56. ORGANIC CARBON AND NITROGEN, SEDIMENT COMPOSITION, AND CLAY MINERALOGY OF DEEP SEA DRILLING PROJECT SITE 603, WESTERN ATLANTIC OCEAN1

• Main Authors: K. -c. Emeis, B. Mycke, H. -h. Richnow, A. Spitzy, E. T. Degens
• Other Authors: The Pennsylvania State University CiteSeerX Archives
• Format: Text
• Language: English
• Subjects: North Atlantic
• Online Access: http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.547.5429; http://www.deepseadrilling.org/93/volume/dsdp93_56.pdf

Sediment and interstitial water samples recovered during DSDP Leg 93 at Site 603 (lower continental rise off Cape Hatteras) were analyzed for a series of geochemical facies indicators to elucidate the nature and origin of the sedimenta-ry material. Special emphasis was given to middle Cretaceous organic-matter-rich turbidite sequences of Aptian to Tu-ranian age. Organic carbon content ranges from nil in pelagic claystone samples to 4.2 % (total rock) in middle Cretaceous car-bonaceous mudstones of turbiditic origin. The organic matter is of marine algal origin with significant contributions of terrigenous matter via turbidites. Maturation indices (vitrinite reflectance) reveal that the terrestrial humic material is reworked. Maturity of autochthonous material (i.e., primary vitrinite) falls in the range of 0.3 to 0.6 % ‰ Carbohy-drate, hydrocarbon, and microscopic investigations reveal moderate to high microbial degradation. Unlike deep-basin black shales of the South and North Atlantic, organic-carbon-rich members of the Hatteras Formation lack trace metal enrichment. Dissolved organic carbon (DOC) in interstitial water samples ranges from 34.4 ppm in a sandstone sample to 126.2 ppm in an organic-matter-rich carbonaceous claystone sample. One to two percent of DOC is carbohydrate-carbon.