Late Wuchiapingian (Late Dzhulfian,early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon,central–eastern Peloponnesus,Greece) |
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Authors: | Emmanuel Skourtsos Daniel Vachard Alexandra Zambetakis-Lekkas Rossana Martini Louisette Zaninetti |
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Affiliation: | 1. Department of historical geology-palaeontology, national university of Athens, Athens, Greece;2. UFR des sciences de la Terre, Upresa 8014 du CNRS, université des sciences et technologies de Lille, 59655 Villeneuve d''Ascq cedex, France;3. Département de géologie et paléontologie, université de Genève, 13 rue des Mara??chers, 1211 Genève, Switzerland |
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Abstract: | Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931. |
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Keywords: | Permian Wuchiapingian Dzhulfian biostratigraphy foraminifera algae palaeogeography Greece Permien Wuchiapingien biostratigraphie foraminifères paléogéographie Grèce Stratigraphie Stratigraphy |
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