Where: Queensland, Australia (18.8° S, 144.9° E: paleocoordinates 18.8° S, 144.8° E)
• coordinate estimated from map
• local area-level geographic resolution
When: Wyandotte Formation, Middle Pleistocene to Middle Pleistocene (0.8 - 0.0 Ma)
• The base of the Wyandotte Formation is beyond the conventional 14C range (>45000 ybp). It is inferred to postdate a 410 ka basalt flow. The rate of downcutting to form the valley is not known, but since 410,000 ybp a substantial valley has been cut. Between 4 to 10 metres of Unit A were deposited prior to unit B, which has a basal date of 30,400 ybp (+750/-700 yrs). It is reasonable to suppose that the erosive phase might easily have taken half of the available interval, a corollary of which is that the base of the Wyandotte Formation may not be much older than 200,000 ybp. The duration of the hiatus between final deposition of Unit A and the onset of Unit B is unknown.
Environment/lithology: "channel"; siliciclastic sediments
Size class: macrofossils
Primary reference: G. C. McNamara. 1990. The Wyandotte Local Fauna: A New, Dated, Pleistocene Vertebrate Fauna from Northern Queensland. Memoirs of the Queensland Museum 28:285-297 [M. Uhen/N. Jones]more details
Purpose of describing collection: paleoecologic analysis
PaleoDB collection 194845: authorized by Matthew Clapham, entered by Matthew Clapham on 01.07.2018
Creative Commons license: CC BY (attribution)
Taxonomic list
Mammalia | |
Dasyurus sp. Geoffroy 1796 quoll | |
Diprotodon optatum Owen 1838 diprotodont marsupial
? Euowenia sp. De Vis 1891 diprotodont marsupial | |
Phascolonus sp. Owen 1872 wombat | |
Reptilia | |
Wonambi cf. naracoortensis Smith 1976 snake |