_version_ 1867170121548562432
author Takata, Hiroyuki
Khim, Boo-Keun
Hyeong, Kiseong
Seo, Inah
Huh, Youngsook
Asahi, Hirofumi
Lee, Jongmin
Seto, Koji
author_facet Takata, Hiroyuki
Khim, Boo-Keun
Hyeong, Kiseong
Seo, Inah
Huh, Youngsook
Asahi, Hirofumi
Lee, Jongmin
Seto, Koji
collection Datos científicos de ciencias marinas y ambientales
contents We investigated benthic foraminifera in cores GPC03 and GPC04 in the northeast tropical Indian Ocean (TIO) over the past ~450 ka to evaluate the ballasting effect of particulate organic matter (POM) and the long-term zonal change during the mid-Brunhes dissolution interval (MBDI). Today, interannual climate and oceanographic variability in the TIO is governed by the Indian Ocean Dipole (IOD), which manifests as asymmetric zonal oceanographic change. Here we provide our sediment geochemical, stable oxygen and carbon isotope data and faunal data of benthic foraminifera in core GPC04.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_962907
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Sediment geochemical and stable isotope data of sediment core GPC04 at the Ninetyeast Ridge, Indian Ocean
Takata, Hiroyuki
Khim, Boo-Keun
Hyeong, Kiseong
Seo, Inah
Huh, Youngsook
Asahi, Hirofumi
Lee, Jongmin
Seto, Koji
AGE; Aluminium oxide; Bay of Bengal; Benthic foraminifera; Calcium oxide; DEPTH, sediment/rock; HI1808_GPC04; Iron oxide, Fe2O3; Isotope ratio mass spectrometry; Magnesium oxide; Major element; Manganese oxide; Oxygen isotope stratigraphy; Hidden Markov Model (HMM); PC; Phosphorus pentoxide; Piston corer; Potassium oxide; Principal component analyses (PCA); Principal component loading of PC axis 1; Silicon dioxide; Sodium oxide; Stable carbon and oxygen isotopes; Sulfur; Titanium dioxide; Trilobatus sacculifer, δ13C; Trilobatus sacculifer, δ18O; X-ray fluorescence (XRF), discrete measurement
We investigated benthic foraminifera in cores GPC03 and GPC04 in the northeast tropical Indian Ocean (TIO) over the past ~450 ka to evaluate the ballasting effect of particulate organic matter (POM) and the long-term zonal change during the mid-Brunhes dissolution interval (MBDI). Today, interannual climate and oceanographic variability in the TIO is governed by the Indian Ocean Dipole (IOD), which manifests as asymmetric zonal oceanographic change. Here we provide our sediment geochemical, stable oxygen and carbon isotope data and faunal data of benthic foraminifera in core GPC04.
title Sediment geochemical and stable isotope data of sediment core GPC04 at the Ninetyeast Ridge, Indian Ocean
topic AGE; Aluminium oxide; Bay of Bengal; Benthic foraminifera; Calcium oxide; DEPTH, sediment/rock; HI1808_GPC04; Iron oxide, Fe2O3; Isotope ratio mass spectrometry; Magnesium oxide; Major element; Manganese oxide; Oxygen isotope stratigraphy; Hidden Markov Model (HMM); PC; Phosphorus pentoxide; Piston corer; Potassium oxide; Principal component analyses (PCA); Principal component loading of PC axis 1; Silicon dioxide; Sodium oxide; Stable carbon and oxygen isotopes; Sulfur; Titanium dioxide; Trilobatus sacculifer, δ13C; Trilobatus sacculifer, δ18O; X-ray fluorescence (XRF), discrete measurement
url https://doi.org/10.1594/PANGAEA.962907