Abstract | The tetrapod tracks from Winterswijk receive global attention for their abundance and preservation quality, including long trackways and skin- and claw impressions. The footprint association is consistent with a Middle Triassic age. It includes four ichnotaxa: Brachychirotherium paraparvum, Rhynchosauroides peabodyi, Procolophonichnium haarmuehlensis and Coelurosaurichnus ratumensis. Their terrestrial producers probably include: archosauriforms, archosauromorphs/lepidosauromophs and both small and large therocephalian therapsids, respectively. These groups are almost completely unknown from the fossil (bone) record of the Vossenveld Formation, which includes mostly aquatic life-forms. The occurrence of vertebrate swimming traces and invertebrate tracks and burrows indicates a marginal marine palaeoenvironment, subject to frequent flooding and rapid drying (tidal fl at).

Staringia

CC BY 3.0 NL ("Naamsvermelding")

Nederlandse Geologische Vereniging

Lorenzo Marchetti, Hans van der Donck, Menko van Hylckama Vlieg, & Melanie A.D. During. (2019). Leaving only trace fossils - the unknown visitors of Winterswijk. Staringia, 16(1), 250–257.