Sediments were cored at six sites (49°24′S to 59°36′S) in water depths ranging from 564 to 4082 m. A total of 77 interstitial-water samples was recovered as part of the routine sampling protocol. In addition, a novel, high-resolution pore-water sampling program was tested. Data collected include interstitial-water sodium, potassium, calcium, magnesium, pH, alkalinity, sulfate, ammonia, phosphate, aqueous silica, salinity, chloride, oxidation-reduction potentials, and sediment chemistry. The northern sector (Sites 736 and 737) is characterized by the highest sedimentation rates (up to 140 m/my) and thermal gradients (70°-98°C/km). The southern portion of the Kerguelen Plateau (Sites 738 and 744) records the lowest sedimentation rates (less than 5 m/my) and thermal gradients (43°C/km) of the three study area. -from Authors
CITATION STYLE
Chambers, S. R., & Cranston, R. E. (1991). Interstitial-water geochemistry of Kerguelen Plateau sediments. Proc., Scientific Results, ODP, Leg 119, Kerguelen Plateau-Prydz Bay, 347–374. https://doi.org/10.2973/odp.proc.sr.119.169.1991
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