Age chronology of mixed planktic foraminifera from sediment core SK237 GC09, northern Indian Ocean

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Main Authors: Saraswat, Rajeev, Mackensen, Andreas
Format: Dataset Open Access
Language:en
Published: PANGAEA 2020
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author Saraswat, Rajeev
Mackensen, Andreas
author_facet Saraswat, Rajeev
Mackensen, Andreas
collection Datos científicos de ciencias marinas y ambientales
contents The gravity core (SK237 GC09) was collected from the central equatorial Indian Ocean (12°00.59′N, 70°52.20′E) from a water depth of 3001 m, during the 237th cruise of the ORV Sagar Kanya. The top section of the core was dated by four accelerator mass spectrometer radiocarbon dates on mixed planktic foraminifera, measured at the Center for Applied Isotope Studies, the University of Georgia, USA. The 14C dates were calibrated by using Calib7.0 software and MARINE13 dataset (Stuiver et al., 2018). The chronology of the older section was established by comparing the stable oxygen isotopic (δ18O) ratio of surface-dwelling planktic foraminifera Globigerinoides ruber (white) with the LR04 global isostack (Lisiecki and Raymo, 2005). The elemental (Mg/Ca) and stable oxygen isotopic (δ18O) ratio of surface-dwelling planktic foraminifera Globigerinoides ruber (white) was analyzed to reconstruct SST and evaporation-precipitation changes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_913741
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Age chronology of mixed planktic foraminifera from sediment core SK237 GC09, northern Indian Ocean
Saraswat, Rajeev
Mackensen, Andreas
AGE; Age, 14C calibrated; Age, error; Age model; Age model according to Lisiecki & Raymo (2005) [LR04]; DEPTH, sediment/rock; GC; Glacial; Globigerinoides ruber; Gravity corer; Indian Ocean; Indo Pacific Warm Pool; Interglacial; Interval comments; Isotopic event; Mg/Ca; northern Indian Ocean; Sedimentation rate; SK237_GC09; δ18O
The gravity core (SK237 GC09) was collected from the central equatorial Indian Ocean (12°00.59′N, 70°52.20′E) from a water depth of 3001 m, during the 237th cruise of the ORV Sagar Kanya. The top section of the core was dated by four accelerator mass spectrometer radiocarbon dates on mixed planktic foraminifera, measured at the Center for Applied Isotope Studies, the University of Georgia, USA. The 14C dates were calibrated by using Calib7.0 software and MARINE13 dataset (Stuiver et al., 2018). The chronology of the older section was established by comparing the stable oxygen isotopic (δ18O) ratio of surface-dwelling planktic foraminifera Globigerinoides ruber (white) with the LR04 global isostack (Lisiecki and Raymo, 2005). The elemental (Mg/Ca) and stable oxygen isotopic (δ18O) ratio of surface-dwelling planktic foraminifera Globigerinoides ruber (white) was analyzed to reconstruct SST and evaporation-precipitation changes.
title Age chronology of mixed planktic foraminifera from sediment core SK237 GC09, northern Indian Ocean
topic AGE; Age, 14C calibrated; Age, error; Age model; Age model according to Lisiecki & Raymo (2005) [LR04]; DEPTH, sediment/rock; GC; Glacial; Globigerinoides ruber; Gravity corer; Indian Ocean; Indo Pacific Warm Pool; Interglacial; Interval comments; Isotopic event; Mg/Ca; northern Indian Ocean; Sedimentation rate; SK237_GC09; δ18O
url https://doi.org/10.1594/PANGAEA.913741