Literature DB >> 34178452

A diverse Late Cretaceous vertebrate tracksite from the Winton Formation of Queensland, Australia.

Stephen F Poropat1,2, Matt A White1,3, Tim Ziegler4, Adele H Pentland1,2, Samantha L Rigby1,2, Ruairidh J Duncan2, Trish Sloan1, David A Elliott1.   

Abstract

The Upper Cretaceous 'upper' Winton Formation of Queensland, Australia is world famous for hosting Dinosaur Stampede National Monument at Lark Quarry Conservation Park, a somewhat controversial tracksite that preserves thousands of tridactyl dinosaur tracks attributed to ornithopods and theropods. Herein, we describe the Snake Creek Tracksite, a new vertebrate ichnoassemblage from the 'upper' Winton Formation, originally situated on Karoola Station but now relocated to the Australian Age of Dinosaurs Museum of Natural History. This site preserves the first sauropod tracks reported from eastern Australia, a small number of theropod and ornithopod tracks, the first fossilised crocodyliform and ?turtle tracks reported from Australia, and possible lungfish and actinopterygian feeding traces. The sauropod trackways are wide-gauge, with manus tracks bearing an ungual impression on digit I, and anteriorly tapered pes tracks with straight or concave forward posterior margins. These tracks support the hypothesis that at least one sauropod taxon from the 'upper' Winton Formation retained a pollex claw (previously hypothesised for Diamantinasaurus matildae based on body fossils). Many of the crocodyliform trackways indicate underwater walking. The Snake Creek Tracksite reconciles the sauropod-, crocodyliform-, turtle-, and lungfish-dominated body fossil record of the 'upper' Winton Formation with its heretofore ornithopod- and theropod-dominated ichnofossil record.
© 2021 Poropat et al.

Entities:  

Keywords:  Actinopterygii; Crocodyliformes; Dinosauria; Dipnoi; Ichnology; Ornithopoda; Sauropoda; Swim tracks; Testudines; Theropoda

Year:  2021        PMID: 34178452      PMCID: PMC8216175          DOI: 10.7717/peerj.11544

Source DB:  PubMed          Journal:  PeerJ        ISSN: 2167-8359            Impact factor:   2.984


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