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Geological Magazine; September 2000; v. 137; no. 5; p. 555-582
© 2000 Cambridge University Press (CUP)
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Article

Lower Palaeozoic stratigraphy and palaeontology, Karadere–Zirze area, Pontus Mountains, northern Turkey

W. T. DEAN*, O. MONOD{dagger}, R. B. RICKARDS{ddagger}, OSMAN DEMIR§ and P. BULTYNCK

* Department of Earth Sciences, University of Wales, Cardiff CF1 3YE, UK; and Department of Geology, National Museum of Wales, Cathays Park, Cardiff CF1 3NP, UK
{dagger} Laboratoire de Géologie Structurale, UMR-CNRS 6530, Université d’Orléans, B.P.6759, 45067 Orléans Cedex 2, France
{ddagger} Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK
§ Turkish Petroleum Corporation, 06520 Ankara, Turkey
Département de Paléontologie, Institut royal des Sciences naturelles de Belgique, Rue Vautier 29, B-1040 Brussels, Belgium

Lower Palaeozoic rocks in the Karadere-Zirze area, east of Safranbolu (Pontides, northern Turkey), range from Early Ordovician to Silurian. Overlying the probably Tremadoc Bakacak Formation are Aydos Formation quartzites, followed conformably by the Karadere Formation, dated as Early Arenig to Early Llanvirn by means of graptolites which are assigned to seventeen genera and include three new forms: Eoglyptograptus bouceki, Prolasiograptus haplus praecursor and Undulograptus? mui. Late Arenig trilobites from the Karadere Formation include Bergamia, Cyclopyge, Dionidella?, Leioshumardia and Seleneceme. In the Limestone Member of the overlying Ketencikdere Formation, uncommon trilobites suggest only a mid- to late Ordovician age, but con-odonts with Colour Alteration Index 5–6 indicate the Amorphognathus tvaerensis Biozone (early Caradoc). Macrofossils are rare in the Siltstone Member, but conodonts from the middle of the unit suggest the highest subzone of the A. tvaerensis Biozone; the youngest visible strata are, on acritarch evidence, at least as high as Caradoc, but the Ashgill is not confirmed and the contact with overlying Silurian rocks is unexposed. The Findikli Formation comprises: a Lower Member, black argillites with Llandovery graptolites and acritarchs; and an Upper Member, grey shales with late Wenlock graptolites, overlain unconformably by Devonian rocks. The succession differs significantly from contemporaneous deposits in southern Turkey and its affinities lie with western Europe, including the Welsh Basin.




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