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author Jöhnck, Janika
Kuhnt, Wolfgang
Holbourn, Ann E
Andersen, Nils
author_facet Jöhnck, Janika
Kuhnt, Wolfgang
Holbourn, Ann E
Andersen, Nils
collection Datos científicos de ciencias marinas y ambientales
contents We reconstructed the Indian Monsoon variability of the Earth's strongest hydrological system, at International Ocean Discovery Program (IODP) Expedition 353 Site U1448 in the Andaman Sea over the interval 6.24 to 4.91 Ma. We used high-resolution benthic and planktic foraminiferal carbon and oxygen isotopes and Mg/Ca measurements of the mixed layer foraminifer Trilobatus sacculifer to reconstruct the isotopic composition of seawater (δ¹⁸Osw) and the gradient between planktic and benthic foraminiferal δ¹³C.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_921091
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Benthic and planktic foraminiferal carbon and oxygen isotopes and Mg/Ca-derived mixed layer temperatures from IODP Hole 353-U1448A and 353-U1448B in the Andaman Sea
Jöhnck, Janika
Kuhnt, Wolfgang
Holbourn, Ann E
Andersen, Nils
353-U1448A; 353-U1448B; AGE; Bay of Bengal; Calculated, according to Anand et al. (2003); Calculated according to (Mohtadi et al. 2014); Calculated according to Bemis et al., 1998; CDRILL; Cibicidoides wuellerstorfi, δ13C; Core drilling; Corrected; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Event label; Exp353; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Indian Monsoon; Joides Resolution; Mass spectrometer; Mg/Ca paleothermometry; Miocene-Pliocene transition; Mixed layer temperature; MSPEC; Sample code/label; see Jöhnck et al. (2020); Size fraction; Species; Stable isotopes; Trilobatus sacculifer, Magnesium/Calcium ratio; Trilobatus sacculifer, δ13C; Trilobatus sacculifer, δ18O; Δδ13C, gradient; Δδ18O, gradient; δ18O, seawater, reconstructed
We reconstructed the Indian Monsoon variability of the Earth's strongest hydrological system, at International Ocean Discovery Program (IODP) Expedition 353 Site U1448 in the Andaman Sea over the interval 6.24 to 4.91 Ma. We used high-resolution benthic and planktic foraminiferal carbon and oxygen isotopes and Mg/Ca measurements of the mixed layer foraminifer Trilobatus sacculifer to reconstruct the isotopic composition of seawater (δ¹⁸Osw) and the gradient between planktic and benthic foraminiferal δ¹³C.
title Benthic and planktic foraminiferal carbon and oxygen isotopes and Mg/Ca-derived mixed layer temperatures from IODP Hole 353-U1448A and 353-U1448B in the Andaman Sea
topic 353-U1448A; 353-U1448B; AGE; Bay of Bengal; Calculated, according to Anand et al. (2003); Calculated according to (Mohtadi et al. 2014); Calculated according to Bemis et al., 1998; CDRILL; Cibicidoides wuellerstorfi, δ13C; Core drilling; Corrected; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Event label; Exp353; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Indian Monsoon; Joides Resolution; Mass spectrometer; Mg/Ca paleothermometry; Miocene-Pliocene transition; Mixed layer temperature; MSPEC; Sample code/label; see Jöhnck et al. (2020); Size fraction; Species; Stable isotopes; Trilobatus sacculifer, Magnesium/Calcium ratio; Trilobatus sacculifer, δ13C; Trilobatus sacculifer, δ18O; Δδ13C, gradient; Δδ18O, gradient; δ18O, seawater, reconstructed
url https://doi.org/10.1594/PANGAEA.921091