Composition of interstitial waters and forms of sulfur compounds in bottom sediments in the northeastern Black Sea

Author:

Rozanov A. G.,Kokryatskaya N. M.,Gurskii Yu. N.

Publisher

Pleiades Publishing Ltd

Subject

Economic Geology,Geochemistry and Petrology

Reference31 articles.

1. Berlin, Yu.M., Bol’shakov, A.M, Verkhovskaya, Z.I., et al., Methane in bottom sediments in the prodelta of the Danube and Kyzyl Irmak rivers, in Litologiya i geokhimiya osadkoobrazovaniya v priust’evykh raionakh zapadnoi chasti Chernogo morya (Lithology and Geochemistry of Sedimentation at Estuaries of the Western Black Sea), Moscow: Inst. Okeanol. RAN, 1987, pp. 116–125.

2. Degens, E. and Ross, D., The Black Sea–Geology, Chemistry and Biology, Tulsa: Am. Ass. Petrol. Geol., 1974, p. 633.

3. Gurskii, Yu.N., Geokhimiya litogidrosfery vnutreenikh morei (Geochemistry of Lithohydrosphere in Internal Seas), Moscow: GEOS, 2003, vol. 1.

4. Gurskii, Yu.N., Rozanov, A.G., and Gudkova, E.A., Behavior of chemical elements in sediments of the Black Sea south of the Kerch Peninsula, in Materialy XIX Mezhdunarodnoi nauchnoi konferentsii po morskoi geologii, Geologiya Morei i okeanov (Materials of the 19th Int. Scientific Conference on Marine Geology: Geology of Seas and Oceans), 2011, vol. 4, pp. 28–32.

5. Jorgensen, B., Buttcher, M., Luschen, H., et al., Anaerobic methane oxidation and a deep H2S sink generate heavy sulphides in black sea sediments, Geochim. Cosmochim. Acta, 2004, vol. 68, no. 9, pp. 2095–2098.

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