Sulfides of Bottom Sediments in the Northeastern Part of the Black Sea


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A study of bottom sediments conducted on the 100th cruise of R/V Professor Shtokman in the northeastern part of the Black Sea along the section from the Kerch Strait to the deep-sea depression allowed estimation of Holocene sulfide sedimentation and consideration of the accompanying diagenetic processes, which involve reactions with C, N, and P. The behavior of dissolved forms of Mn and Fe is considered from the viewpoint of their different solubility and formation of sulfides. The redox system of the Black Sea sediments can significantly be expanded at the expense of the migration methane and hydrogen, which accompanies its anaerobic oxidation.

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A. Rozanov

Shirshov Institute of Oceanology

编辑信件的主要联系方式.
Email: rozanov@ocean.ru
俄罗斯联邦, Moscow, 117997

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