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
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Orthoscytina tetraneura n. sp.
Tillyard 1926
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1 specimen | |||||||||
July 14th, 1922 (1 measurement) | ||||||||||
Orthoscytina belmontensis n. sp.
Tillyard 1926
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1 specimen | |||||||||
February 2, 1922 (1 measurement) | ||||||||||
Orthoscytina subcostalis n. sp.
Tillyard 1926
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1 specimen | |||||||||
(1 measurement) | ||||||||||
Insecta
- Protelytroptera
- Permophilidae
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Permophilus pincombei n. gen., n. sp.
Tillyard 1924
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Tillyard 1924 | 1 specimen | ||||||||
Undated, but before 1924 (1 measurement) | ||||||||||
Insecta
- Coleoptera
- Schizocoleidae
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Permosyne pincombeae n. sp.
Tillyard 1924
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Tillyard 1924 | 1 specimen | ||||||||
recombined as Karakanocoleus pincombeae | ||||||||||
Undated, but before 1924 (1 measurement) | ||||||||||
Insecta
- Coleoptera
- Permosynidae
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Permosyne belmontensis n. gen., n. sp.
Tillyard 1924
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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] |