core M94-482 PC, which was recovered from the northern Campeche Bank (Gulf of Mexico; 23°49.155'N 87°07.752'W) from 630 m water depth during R/V Meteor Cruise M94 in 2013 (https://doi.org/10.2312/cr_m94). Sampling and analytical studies were carried out from ~0.5 cm to 879 cm core depth at 1-5 cm spatial resolution. The records cover the last ~288 kyrs. The stable carbon (δ13C; ‰ VPDB) and oxygen isotope (δ18O, ‰ VPDB) analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV Carbonate Preparation Device. The isotope data provide stratigraphical information.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_947795
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Benthic stable isotopes of sediment core M94-482 PC
Nürnberg, Dirk
AGE; Benthic stable isotopes; DEPTH, sediment/rock; Gulf of Mexico; Loop Current; M94; M94_482; Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV; Meteor (1986); Mid Pleistocene Transition; northern Campeche bank; northern hemisphere cooling; PC; Piston corer; Surface and Intermediate Water Variability in Yucatan Strait and the Gulf of Mexico; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O; YUCATAN_THROUGHFLOW
Proxy parameter of core M94-482 PC: Benthic stable isotopes of sediment core M94-482 PC. Isotope analyses were performed on the benthic foraminiferal species Uvigerina peregrina. Sedimentological and logging data as well as the foraminiferal analyses were performed on piston core M94-482 PC, which was recovered from the northern Campeche Bank (Gulf of Mexico; 23°49.155'N 87°07.752'W) from 630 m water depth during R/V Meteor Cruise M94 in 2013 (https://doi.org/10.2312/cr_m94). Sampling and analytical studies were carried out from ~0.5 cm to 879 cm core depth at 1-5 cm spatial resolution. The records cover the last ~288 kyrs. The stable carbon (δ13C; ‰ VPDB) and oxygen isotope (δ18O, ‰ VPDB) analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV Carbonate Preparation Device. The isotope data provide stratigraphical information.
title Benthic stable isotopes of sediment core M94-482 PC
topic AGE; Benthic stable isotopes; DEPTH, sediment/rock; Gulf of Mexico; Loop Current; M94; M94_482; Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV; Meteor (1986); Mid Pleistocene Transition; northern Campeche bank; northern hemisphere cooling; PC; Piston corer; Surface and Intermediate Water Variability in Yucatan Strait and the Gulf of Mexico; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O; YUCATAN_THROUGHFLOW
url https://doi.org/10.1594/PANGAEA.947795