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in the eastern part of the Swabian Alb (SW Germany), close to the town of Heidenheim an der Brenz (Fig.1). It has a diameter of c. 3.5 kilometres and is characterised by a remarkable uplift (“Zentralhügel”) in its centre. In the surroundings of the Steinheim Basin, Upper Jurassic (Kimmeridgian) limestones crop out, whereas in the central uplift, Middle Jurassic clays and ferruginous sandstones occur. Originally interpreted as a cryptovolcanic structure, the Steinheim Basin is today recognised as a meteoritic impact crater. This is confirmed by drillings, planar elements in quartzes from Middle Jurassic sandstones

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Revision of the plant assemblage of Steinheim am Albuch (Baden- W&amp;uuml;rttemberg, Germany, middle Miocene, reference locality of Mammal Neogene Zone MN 7)