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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.
International Ocean Discovery Program, Guaymas Basin Tectonics and Biosphere, alteration, Expedition 385, heat flow, IODP, JOIDES Resolution, Site U1545, Site U1546, carbon budget, Site U1549, Site U1547, Gulf of California, Site U1548, deep biosphere, Ringvent, sill emplacement, Site U1552, hydrothermal alteration, Site U1550, Site U1551
International Ocean Discovery Program, Guaymas Basin Tectonics and Biosphere, alteration, Expedition 385, heat flow, IODP, JOIDES Resolution, Site U1545, Site U1546, carbon budget, Site U1549, Site U1547, Gulf of California, Site U1548, deep biosphere, Ringvent, sill emplacement, Site U1552, hydrothermal alteration, Site U1550, Site U1551
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