Dissolution indices above the lysocline over the last ~40 ka measured in sediment core SSD044_GC01 from the central equatorial Indian Ocean
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2022
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| _version_ | 1867170115286466560 |
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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 | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_948518 |
| institution | PANGAEA |
| language | en |
| publishDate | 2022 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Dissolution indices above the lysocline over the last ~40 ka measured in sediment core SSD044_GC01 from the central equatorial Indian Ocean Yadav, Ramanand Naik, Sushant S Naidu, Pothuri Divakar AGE; calcite dissolution; carbonate ion; Central equatorial Indian Ocean; DEPTH, sediment/rock; Dissolution index, susceptible plankt foraminifera; Equatorial Indian Ocean; Foraminiferal dissolution indices; GC; Gravity corer; Lysocline; Sindhu Sadhana; Size index; SSD-044; SSD044_GC-01; Stereo microscope 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. |
| title | Dissolution indices above the lysocline over the last ~40 ka measured in sediment core SSD044_GC01 from the central equatorial Indian Ocean |
| topic | AGE; calcite dissolution; carbonate ion; Central equatorial Indian Ocean; DEPTH, sediment/rock; Dissolution index, susceptible plankt foraminifera; Equatorial Indian Ocean; Foraminiferal dissolution indices; GC; Gravity corer; Lysocline; Sindhu Sadhana; Size index; SSD-044; SSD044_GC-01; Stereo microscope |
| url | https://doi.org/10.1594/PANGAEA.948518 |