Belmont (Pincombe 1922 coll): Changhsingian, Australia
collected by T.H. Pincombe 1922

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Insecta - Hemiptera - Prosbolidae
Orthoscytina tetraneura n. sp. Tillyard 1926
1 specimen
July 14th, 1922 (1 measurement)
Orthoscytina belmontensis n. sp. Tillyard 1926
1 specimen
February 2, 1922 (1 measurement)
Orthoscytina subcostalis n. sp. Tillyard 1926
1 specimen
(1 measurement)
Insecta - Protelytroptera - Permophilidae
Permophilus pincombei n. gen., n. sp. Tillyard 1924
Tillyard 1924 1 specimen
Undated, but before 1924 (1 measurement)
Insecta - Coleoptera - Schizocoleidae
Permosyne pincombeae n. sp. Tillyard 1924
Tillyard 1924 1 specimen
recombined as Karakanocoleus pincombeae
Undated, but before 1924 (1 measurement)
Insecta - Coleoptera - Permosynidae
Permosyne belmontensis n. gen., n. sp. Tillyard 1924
Tillyard 1924 1 specimen
Undated, but before 1924 (1 measurement)
see common names

Geography
Country:Australia State/province:New South Wales
Coordinates: 33.0° South, 151.7° East (view map)
Paleocoordinates:66.5° South, 144.4° East
Basis of coordinate:estimated from map
Geographic resolution:outcrop
Time
Period:Permian Epoch:Lopingian
Stage:Changhsingian 10 m.y. bin:Permian 4
Key time interval:Changhsingian
Age range of interval:254.14000 - 251.90200 m.y. ago
Stratigraphy
Formation:Croudace Bay Member:Belmont Conglomerate
Stratigraphic resolution:bed
Stratigraphy comments: 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).
Lithology and environment
Primary lithology:tuffaceous lithified chert
Environment:pond Tectonic setting:foreland basin
Geology comments: Insect bed appears to have been deposited in shallow ephemeral floodbasin ponds and is stratigraphically positioned between fast-flowing river and coal swamp deposits. Volcanic ash draped the area, infilling the pools and preserving the taphocoenosis. Switch to contractional deformation in Hunter-Bowen orogeny occurred c. 265 Ma; Sydney basin transitioned into foreland basin.
Taphonomy
Modes of preservation:mold/impression
Size of fossils:macrofossils,mesofossils
Collection methods and comments
Reason for describing collection:taxonomic analysis
Collectors:T.H. Pincombe Collection dates:1922
Metadata
Database number:122414
Authorizer:M. Clapham Enterer:M. Clapham
Modifier:M. Clapham Research group:paleoentomology
Created:2011-12-26 17:13:23 Last modified:2017-05-23 16:34:15
Access level:the public Released:2011-12-26 17:13:23
Creative Commons license:CC BY
Reference information

Primary reference:

39003. R. J. Tillyard. 1926. Upper Permian insects of New South Wales Part 1. Introduction and the order Hemiptera. Proceedings of the Linnean Society of New South Wales 51:1-30 [M. Clapham/M. Clapham/M. Clapham]

Secondary references:

39031 R. J. Tillyard. 1924. Upper Permian Coleoptera and a new order from the Belmont Beds, New South Wales. Proceedings of the Linnean Society of New South Wales 49:429-435 [M. Clapham/M. Clapham]