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- W49787524 abstract "A biological reduction of sulfates is made in the water and muds of the Black Sea. The fractionation of sulfur isotopes in this process was studied. The most extensive range of fractionation of suifur isotopes occurred during the formation of different forms (dipyrite, troilite, organic sulfur, and free sulfur), as a consequence of the reduction of sulfates in a maritime basin in the absence of ventilation by dissolved oxygen. The smallest fractionation effect was observed when the basin is composed of fresh water with ventilation by air. On these bases, it was shown that st run. Concent 8000 years ago, the North Sea was a basin of fresh water. (trauth)" @default.
- W49787524 created "2016-06-24" @default.
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- W49787524 date "1963-01-01" @default.
- W49787524 modified "2023-09-24" @default.
- W49787524 title "FRACTIONATION OF SULFUR ISOTOPES IN THE BLACK SEA AND ITS HISTORY" @default.
- W49787524 hasPublicationYear "1963" @default.
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