Species abundances above the lysocline over the last ~40 ka measured in sediment core SSD044_GC01 from the equatorial Indian Ocean

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Auteurs principaux: Yadav, Ramanand, Naik, Sushant S, Naidu, Pothuri Divakar
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2022
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author Yadav, Ramanand
Naik, Sushant S
Naidu, Pothuri Divakar
author_facet Yadav, Ramanand
Naik, Sushant S
Naidu, Pothuri Divakar
collection Datos científicos de ciencias marinas y ambientales
contents In this data set, we present percentage of calcium carbonate (CaCO3), ratio of organic carbon to total nitrogen, coarse fraction (>63 μm), size index percentage, total planktic foraminifera number, foraminifera fragment percentage (>125 μm), the ratio of benthic to planktic foraminifera, Globorotalia spp. percentage and Radiolarian percentage as well as the planktic foraminifera assemblage to show the carbonate dissolution in the deep sea region of the central Equatorial Indian Ocean (5°N & 77°E) over the last 40 ka. The marine sediment core SSD044_GC-01 was collected during the 044th Cruise of Research Vessel Sindhu (SSD044) Sadhana using a Gravity corer. To analyze the species abundance of planktic foraminifera, a portion of the Coarse Fraction (>63 μm) was dry sieved from 125 μm size fractions. Approximately ~300 intact tests of planktic foraminifera were picked and dissolution-sensitive and insensitive species abundance were made to show a carbonate ion concentration in the deep sea region of the study area during the last 43ka.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_948516
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Species abundances above the lysocline over the last ~40 ka measured in sediment core SSD044_GC01 from the equatorial Indian Ocean
Yadav, Ramanand
Naik, Sushant S
Naidu, Pothuri Divakar
Age; calcite dissolution; Calcium carbonate; Carbon, organic/nitrogen, organic ratio; carbonate ion; Central equatorial Indian Ocean; Coarse fraction; DEPTH, sediment/rock; Equatorial Indian Ocean; Foraminifera, benthic/planktic ratio; Foraminifera, planktic; Foraminifera, planktic, total; Foraminiferal dissolution indices; GC; Globorotalia menardii; Gravity corer; Lysocline; Radiolarians; Sindhu Sadhana; Size index; SSD-044; SSD044_GC-01; Stereo microscope; TOC analyzer, Shimadzu, TOC-L CPH/CPN; UIC-Coulometer
In this data set, we present percentage of calcium carbonate (CaCO3), ratio of organic carbon to total nitrogen, coarse fraction (>63 μm), size index percentage, total planktic foraminifera number, foraminifera fragment percentage (>125 μm), the ratio of benthic to planktic foraminifera, Globorotalia spp. percentage and Radiolarian percentage as well as the planktic foraminifera assemblage to show the carbonate dissolution in the deep sea region of the central Equatorial Indian Ocean (5°N & 77°E) over the last 40 ka. The marine sediment core SSD044_GC-01 was collected during the 044th Cruise of Research Vessel Sindhu (SSD044) Sadhana using a Gravity corer. To analyze the species abundance of planktic foraminifera, a portion of the Coarse Fraction (>63 μm) was dry sieved from 125 μm size fractions. Approximately ~300 intact tests of planktic foraminifera were picked and dissolution-sensitive and insensitive species abundance were made to show a carbonate ion concentration in the deep sea region of the study area during the last 43ka.
title Species abundances above the lysocline over the last ~40 ka measured in sediment core SSD044_GC01 from the equatorial Indian Ocean
topic Age; calcite dissolution; Calcium carbonate; Carbon, organic/nitrogen, organic ratio; carbonate ion; Central equatorial Indian Ocean; Coarse fraction; DEPTH, sediment/rock; Equatorial Indian Ocean; Foraminifera, benthic/planktic ratio; Foraminifera, planktic; Foraminifera, planktic, total; Foraminiferal dissolution indices; GC; Globorotalia menardii; Gravity corer; Lysocline; Radiolarians; Sindhu Sadhana; Size index; SSD-044; SSD044_GC-01; Stereo microscope; TOC analyzer, Shimadzu, TOC-L CPH/CPN; UIC-Coulometer
url https://doi.org/10.1594/PANGAEA.948516