Where: Queensland, Australia (27.5° S, 152.8° E: paleocoordinates 58.5° S, 101.2° E)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: Mount Crosby Formation, Norian (228.0 - 208.5 Ma)
• Purdy & Cranfield (2013) reported an unpublished SHRIMP date of 226±2 Ma for the Brisbane Tuff. Therefore, the Blackstone Formation may be considered younger than 226 Ma in absolute age. Thus, the Ipswich Coal Measures above the Brisbane Tuff, which is to say, the succession from the Mount Crosby Formation to the top of the Blackstone Formation must now be considered Norian.
• bed-level stratigraphic resolution
Environment/lithology: lacustrine - small; lithified shale
Size classes: macrofossils, mesofossils
Preservation: mold/impression
Collected by R.J. Tillyard; reposited in the BMNH
Primary reference: V. A. Blagoderov. 1999. New Bibionomorpha from the Triassic of Australia and Jurassic of central Asia with notes on Paraxymyiidae Rohdendorf (Insecta, Diptera). Proceedings of the First International Palaeoentomological Conference 11-15 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 113431: authorized by Matthew Clapham, entered by Matthew Clapham on 30.07.2011
Creative Commons license: CC BY (attribution)
Taxonomic list
Insecta | |
Tillyardiptera prima n. gen. n. sp.1
| |
Veriplecia handlirschi n. gen. n. sp.
Veriplecia handlirschi n. gen. n. sp. Blagoderov 1999 fungus gnat | |
Austrocramptonomyia minuta n. gen. n. sp.
Austrocramptonomyia minuta n. gen. n. sp. Blagoderov 1999 fly | |
"Heteroscytina tillyardi" = Hexascytina tillyardi2, "Hexascytina transecta n. gen. n. sp." = Hexascytina tillyardi2, Platyscytinella paradoxa2, Microscytinella radians n. gen. n. sp.2
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