Embankment of the Burwood colliery railway: Wuchiapingian, Australia
collected by John Mitchell
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Arberiopsida
- Arberiales
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Glossopteris sp.
Brongniart 1828
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Insecta
- Hemiptera
- Prosbolidae
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Mitchelloneura permiana n. gen., n. sp.
Tillyard 1921
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1 specimen | |||||||||
(1 measurement) | ||||||||||
Insecta
- Lophioneurida
- Lophioneuridae
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Lophioneura ustulata n. gen., n. sp.
Tillyard 1921
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1 specimen | |||||||||
(1 measurement) | ||||||||||
see common names |
Geography
Country: | Australia | State/province: | New South Wales |
Coordinates: | 33.0° South, 151.7° East (view map) | ||
Paleocoordinates: | 67.8° South, 150.1° East | ||
Basis of coordinate: | estimated from map | ||
Geographic resolution: | outcrop |
Time
Period: | Permian | Epoch: | Lopingian |
Stage: | Wuchiapingian | 10 m.y. bin: | Permian 4 |
Key time interval: | Wuchiapingian | ||
Age range of interval: | 259.51000 - 254.14000 m.y. ago |
Stratigraphy
Geological group: | Newcastle Coal Measures | ||||
Stratigraphy comments: Likely only three or four feet above the Dirty Seam of the Newcastle Series of coal seams, but possibility that fossil came from higher up in the sequence from the Burwood coal seam horizon, which is one hundred to one hundred and twenty feet above the dirty coal seam. The Dirty Seam is dated as Wuchiapingian, as Metcalf et al. (2015) dated the overlying Nobbys Tuff at 255.26 +/- 0.07 Ma and 255.02 +/- 0.03 Ma. |
Lithology and environment
Primary lithology: | red or brown lithified mudstone | ||
Lithology description: The material in which the fossils occur is of a bright brick-red colour and very hard, reminding one of the bricks made by the Romans and used by them in ancient Roman buildings in England. The materila has a shallow conchoidal fracture, for the most part very smooth." (Tillyard, 1921) | |||
Environment: | terrestrial indet. | Tectonic setting: | foreland basin |
Geology comments: 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
Collection methods: | surface (float),survey of museum collection |
Reason for describing collection: | taxonomic analysis |
Collectors: | John Mitchell |
Metadata
Database number: | 112125 | ||
Authorizer: | M. Clapham | Enterer: | J. Karr |
Modifier: | M. Clapham | Research group: | paleoentomology |
Created: | 2011-07-03 17:27:34 | Last modified: | 2017-05-23 16:34:15 |
Access level: | the public | Released: | 2011-07-03 17:27:34 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
36599. | R. J. Tillyard. 1921. Two fossil insect wings in the collection of Mr John Mitchell, from the Upper Permian of Newcastle, NSW belonging to the order Hemiptera. The Proceedings of the Linnean Society of New South Wales 46:413-422 [M. Clapham/J. Karr] |