IODP Expedition 379 Inorganic carbon (coulometer)

• Main Authors: Gohl, Karsten, Wellner, Julia S., Klaus, Adam, Bauersachs, Thorsten, Bohaty, Steven, Courtillat, Margot, Cowan, Ellen A., De Lira Mota, Marcelo A., Esteves, Mariana S.R., Fegyveresi, John M., Frederichs, Thomas, Gao, Liang, Halberstandt, Anna R., Hillenbrand, Claus-Dieter, Horikawa, Keiji, Iwai, Masao, Kim, Ji-Hoon, King, Theresa M., Klages, Johann P., MacCaull, J.G.N., Passchier, Sandra, Penkrot, Michelle, Powell, John L., Prebble, Joseph Graham, Rahaman, Waliur, Reinardy, Benedict T.I., Renaudie, Johan, Robinson, Delaney E., Scherer, Reed P., Siddoway, Christine S., Wu, Li, Yamane, Masako
• Other Authors: International Ocean Discovery Program
• Format: Other/Unknown Material
• Language: unknown
• Published: International Ocean Discovery Program 2021
• Subjects: International Ocean Discovery Program; IODP; JOIDES Resolution; Expedition 379; Site U1532; Site U1533; Amundsen Sea West Antarctic Ice Sheet History; Amundsen Sea Embayment; Pine Island Glacier; Thwaites Glacier; Marie Byrd Land; paleoclimate; paleo-ice sheet; continental rise; sediment drift; contourite; ice-rafted debris; Environmental change; processes; and effects; glacial-interglacial cyclicity; seismic stratigraphy; Amundsen Sea; Antarc*; Antarctic; Ice Sheet
• Online Access: https://doi.org/10.5281/zenodo.11200303

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.