For the first time, rather well-preserved holothurian selerites from epimetamorphic, strongly tectonized Triassic rock sequences are reported. Nine new specles and subspecies are described. The stratigraphy and tectonics of the regions in which the holothurian-bearing rocks occur, are briefly discussed. Attention is drawn to the fact that Triassic microfauna may be very valuable for establishing detailed stratigraphies, even in epimetamorphie rock sequences.
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