Abstract
The paper presents biostratinomicalcharacteristics of the Cenomanian and the Turonian fossilcomplexes found in theMiddle Turonian phosphorite horizon from the Senomanskaya Stenka section (Volgograd region, Zhirnovsk district) constituting the basis of the benthic colonies and nekton communities. Probable interpretations for the settings contributory to generation of the phosphorite inclusion clusters are provided.
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