The Permian (Autunian) Sotres Formation is a sequence of volcanoclastics and coal-bearing shales overlain by thinly-laminated limestone. Microfacies study indicates sponge-bacterial bafflestones with Bevocastria and ostracods. Absence of marine microfauna/microflora suggests a lacustrine environment. Geodes and cavities are criss-crossed by coelobiont veils formed by Palaeomicrocodium and bacterial bands.
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