• "The sequence containing vertebrate remains constitutes a 36 m thick coarsening-upwards unit. The lower 13 m consists of poorly consolidated mudstones with minor silty interbeds. Occasional vague moulds after decalcified bivalves are seen in the mudstones. Thin sideritic beds are often associated with well-rounded bone fragments. ... The overlying 16 m of the section forms a coarsening-upwards sequence with a gradually increasing component of thin silt- and sandstone interbeds showing well-developed lenticular and wavy bedding. Sideritic beds contain vertebrate remains, and bones fill the bases of small erosive washout structures. One sandy bed contains a sideritic concretion which encapsules the reptile skeleton .... This coarsening-upwards sequence culminates in a 2 m thick massive sandstone which is overlain by thin siltstones and mudstones. These fine rapidly upwards into mudstones characterised by non-marine palynomorphs."