Mg/Ca ratio of Planulina wuellerstorfi and isotopic composition of seawater from IODP Site 363-U1482

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Hauptverfasser: Chen, Yixin, Xu, Jian, Liu, Jun, Li, Tiegang, Xiong, Zhifang, Zhang, Peng, Yan, Hong
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2024
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author Chen, Yixin
Xu, Jian
Liu, Jun
Li, Tiegang
Xiong, Zhifang
Zhang, Peng
Yan, Hong
author_facet Chen, Yixin
Xu, Jian
Liu, Jun
Li, Tiegang
Xiong, Zhifang
Zhang, Peng
Yan, Hong
collection Datos científicos de ciencias marinas y ambientales
contents We present our work on a total of 1368 sediment samples spanning the past ~3.17–1.07 Ma from Site U1482 (15°3.32ʹS, 120°26.10ʹE, water depth of 1466m), which was drilled during the International Ocean Discovery Program Expedition 363 in the Timor Passage, the main exit of the Indonesian Throughflow to the Indian Ocean.Here we present benthic Mg/Ca ratios of Planulina wuellerstorfi during ~2-1.07 Ma. Together with the Mg/Ca-temperature calibration , oxygen isotopic composition of seawater (δ18Oseawater) and δ18Oresidual derived from benthic foraminiferal Mg/Ca ratios and benthic δ18O.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_948723
institution PANGAEA
language en
publishDate 2024
publisher PANGAEA
record_format pangaea
spellingShingle Mg/Ca ratio of Planulina wuellerstorfi and isotopic composition of seawater from IODP Site 363-U1482
Chen, Yixin
Xu, Jian
Liu, Jun
Li, Tiegang
Xiong, Zhifang
Zhang, Peng
Yan, Hong
363-U1482; AGE; benthic δ13C; benthic δ18O; Calculated (see README file in further details); COMPCORE; Composite Core; Exp363; Joides Resolution; Mg/Ca ratios; North west Australian continental margin; Planulina wuellerstorfi, Magnesium/Calcium ratio; Sea surface temperature; δ18O, seawater, reconstructed; δ18O, seawater, reconstructed, residual
We present our work on a total of 1368 sediment samples spanning the past ~3.17–1.07 Ma from Site U1482 (15°3.32ʹS, 120°26.10ʹE, water depth of 1466m), which was drilled during the International Ocean Discovery Program Expedition 363 in the Timor Passage, the main exit of the Indonesian Throughflow to the Indian Ocean.Here we present benthic Mg/Ca ratios of Planulina wuellerstorfi during ~2-1.07 Ma. Together with the Mg/Ca-temperature calibration , oxygen isotopic composition of seawater (δ18Oseawater) and δ18Oresidual derived from benthic foraminiferal Mg/Ca ratios and benthic δ18O.
title Mg/Ca ratio of Planulina wuellerstorfi and isotopic composition of seawater from IODP Site 363-U1482
topic 363-U1482; AGE; benthic δ13C; benthic δ18O; Calculated (see README file in further details); COMPCORE; Composite Core; Exp363; Joides Resolution; Mg/Ca ratios; North west Australian continental margin; Planulina wuellerstorfi, Magnesium/Calcium ratio; Sea surface temperature; δ18O, seawater, reconstructed; δ18O, seawater, reconstructed, residual
url https://doi.org/10.1594/PANGAEA.948723