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Upper Permian conodonts from Hydra, Greece

Published online by Cambridge University Press:  14 July 2015

Merlynd K. Nestell  and
Bruce R. Wardlaw
Merlynd K. Nestell
Affiliation:
Department of Geology, University of Texas at Arlington, Arlington 76019
Bruce R. Wardlaw
Affiliation:
United States Geological Survey, Washington, D.C. 20560
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Abstract

Conodont faunas recovered from the upper 80 m of Late Permian limestones on the Greek island of Hydra (Idhra) include Neogondolella leveni (Kozur, Mostler, and Pjatakova), Neogondolella orientalis (Barskov and Koroleva), Hindeodus julfensis Sweet, Xaniognathus hydraensis n. sp., and Ellisonia sp. The conodonts occur with a rich assemblage of silicified brachiopods, fusulines, and other invertebrates. Diagnostic fusulines include Reichelina media Miklukho-Maklai and Palaeofusulina cf. P. prisca Deprat. The conodont and fusuline faunas are correlative with well-known faunas described from the lower part of the Ali Bashi Formation of the Djulfa region of Iran, and with similar faunas described from other regions of Central Asia. The presence of conodonts from the Neogondolella orientalis Zone of Kozur indicates that the age of the upper part of the Permian sequence on Hydra is early-middle Dzhulfian (Baisalian Substage).

Type
Research Article
Information
Journal of Paleontology , Volume 61 , Issue 4 , July 1987 , pp. 758 - 772
Copyright
Copyright © The Paleontological Society 

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