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Additional resources for 8th International Symposium on the Cretaceous System, University of Plymouth, September 5-12 2009. Abstracts volume
In Sierra San Jose section (SSJ), small variations are observed in the CaC03 contents in the CLC, TS, CLP and CLE members whereas large variations are observed in the LC member. In Cerro El Caloso Pitaycachi section (CECP), both Canova and El Caloso members show least variations in C a C 0 3 contents. Large variations in S i 0 2 contents are observed in CP and SSJ sections whereas least variations are observed in the CECP section. 40 ppm). In PAAS normalized REE+Y patterns, the limestones from LC, CLP, CLE, Canova and El Caloso members show low contents of detrital materials which exhibits seawater-like REE+Y patterns whereas CLC, TS and MQ members show non-seawater-like REE+Y patterns.
2008. Stratigraphy and Boreal-Tethyan correlation of marine Upper Hauterivian of Russia and CIS. A. N. (eds), Cretaceous System of Russia and adjacent countries: problems of stratigraphy and paleogeography. Proceedings of the Fourth All-Russian meeting, Novosibirsk, September 19-23, 2008. Novosibirsk: Publishing House SB RAS, 28-31 [in Russian]. Yu. B. 2006. Yatriya (Pripoliarnyi Ural). [The new data on the stratigraphy of tie boundary deposits of Valanginian and Hauterivian of Yatria River (Subpolar Urals)].
Marine Micropaleontology, 14, 153-235. Pop, G. 1994. Calpionellid evolutive events and their use in biostratigraphy. Romanian Journal of Stratigraphy, 76, 7-24. Rehakova, D. & Michalik, J. 1997. Evolution and distribution of calpionellids- the most characteristic constituents of Lower Cretaceous Tethyan microplankton. Cretaceous Research, 18, 493-504 Remane, J. 1986. Calpionellids and the Jurassic-Cretaceous boundary. Acta Geologica Hungarica, 29, 15-26. A. A. L. B. 1 2 Geological Institute, Russian Academy of Sciences, 7 Pyzhevskii Lane, 11'9017 Moscow, Russia Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, Koptyugav.