Arthropod trackways and their preservational variants from the Bagh Formation (Upper Cretaceous), India

Tidal siliciclastic deposits of the Turonian Nimar Sandstone (Bagh Formation), India, contain several arthropod trackways which have been ascribed to different ichnogenera by Chiplonkar and Badve (1970). Examination their type material along with additional from same allows a revision these ichnotaxa. As result, Oniscoidichnus communis Badve, 1970 is retained, ampla 1970, O. elegans robustus Dreginozoum orientale Nereites malwaensis Arthropodichnus indicus Tasmanadia sp. indet., Permichnium bosei are treated as its subjective synonyms. Their morphological differences variants trace fossils, transitions between them, resulted minor changes in behavior tracemaker, substrate properties preservation. The features point tracemaker having segmented locomotion appendages, carapace, short abdomen, was probably an isopod. Supposedly, produced associated Rusophycus ispp. A, B, cf. C, D chevron traces E. Diplopodomorpha cretaceca maintained separate ichnogenus ichnospecies being trackway unknown arthropod.