Also known as Winton

Where: Queensland, Australia (22.3° S, 143.1° E: paleocoordinates 51.8° S, 134.1° E)

• coordinate based on nearby landmark

• small collection-level geographic resolution

When: Winton Formation, Cenomanian to Cenomanian (100.5 - 89.3 Ma)

• Tucker et al. 2013 and Tucker et al. 2016 detrital zircon analysis suggest a maximum depositional age of 94–92Ma for the Winton Formation. The underlying upper Mackunda Formation had a maximum depositional age of 104–102Ma, suggesting that the base of the Winton Formation could be no older than Latest Albian.

• bed-level stratigraphic resolution

Environment/lithology: "floodplain"; concretionary siltstone

Size class: macrofossils

Preservation: concretion

Collected by D. Elliot in 2005, 2006, 2013

Collection methods: quarrying, surface (float), surface (in situ), mechanical,

Primary reference: S. F. Poropat, P. D. Mannion, P. Upchurch, S. A. Hocknull, B. P. Kear, M. Kundrát, T. R. Tischler, T. Sloan, G. H. K. Sinapius, J. A. Elliott, and D. A. Elliott. 2016. New Australian sauropods shed light on Cretaceous dinosaur palaeobiogeography. Scientific Reports 6:34467:1-12 [P. Mannion/P. Mannion]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 153781: authorized by Philip Mannion, entered by Philip Mannion on 14.01.2014, edited by Graeme Lloyd and Matthew Carrano

Creative Commons license: CC BY (attribution)