IODP Expedition 379 Elemental analysis (CHNS) ...

• 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
• Format: Dataset
• 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; Antarctic; Amundsen Sea; West Antarctic Ice Sheet; Byrd; Antarc*; Ice Sheet
• Online Access: https://dx.doi.org/10.5281/zenodo.11200275; https://zenodo.org/doi/10.5281/zenodo.11200275

Fundamental elemental component (total carbon, hydrogen, nitrogen, and sulfur) fluctuations help define the origin, depositional environment, and diagenetic alteration of source materials. To determine C, H, N, and S, solid samples are reacted with a catalyst, separated by chromatography, and detect...