By Hart M.B. (Ed.)
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Extra resources for 8th International Symposium on the Cretaceous System, University of Plymouth, September 5-12 2009. Abstracts volume
At the bottom and some unknown species of Hedbergella towards the top. The studied interval belongs possibly to the Upper Bedoulian-Gargasian (Late Early Aptian - Middle Aptian). At the contact between two formations, a brecciated surface with iron oxide is present displaying a mantling epikarstic condition. This implies that before the drowning surface exposure conditions should have occurred. The time gap is hardly determined and hosted a rapid tectonic event. The section is followed up by classical turbidites of Aptian-Albian in age and unconformably overlain by Late Santonian pelagic limestones of the Unaz Formation.
Modern data do not support the platycopid signal, but neither do they disprove it. There is clearly a platycopid signal associated with OAE 2, although its wider application, as well as palaeobiological explanations of cause and effect, require more cautious and critical consideration than has hitherto been exercised. Brandao, S. N. & Home, D. J. (submitted). The Platycopid Signal of oxygen depletion in the ocean: a critical evaluation of the evidence from modern ostracod biology, ecology and depth distribution.
16, Leningrad, Nedra Press, 244-285 [in Russian]. A. G. 1977. New data on the stratigraphy of the Boreal Hauterivian. Geologiia i Geofizika, Siberian Branch, No. 7, Novosibirsk, 75-82 [in Russian]. A. & Kemper, E. 1988. Comparative paleontology and stratigraphy of Valanginian Polyptychitinae and Simbirskitinae in Sverdrup Basin (Arctic Canada) and Lower Saxony Basin (Northwest Germany). Geological Survey of Canada, Bulletin, 377, 335 pp.. V. G. 2003. Atlas of geological monuments of nature of Yaroslavl region.
8th International Symposium on the Cretaceous System, University of Plymouth, September 5-12 2009. Abstracts volume by Hart M.B. (Ed.)