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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
Nevertheless, in the application of modern data to the interpretation of Cretaceous evidence, we must allow that evolution has occurred over the intervening millions of years; how ostracod species behave in the present is not necessarily a reliable key to how their ancestors may have behaved in the past. 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.
J. 2005. Isotopic signals from RhyazanianHauterivian arctic belemnites of the Boyarka River, northern Central Siberia. , Under, P. & Bodin, S. (eds), 7th International Symposium on the Cretaceous, 5-9 September 2005, Neuchatel, Scientific Program and Abstracts, 157-158. A. Ya. 1971. Paleomagnetic zones of Hauterivian Stage (of Khatanga depression deposits). Geology and Geophysics, Novosibirsk, 8, 62-71 [in Russian]. V. ) 2005. Atlas of Early Cretaceous fauna of Georgia. Tbilisi, Poligrafist Press [in Russian].
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. Cyclostratigraphy of the pelagic successions display the rhythmic alternation of black shales/mudstones and sandstones or limestones/marls. At the bottom of the section, black shales/mudstones display thicker beds and sandstones/limestone beds show thickening towards top.
8th International Symposium on the Cretaceous System, University of Plymouth, September 5-12 2009. Abstracts volume by Hart M.B. (Ed.)