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Current studies in the Holy Cross Mts, Central Poland did not confirm an idea of the persistence of stromatoporoid-coral build-ups into the Famennian, i.e. distinctly after Frasnian/Famennian reef extinction event. Stepwise termination of the Frasnian-type biotas was joined with successive sea-level fluctuations interfering with local tectonic activity, but diversified and locally abundant coral-dominated...
The succession of Givetian to Frasnian faunas in the Holy Cross Mts is analysed in context of biotic responses to cyclic depositional events, primarily of eustatic origin. This cyclicity stimulated the succession of brachiopod bottom-level assemblages from stringoce-phalid to ambocoeliid to atrypid (cyrtospiriferid) and to rhynchonellid faunas. This obviously supraregional pattern reflects sequential...
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