Sulfhydrolase Activity in Sediments of Wintergreen Lake, Kalamazoo County, Michigan

Author:

King Gary M.1,Klug Michael J.2

Affiliation:

1. Kellogg Biological Station, Michigan State University, Hickory Corners, Michigan 49060

2. Department of Microbiology and Public Health, Michigan State University, East Lansing, Michigan 48824

Abstract

The hydrolysis of p -nitrophenyl sulfate, p -nitrocatechol sulfate, and [ 35 S]sodium dodecyl sulfate was examined in anoxic sediments of Wintergreen Lake, Michigan. Significant levels of sulfhydrolase activity were observed in littoral, transition, and profundal sediment samples. Rates of sulfate formation suggest that the sulfhydrolase system would represent a major source of sulfate within these sediments. Sulfate formed by ester sulfate hydrolysis can support dissimilatory sulfate reduction as shown by the incorporation of 35 S from labeled sodium dodecyl sulfate into H 2 35 S. Sulfhydrolase activity varied with sediment depth, was greatest in the littoral zone, and was sensitive to the presence of oxygen. Estimations of ester sulfate concentrations in sediments revealed large quantities of ester sulfate (∼30% of total sulfur). Both total sulfur and ester sulfate concentrations varied with the sediment type and were two to three orders of magnitude greater than the inorganic sulfur concentration.

Publisher

American Society for Microbiology

Subject

Ecology,Applied Microbiology and Biotechnology,Food Science,Biotechnology

Reference17 articles.

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3. Arylsulfatase activity in marine sediments;Chandranrohan D.;Mar. Biol.,1974

4. Arylsulfatase activity in northern Nigerian soils;Cooper P. J. M.;Soil Biol. Biochem.,1972

5. Sulfate ester formation and hydrolysis: a potentially important yet often ignored aspect of the sulfur cycle of aerobic soils;Fitzgerald J. W.;Bacteriol. Rev.,1976

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