Organic carbon, calcium carbonate and carbon/nitrogen ratio at DSDP Leg 93 sites

• Main Author: Meyers, Philip A
• Format: Dataset
• Language: English
• Published: PANGAEA 1987
• Subjects: 93-603; 93-603B; 93-603C; 93-604; 93-605; Calcium carbonate; Carbon; organic; total; Carbon/Nitrogen ratio; Carbonate bomb (Müller & Gastner; 1971); Deep Sea Drilling Project; DEPTH; sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analyzer CHN (Hewlett-Packard 185-B); Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg93; Longitude of event; North Atlantic; North Atlantic/CONT RISE; Sample code/label
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.789398; https://doi.org/10.1594/PANGAEA.789398

A large number of samples of nonlithified and lithified sediments from Leg 93 sites were analyzed for their contents of organic carbon and calcium carbonate. An average of two samples was selected from every core for carbonate determination; organic carbon was measured in most of these samples. Nearly all of these analyses were performed on board Glomar Challenger for samples from Sites 603 and 604. Site 605 samples, plus some of the deeper samples from Hole 603B, were analyzed at the University of Michigan. The procedures used in both cases were virtually the same, and their results compared well. Organic carbon analyses were done using a Hewlett- Packard 185-B CHN Analyzer. Portions of samples selected for calcium carbonate determinations were treated with dilute HC1 to remove carbonate, washed with deionized water, and dried at 110°C. A Cahn Electrobalance was used to weight 20-mg samples of sediment for CHN analysis. Samples were combusted at 1050°C in the presence of an oxidant, and the volumes of the evolved gases determined as measures of the C, H, and N contents of sediment organic matter. Areas of gas peaks were determined and compared to those of rock standards of known carbon and nitrogen contents. These values were used to standardize instrument response so that C/N atomic ratios could be reported. Organic carbon concentrations were calculated on the basis of sediment dry weight. Hydrogen elemental analysis with the procedure used is untrustworthy because of the variable amounts of clay minerals and their hydrates, hence hydrogen values are not reported for samples analyzed by this method.