Abstract
The newly rediscovered specimen ofEopelobates from the uppermost Oligocene brown coal measures near Bonn, Germany, deposited since the last century in the collections of the Institut und Museum fur Geologie und Palaontologie der Universitat Tubingen, most probably belongs toE. anthracinus. Its small but fully ossified skeleton suggests that it is reasonable to keep the speciesE. anthracinus separate fromE. bayeri, although both species are closely related.
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