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Title

Late Wuchiapingian (Late Dzhulfian, early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon, central–eastern Peloponnesus, Greece)

Authors
Skourtsos, Emmanuel
Vachard, Daniel
Zambetakis-Lekkas, Alexandra
Published in Comptes rendus géoscience. 2002, vol. 334, no. 12, p. 925-931
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.
Keywords PermianWuchiapingianDzhulfianbiostratigraphyforaminiferaalgaepalaeogeographyGreeceAuthor Keywords: PermienWuchiapingienbiostratigraphieforaminifèrespaléogéographieGrèce
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Structures
Research group Sedimentology, Biostratigraphy and Micropaleontology
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SKOURTSOS, Emmanuel et al. Late Wuchiapingian (Late Dzhulfian, early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon, central–eastern Peloponnesus, Greece). In: Comptes rendus géoscience, 2002, vol. 334, n° 12, p. 925-931. https://archive-ouverte.unige.ch/unige:4405

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Deposited on : 2009-11-30

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