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Late Mesozoic bivalve faunas from the Tetori Group,Japan
Institution:1. Museo Argentino de Ciencias Naturales B. Rivadavia, A. Gallardo 470, C1405DJR Buenos Aires, Argentina;2. Facultad de Ciencias, Departamento de Evolución de Cuencas, Universidad de la República, Iguá 4225, 11400 Montevideo, Uruguay;1. CICTERRA, CONICET, Universidad Nacional de Córdoba, Av. Vélez Sarsfield 1611, Ciudad Universitaria, X5016GCA Córdoba, Argentina;2. CIPAL, Facultad de Ciencias Exactas Físicas y Naturales, Universidad Nacional de Córdoba, Av. Vélez Sarsfield 299, 5000 Córdoba, Argentina;3. CONICET, Universidad Nacional de La Rioja, Av. Luis M. de la Fuente s/n, La Rioja 5300, Argentina
Abstract:The Tetori Group of Japan ranks amongst the more important Upper Mesozoic strata in East Asia, with common animal and plant fossils throughout and is well suited for analyses of the links between environmental changes and the various animal and plant fossil assemblages. Three marine transgressions (i. e., Bathonian–Oxfordian, Tithonian–Berriasian and Hauterivian–Barremian in age) have been recognized in the Tetori Group, based on ammonite index taxa. These pulses are also reflected in bivalve faunas which comprise, 81 species in 65 genera (marine taxa) and 16 species in 13 genera (non-marine taxa). Many of these are considered as endemic species to the Tetori Group. In view of the fact that the occurrence of non-marine taxa was primarily controlled by environmental conditions, these do not constitute chronological indices. The faunal composition of the first marine transgressive phase is similar to that found elsewhere in southeast Asia, while that of the second one resembles both that of southeast Asia and of northeast China and Far East Russia. Assemblages of the third phase are similar to those of Heilongjiang, northeast China. Currents from the equator and high-latitudes explain these similarities.
Keywords:Marine  brackish and freshwater bivalves  Assemblages  Paleoecology  Paleobiogeography
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