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Abstract: This paper presents biostratigraphical and palaeogeographical correlations, in a
post-Hercynian and pre-Cimmerian tectonic framework, between stratigraphic sections of
Late Permian age in two important and remote areas, with some considerations concerning
neighbouring countries. It concerns mainly the Nikitin sequence (Kuban, Russia) and
the Bfikk Mountains (Hungary), and describes the carbonate environments, microfauna
diversity, foraminiferal assemblages, calcisponge and brachiopod constructions, and
gymnocodiacean accumulations. This study is extended to former Transcaucasia (southern
Armenia, Georgia and Adzerbadjan), the Alborz Belt in northern Iran, Italy and the Carnic
Alps. It emphasizes a relatively simple biosedimentary evolution, which permits a confident
palaeogeographic reconstruction. New geochemical results provided some additional markers,
in particular small microspherules consisting of Cr/Ni spinels of cosmic

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