Abstract

The bats from the karstic fissure fill sites Petersbuch 6, 10, 18, 31, 35 and 48 include 14 species, four of which are new. All samples are numerically dominated by rhinolophids, especially by Rhinolophus delphinensis. The rich samples from Petersbuch 6-18 are striking in their high species diversity (seven species each). Myotis bavaricus nov. sp. is characterised by a series of plesiomorphous characters, while Myotis reductus nov. sp. is more derived. A special trait of Submyotodon petersbuchensis nov. gen. nov. sp. is the coexistence of nyctalodont and (sub-) myotodont molars in one dentary. Miniopterus rummeli nov. sp. is characterised by its large size, a high coronoid process and its widely spaced lower premolars. Composition and origin of the chiropteran faunas are discussed. They are interpreted as an accumulation of bats that perished in the cave or rock crevice and to a negligible extent as remains of owl pellets. The stratigraphic correlation of the faunas, based on rodents, is late Middle Miocene (MN 7/8). This study is based on several thousand specimens.

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