Ophiuroids from the Muschelkalk sediments of the eastern part of the Germanic Basin (Poland) have been recorded few times (Piotrowski and Liszkowski, 1981; Radwański, 2002; Salamon et al., 2003). All ophuiroid specimens come from a thin layer of organodetrital limestone located within the Ceratites Beds (2 metres below the Muschelkalk/Keuper boundary)
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