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- W2247364550 abstract "Measurements of stables sulfur isotope ratios are used to explain some biogeochemical problems in nature. Laboratory experiments with bacteria included: bacterial sulfate reduction, bacterial chemosyntheticr oxidation of sulfur and hydrogen sulfide, bacterial photosynthetic oxidation of sulfide. and an artificial sulfur spring. Results obtained from these expertments were used to interpret measurements made on natural environments from which sulfur compounds could be isolated and the scology of whirh was studied previously. The environments investigated were the Cyrenaican Lakes. North Africa; the sulfur nodules of Lake Eyrs, South Australia; sulfur from Kona. Masulipatam, east coast of India; a natural sulfur spring at Waipara, North Canterbury. New Zealand; the sulfur cycle in some Australian sewage phodents; and mud and sea water from Milford Sound (a fjord), New Zealand. Bacterial sulfate reduction and chemosynthetic oxidation of sulfides gave enrichment in the lighter isotope (S/ sup 32/) in laboratory experiments. Preliminary work with other bacterial steps in the cycle did not show any conclusive pattern of isotope fractionation. Measurements of naturelly occurring deposits gave conflicting results. In some cases (e.g.. Milford round) the explanation of the S/sup 32/ S/sup 34/ ratios was relatively straight-forward; in others, no explanation could be offered for the apparently anomalousmore » results. (auth)« less" @default.
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- W2247364550 date "1960-06-01" @default.
- W2247364550 modified "2023-09-23" @default.
- W2247364550 title "SULPHUR ISOTOPIC VARIATIONS IN NATURE. PART 8. APPLICATION TO SOME BIOGEOCHEMICAL PROBLEMS" @default.
- W2247364550 hasPublicationYear "1960" @default.
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