New Quarry dinosaur tracksite (QM) (Cretaceous of Australia)

Also known as Winton

Where: Queensland, Australia (23.1° S, 142.8° E: paleocoordinates 52.8° S, 132.7° E)

• coordinate estimated from map

• outcrop-level geographic resolution

When: Winton Formation (Rolling Downs Group), Cenomanian (100.5 - 93.9 Ma)

• "about the same stratigraphic level as Lark Quarry" with two track-bearing layers.

• group of beds-level stratigraphic resolution

Environment/lithology: lacustrine; poorly lithified, red sandstone and lithified, red claystone

• lacustrine origin. "Sandstones above and below the footprint bed probably resulted from periodic sheet-floods...Shrinkage of the lake had exposed extensive mud-flats marked with narrow run-off channels.". Supposedly a "much-trampled watering-place."
• "Sediments exposed at Lark Quarry are mainly soft and fine-grained arkosic sandstones of reddish-buff colour. The sandstones for thick beds (each built of innumerable small sets of cross-bedding) and are interlayered with thin and persistent seams of indurated pinkish claystone. The dinosaur tracks are impressed in an 8-10 cm seam of finely laminated claystone that is evidently of lacustrine origin...There are no ripple-marks, rain-prints or sun-cracks, and the dinosaur tracks were impressed in firm moist mud."

Size class: macrofossils

Preservation: mold/impression, trace

Collected in 1978

Collection methods: surface (in situ), mechanical,

Primary reference: M. Wade. 1979. Tracking dinosaurs: the WInton excavation. Australian Natural History 19(9):286-291 [M. Carrano/M. Carrano]more details

Purpose of describing collection: paleoecologic analysis

PaleoDB collection 185501: authorized by Matthew Carrano, entered by Matthew Carrano on 25.04.2017

Creative Commons license: CC BY (attribution)

Taxonomic list

Show authors, comments, and common names
Reptilia
 Avetheropoda -
Carnosauria indet.
 Theropoda -
Coelurosauria indet.