Abstract
At Site 618 in Orca Basin, the DOC content of the interstitial water peaks in the hypersaline sulfate reduction zone. The sugar content reaches a maximum and the DOC content begins to decrease at the depth of methane gas generation. Below that depth, the sugar and DOC contents are about constant. At Site 619 in Pigmy Basin, the DOC content increases slightly with depth in the sulfate reduction and the methane fermentation zones. The sugar content is lower in the sulfate reduction zone than in the methane fermentation zone; sugar concentration increases and fluctuates with methane gas percentages within the methane fermentation zone. At Site 623 in the lower fan region of the Mississippi Fan, there is no sulfate reduction zone. The DOC and sugar contents of the interstitial water are almost constant with depth. -from Authors
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CITATION STYLE
Ishizuka, T., Ittekkot, V., Degens, E. T., & Kawahata, H. (1986). Preliminary data on dissolved organic carbon and sugar in interstitial water from the Mississippi Fan and Orca and Pigmy basins, Deep Sea Drilling Project Leg 96. Initial Reports DSDP, Leg 96, Ft. Lauderdale to Galveston, Texas, 1983, 729–732. https://doi.org/10.2973/dsdp.proc.96.143.1986
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