Fig. 3From: New data on the biostratigraphy (charophytes, nannofossils, mammals) and lithostratigraphy of the Late Eocene to Early Late Miocene deposits in the Swiss Molasse Basin and Jura Mountainsa Oberdorf section above the railway station and along the road to the Weissenstein (survey 2014 by P.-O. Mojon, amended and redrawn from fig. 13 of Rollier 1910). Bolustone: reddish-grey calcareous clays with iron pisolites (Bohnerz). 1: Yellowish ferruginous lacustrine limestone and some thin marly layers with charophytes (Oberdorf Süsswasserkalk). 2: Red-brown clays with iron pisolites (Bräunlichrote Bolustone, z.T. mit Bohnerz). 3: Grey clayey marls. 4–5: Lower calcareous marl and greenish-grey marls with pisolites. 6: Dysodile: thin laminated calcareous layer with fossil fishes and ostracods. 7–8: Lower thin calcareous layers and blue-grey marls. 9: Whitish lacustrine limestones with charophytes and gastropods (Hydrobiidae). 10: Blue-grey marls. 11: Grey limestone. 12: Greenish-grey marls. 13: Lacustrine limestones and marly layers, upper part with lignitic interbeds (14) containing compressed lacustrine and terrestrial gastropods (Planorbidae, Lymnaeidae, Helicidae). 15: Sandy marls. 16: Moraine of the last glaciation with alpine blocks and topsoil. b Log of the Del 1/Rossemaison borehole (survey 1990 by M. Weidmann, detailed description in the text).Back to article page