January 1, 1990Marine Ecology Progress Series197 citationsOpen Access
Anaerobic mineralization in marine sediments from the Baltic Sea-North Sea transition
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Abstract
Mineralization was studied withln the upper 2 m of sediments from the Belt Sea, Kattegat, and Skagerrak at 15 to 200 m water depth. Radiotracer measurements of sulfate reduction rates were related to porewater chemistry (SO,'-, HC03-, P O ~~-, NH4+, H2S, and CH,), to solid-phase chemistry (C, S , N, and Fe), and to bacterial distributions. Sulfate penetrated 0.9 to > 3 . 5 m into the sediment.
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Jørgensen et al. (Mon,) studied this question.