Composition of sedimentary rocks from the Mountainous Crimea and the Northwestern Caucasus

DOI

Detailed data obtained on chemistry of sedimentary rocks from the Mountainous Crimea and the Northwestern Caucasus that were dated at the Cenomanian/Turonian boundary and formed during Oceanic Anoxic Event 2 make it possible to calculate dissolved oxygen concentration in bottom waters of the sedimentation basin. Enrichment factors of trace elements in black shales are revised and an explanation is suggested for genesis of the rocks with regard for unusual climatic changes.

Supplement to: Levitan, Mikhail A; Alekseev, A S; Badulina, N V; Girin, Yury P; Kopaevich, L F; Kubrakova, I V; Tyutyunnik, O A; Chudetsky, MYu (2010): Geochemistry of Cenomanian/Turonian boundary sediments in the mountainous part of Crimea and the Northwestern Caucasus. Translated from Geokhimiya, 2010, 48(6), 570-591, Geochemistry International, 48(6), 534-554

Identifier
DOI https://doi.org/10.1594/PANGAEA.809736
Related Identifier https://doi.org/10.1134/S0016702910060029
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.809736
Provenance
Creator Levitan, Mikhail A; Alekseev, A S; Badulina, N V; Girin, Yury P; Kopaevich, L F; Kubrakova, I V; Tyutyunnik, O A; Chudetsky, MYu
Publisher PANGAEA
Publication Year 2010
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 4 datasets
Discipline Earth System Research
Spatial Coverage (33.750W, 44.370S, 38.860E, 44.880N)