Where: New South Wales, Australia (33.0° S, 151.7° E: paleocoordinates 66.5° S, 144.4° E)
• coordinate estimated from map
• small collection-level geographic resolution
When: Belmont Conglomerate Member (Croudace Bay Formation), Changhsingian (254.2 - 252.2 Ma)
• Insect bed is 30 cm thick, but insects concentrated approximately 2 cm below top. From horizon 70 feet below base of Fassifern Coal, according to Knight (1950). Fassifern coal dated at 253.38 +/- 0.08 Ma and the underlying Upper Pilot A seam at 253.55 +/- 0.06 Ma by Metcalf et al. (2015).
• bed-level stratigraphic resolution
Environment/lithology: pond; lithified, fine-grained, tuffaceous, gray chert
Size classes: macrofossils, mesofossils
Preservation: mold/impression
Collected by R. Brown, R. Beattie in 2002-2005
Primary reference: O. BĂ©thoux, R. G. Beattie, and A. Nel. 2007. Wing venation and relationships of the order Glosselytrodea (Insecta). Alcheringa 31:285-296 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 111680: authorized by Matthew Clapham, entered by Matthew Clapham on 27.06.2011
Creative Commons license: CC BY (attribution)
Taxonomic list
Insecta | |
Gondvanocoleus chikatunovi n. gen. n. sp.
| |
"Eoglosselytrum perplexa" = Eoglosselytrum perplexum
"Eoglosselytrum perplexa" = Eoglosselytrum perplexum Riek 1953 winged insect |