| Snowy Plains Formation | |
|---|---|
| Stratigraphic range: Mississippian (Tournaisian), | |
| Type | Geological formation |
| Unit of | Mansfield Group |
| Overlies | Devonian rocks |
| Thickness | Between 250 m (820 ft) to 500 m (1,600 ft) (Home Station Sandstone Member) |
| Lithology | |
| Primary | Siltstone, mudstone, sandstone |
| Location | |
| Location | Mansfield, Victoria |
| Coordinates | 37°03′0″S 146°05′0″E / 37.05000°S 146.08333°E |
| Region | Victoria |
| Country | Australia |
The Snowy Plains Formation is a fossiliferous formation of the Mansfield Group, which had yielded most of the historically described Carboniferous fish taxa in Australia, located near Mansfield, Victoria. Specifically, it is of early Tournaisian age, the oldest subdivision of the Mississippian epoch.
Although the Snowy Plains Formation is most notable for its body fossils of various fish, it has also been the discovery site of several ichnotaxa.
The formation consists of the following members, in descending order (youngest to oldest):
The age of the Mansfield fish fauna of the formation was once determined to be of Late Devonian age by George Sweet in 1889 and Frederick McCoy in 1890, on the basis that the lithology of the rock strata was similar to the Old Red Sandstone of the Late Devonian in Scotland, and that the fossil taxa were similar. However, it was later determined by Arthur S. Woodward in 1906 that the fauna were actually of Carboniferous age, due to similarities with other Carboniferous fish faunas of Europe and America, and concluded that McCoy's account was erroneous. In more recent decades, it appeared that Eupleurogmus creswelli could no longer be substantiated due to insufficient material, and Acanthodes australis could not be identified at the species level. However, later works continue to include E. creswelli and A. australis.
Color key
|
Notes
Uncertain or tentative taxa are in small text
crossed out taxa are discredited.
| Actinopterygians of the Snowy Plains Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Images |
| Mansfieldiscus | M. sweeti (Formerly Elonichthys sweeti) |
Palaeonisciformes, Palaeoniscoidea |
|
| ?M. sp. | |||
| Novogonatodus | N. gibbus (Formerly Elonichthys gibbus) |
Palaeonisciformes, Palaeoniscoidea |
|
| N. kasantsevae | |||
| Chondrichthyans of the Snowy Plains Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Images |
| Acanthodes | A. australis | Acanthodiformes, Acanthodidae |
|
| A. sp. | |||
| Ageleodus | A. altus | Elasmobranchii incertae sedis |
|
| Ctenacanthus | C. sp. | Euselachii, Ctenacanthidae |
|
| Eupleurogmus | E. creswelli | Acanthodiformes, Acanthodidae |
|
| Gyracanthides | G. murrayi | Climatiiformes, Gyracanthidae |
|
| ?Tristychius | ?T. sp. | Euselachii, | |
| Acanthodii indet. | sp. indet. | Acanthodii incertae sedis |
|
| Hybodontoidea
gen. et sp. indet. |
sp. indet. | Euselachii (Hybodontiformes incertae sedis) |
|
| Sarcopterygians of the Snowy Plains Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Images |
| Barameda | B. decipiens | Rhizodontida, Rhizodontidae |
|
| B. mitchelli | |||
| Delatitia | D. breviceps
(Formerly Ctenodus breviceps) |
Dipnoi incertae sedis | |
| Ichnotaxa of the Snowy Plains Formation | |||
|---|---|---|---|
| Genus | Species | Notes | Images |
|
C. problematica |
Varies in size and surficial morphology due to animal behaviour. Possibly a result of an arthropod ploughing into the sandy sediment to feef. |
||
|
F. commerfordi |
Possibly made by insect larvae. |
||
|
M. mansfieldi |
Likely to have been made by a bivalve. |
||
|
P. tubularis |
Branching tubular burrows, possibly by an arthropod. |
||
|
P. lioparadus |
Unbranched tubular burrows, possibly by an arthropod. |
||
| Rusophycus | R. biloba | Likely to have been produced by a non-trilobite arthropod. | |
| R. eutendorfensis | |||
| R. jenningsi | |||
| R. sp. | |||
|
S. lincki |
Possibly made by an ostrocod. |
||