Calcium carbonate, sedimentary organic carbon, and shell weight of selected planktic foraminifera from ODP Hole 115-716A

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Auteurs principaux: Yadav, Ramanand, Naik, Sushant S
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2022
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author Yadav, Ramanand
Naik, Sushant S
author_facet Yadav, Ramanand
Naik, Sushant S
collection Datos científicos de ciencias marinas y ambientales
contents To understand the variations in carbonate burial for the last 30 kiloannum (ka), we have utilized a core from the Ocean DrillingProgram (ODP), Site716A (04.56°N and 73.17°E) retrieved from a water depth of 533 m from the Maldives (carbonate platform) Sea. We analyzed calcium carbonate (CaCO%), sedimentary organic carbon (C-org %) and shell weights of selected planktic foraminifera species (Globigerinoides ruber, Pulleniatina obliquiloculata and Neogloboquadrina dutertrei) to see the contrast in carbonate preservation during the late last glacial-Holocene. Our dataset reveals that carbonate preservation declined during the last glacial maximum (LGM) and the Holocene, probably due to organic matter degradation in sediments. The ratio of C-org/CaCO was relatively higher during the LGM than during the last deglacial period (LDP) and the Holocene. Furthermore, the heavier planktic foraminifera shell weights during the LDP indicate relatively increased carbonate preservation, which is linked to the deglacial release of carbon dioxide (CO₂) from the ocean to the atmosphere.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_949551
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Calcium carbonate, sedimentary organic carbon, and shell weight of selected planktic foraminifera from ODP Hole 115-716A
Yadav, Ramanand
Naik, Sushant S
115-716A; AGE; CaCO 3 %; Calcium carbonate; Carbon, organic; Carbon, organic/calcium carbonate ratio; carbonate preservation; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Globigerinoides ruber, shell, weight; Joides Resolution; Lakshadweep Sea; Leg115; Maldives carbonate platform; Neogloboquadrina dutertrei, shell, weight; Ocean Drilling Program; ODP; Pulleniatina obliquiloculata, shell, weight; shell weights
To understand the variations in carbonate burial for the last 30 kiloannum (ka), we have utilized a core from the Ocean DrillingProgram (ODP), Site716A (04.56°N and 73.17°E) retrieved from a water depth of 533 m from the Maldives (carbonate platform) Sea. We analyzed calcium carbonate (CaCO%), sedimentary organic carbon (C-org %) and shell weights of selected planktic foraminifera species (Globigerinoides ruber, Pulleniatina obliquiloculata and Neogloboquadrina dutertrei) to see the contrast in carbonate preservation during the late last glacial-Holocene. Our dataset reveals that carbonate preservation declined during the last glacial maximum (LGM) and the Holocene, probably due to organic matter degradation in sediments. The ratio of C-org/CaCO was relatively higher during the LGM than during the last deglacial period (LDP) and the Holocene. Furthermore, the heavier planktic foraminifera shell weights during the LDP indicate relatively increased carbonate preservation, which is linked to the deglacial release of carbon dioxide (CO₂) from the ocean to the atmosphere.
title Calcium carbonate, sedimentary organic carbon, and shell weight of selected planktic foraminifera from ODP Hole 115-716A
topic 115-716A; AGE; CaCO 3 %; Calcium carbonate; Carbon, organic; Carbon, organic/calcium carbonate ratio; carbonate preservation; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Globigerinoides ruber, shell, weight; Joides Resolution; Lakshadweep Sea; Leg115; Maldives carbonate platform; Neogloboquadrina dutertrei, shell, weight; Ocean Drilling Program; ODP; Pulleniatina obliquiloculata, shell, weight; shell weights
url https://doi.org/10.1594/PANGAEA.949551