Article ID Journal Published Year Pages File Type
1753192 International Journal of Coal Geology 2013 38 Pages PDF
Abstract
The response of lacustrine faunas to climatic oscillations around the Carboniferous-Permian transition is less prominent than that of plants. The origin of the transition between the local Elonichthys-Sphaerolepis and Acanthodes gracilis bio/ecozones around the Carboniferous/Permian boundary is impossible to deduce from the existing fossil record.
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Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
Preview
Climatic and biotic changes around the Carboniferous/Permian boundary recorded in the continental basins of the Czech Republic
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