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Abstract

The Telbesmi Formation, at the northern margin of the Arabian Plate, Turkey, is composed of alternating darkbrown,

pinky-brown fluvial arkosic sandstone/mudstones with thin-bedded cherty limestones and channel

conglomerates. The formation contains rare and poorly diversified trace fossils. The siltstone/sandstone beds of

levels 1 and 2 of the formation yielded, however, a moderately diverse assemblage composed of: Cochlichnus

isp., Palaeophycus isp., Planolites beverleyensis, Teichichnus isp. and ?Treptichnus rectangularis. This assemblage,

made up of traces left by deposit feeding organisms, represents the Scoyenia ichnofacies. Treptichnus

rectangularis and Palaeophycus isp., of the assemblage, can be considered markers for the base of the Cambrian

in southeast Turkey.

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Authors and Affiliations

Huriye Demírcan
Semih Gürsu
M. Cemal Göncüoğlu

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