Dissolution indices above the lysocline over the last ~40 ka measured in sediment core SSD044_GC01 from the central equatorial Indian Ocean
2022
Yadav, Ramanand | Naik, Sushant S | Naidu, Pothuri Divakar
We have deciphered the deep sea carbonate-ion content and associated dissolution in the central Equatorial Indian Ocean (5°N & 77°E). The marine sedimentary core was collected during the 044th Cruise of RV Sindhu Sadhana (SSD-044/GC01) using Gravity corer, which covers the period of the last 43 ka. Variations of dissolution indices were observed for the last 43ka. The overall data set shows the variation in carbonate dissolution during the late Glacial to Holocene epoc.
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Библиографическая информация
Издатель
PANGAEA
Другие темы
Ssd044_gc-01; Sindhu sadhana; Foraminiferal dissolution indices; Calcite dissolution; Sediment/rock; Central equatorial indian ocean; Dissolution index; Stereo microscope; Equatorial indian ocean; Carbonate ion; Size index; Susceptible plankt foraminifera; Ssd-044; Gravity corer
Язык
Английский
Формат
text/tab-separated-values, 148 data points
Лицензия
CC-BY-4.0: Creative Commons Attribution 4.0 International, Access constraints: unrestricted, info:eu-repo/semantics/openAccess
Тип
Dataset
2024-11-28
Dublin Core
Поставщик данных
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