Abstract
Abstract Two cores drilled through late Wenlockian rocks in the Ostra Odarslov area of Skane are described. They consist of grey shale intercalated with yellowishgrey laminae and thin beds of dark, dense, silicified limestone. There are also thin beds of dense, non-stratified, silicified shale. The shale contains a meagre fauna, consisting mainly of poorly preserved graptolites. Core No. 1 is characterized by Pristiograptus dubius (Suess) and Gothograptus nassa (Holm). No other determinable graptolites have been found. The fauna is considered to be an equivalent to the nassa/dubius Interregnum of Jaeger (1959), belonging to the uppermost Wenlock. In core No. 2, P. dubius predominates. Monograptus cf. flemingii (Salter) and M. testis cf. inornatus Elles occur sparsely. Cyrtograptus lundgreni Tullberg is relatively common, and a fragmentary specimen of C. radians Tornquist has been found. Some species of inarticulate brachiopods, Cardiola interrupta (Sowerby), two specimens of hyolithids and some flattened ...
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