IODP Expedition 379 Magnetic susceptibility (point or contact system) ...

• 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.11200411; https://zenodo.org/doi/10.5281/zenodo.11200411

Magnetic susceptibility was measured on section halves on the Section Half Multisensor Logger (SHMSL) using a Bartington MS2 meter and either a MS2E or MS2K probe. Because all JRSO cores meet minimum size requirements for these two probes, MSPOINT data are corrected for volume and recorded in SI sus...