IODP Expedition 361 Elemental analysis (CHNS)

• Main Authors: Hall, I.R., Hemming, S.R., LeVay, L.J., Barker, S., Berke, M.A., Brentegani, L., Caley, T., Cartagena-Sierra, A., Charles, C.D., Coenen, J.J., Crespin, J.G., Franzese, A.M., Gruetzner, J., Han, X., Hines, S.K.V., Jimenez-Espejo, F.J., Just, J., Koutsodendris, A., Kubota, K., Lathika, N., Norris, R.D., Pereira dos Santos, T., Robinson, R., Rolinson, J.M., Simon, M.H., Tangunan, D., van der Lubbe, J.J.L., Yamane, M., Zhang, H.
• Format: Dataset
• Language: unknown
• Published: Zenodo 2020
• Subjects: Expedition 361; JOIDES Resolution; South African Climates; Agulhas LGM Density Profile; Site U1474; Site U1475; Site U1476; Site U1477; Site U1478; Ancillary Project Letter APL-845; Climate and Ocean Change; monsoons; AABW Antarctic Bottom Water; AAIW Antarctic Intermediate Water; Agulhas Bank; Agulhas Current; Agulhas leakage; Agulhas Plateau; Agulhas Return Current; Agulhas ring; Agulhas Undercurrent; ASHSW Arabian Sea High Salinity Water; Cape Basin; CDW Circumpolar Deep Water; Davie Ridge; Delagoa Bight; DSTF Dynamical Southern Ocean Subtropical Front; East Madagascar Current; EIOW Equatorial Indian Ocean Water; Indian-Atlantic Ocean gateway; IOW Indian Ocean Water; ITCZ Intertropical Convergence Zone; Limpopo River; Mozambique Channel; Mozambique Undercurrent; NADW North Atlantic Deep Water; Natal Pulses; Natal Valley; RSIW Red Sea Intermediate Water; SAF Subantarctic Front; SICW South Indian Central Water; South Atlantic Ocean; Southeast African margin; Southwest Indian Ocean; STF Subtropical Front; STSW Subtropical Surface Water; TSW Tropical Surface Water; Zambezi River; Antarctic; Indian; Southern Ocean; Antarc*; NADW; North Atlantic Deep Water; North Atlantic
• Online Access: https://dx.doi.org/10.5281/zenodo.3633181; https://zenodo.org/record/3633181

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 detected by thermal conductivity on a FlashEA 1112 CHNS elemental analyzer. Organic carbon can be directly measured on the elemental analyzer by acidification of the sample to drive off carbonate as carbon dioxide before analyzing. Total organic carbon on this report is measured rather than calculated.