PALEO OCEANOGRAPHIC AND GEOCHEMICAL SEDIMENTARY ENVIRONMENTS OF UPPER VENDIAN BLACK SHALE PHOSPHORITE-BEARING DEPOSITS OF THE SOUTH-WESTERN MARGIN EAST-EUROPEAN PLATFORM

 On the base of analysis of materials on geological paleooceanography of the World Ocean and factual data on ancient sedimentogenesis of "early Paleo-Tethys" for the first time the depositional environments of black shale phosphorite-bearing formation of Vendian (Kalus beds) of the Volyno-...

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Bibliographic Details
Date:2012
Main Authors: SENKOVSKY, Yu. M., PALIY, V. M., RADKOVEC, N. Ya., KOLTUN, Yu. V.
Format: Article
Language:Ukrainian
Published: Institute of Geological Sciences, NAS of Ukraine 2012
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Online Access:http://geojournal.igs-nas.org.ua/article/view/139127
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Journal Title:Geological journal

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Geological journal
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Summary: On the base of analysis of materials on geological paleooceanography of the World Ocean and factual data on ancient sedimentogenesis of "early Paleo-Tethys" for the first time the depositional environments of black shale phosphorite-bearing formation of Vendian (Kalus beds) of the Volyno-Podilian monocline and adjacent regions were reconstructed. Process of phosphorogenesis of black shale deposits was genetically interrelated with sedimentation of primary producer of organic matter: plant detritus, phyto- and, possibly, zooplankton, caused by the influence of coastal upwelling, as a result of geochemical activity of biogenic triad P - С - N as a result of coastal upwellig. Deposition of these carbon-bearing deposits occurred in anoxic environment. The Late Vendian oceanic anoxic event has been indexed by the authors as "OAEV".