IODP Expedition 392 Inorganic carbon (coulometer)

Inorganic carbon (carbonate) is determined by coulometry, which uses a photodetection cell to measure carbon dioxide evolved during sample acidification. Report includes percent inorganic carbon and calcium carbonate.

Bibliographic Details
Main Authors:	Uenzelmann-Neben, Gabriele, Bohaty, Steven M., Childress, Laurel B., Archontikis, Odysseas A., Batenburg, Sietske J., Bijl, Peter K., Burkett, Ashley M., Cawthra, Hayley C., Chanda, Pratyusha, Coenen, Jason J., Dallanave, Edoardo, Davidson, Peter C., Doiron, Kelsey E., Geldmacher, Jörg, Gürer, Derya, Haynes, Shannon J., Herrle, Jens O., Ichiyama, Yuji, Jana, Debadrita, Jones, Matthew M., Kato, Chie, Kulhanek, Denise K., Li, Juan, Liu, Jia, McManus, James, Minakov, Alexander N., Penman, Donald E., Sprain, Courtney J., Tessin, Allyson C., Wagner, Thomas, Westerhold, Thomas
Other Authors:	International Ocean Discovery Program
Format:	Dataset
Language:	unknown
Published:	2023
Subjects:	International Ocean Discovery Program IODP JOIDES Resolution Expedition 392 Site U1579 Site U1580 Site U1581 Site U1582 Algulhas Plateau Cretaceous Climate Earth connections Climate and ocean change K/Pg boundary large igneous province PETM LIP zeolite authigenesis Paleocene-Eocene Thermal Maximum igneous sill intrusion Campanian Oligocene pelagic carbonates paleoceanography African-Southern Ocean Gateway Southern Ocean
Online Access:	https://zenodo.org/record/8277568 https://doi.org/10.5281/zenodo.8277568

Description
Summary:	Inorganic carbon (carbonate) is determined by coulometry, which uses a photodetection cell to measure carbon dioxide evolved during sample acidification. Report includes percent inorganic carbon and calcium carbonate.