IODP Expedition 392 Magnetic susceptibility (point or contact system)

• 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/8277774; https://doi.org/10.5281/zenodo.8277774

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 susceptibility units (x10-5).