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The Mandagery Sandstone is a Late Devonian geological formation in New South Wales, Australia. It is one of several famed Australian lagerstätten, with thousands of exceptional fish fossils found at a site near the town of Canowindra.
| Mandagery Sandstone | |
|---|---|
| Stratigraphic range: | |
.jpg) Cast of the slab found in 1956, that preserves 114 fish individuals, which died when their freshwater pond dried up. Most of the individuals in the slab are the placoderms Remigolepis walkeri and Bothriolepis yeungae. One sarcopterygian individual is present, Canowindra grossi, the largest fish in the slab. Two small and inconspicuous juvenile Groenlandaspis are also preserved.[1] | |
| Type | Geological formation |
| Unit of | Nangar Subgroup, Hervey Group |
| Underlies | Pipe Formation |
| Overlies | Kadina Formation |
| Lithology | |
| Primary | Sandstone, Siltstone |
| Location | |
| Location | Canowindra, New South Wales |
| Region | New South Wales |
| Country |  Australia |
A sandstone block containing 114 fish was discovered in 1956 about 10 km west of Canowindra, on the road to Gooloogong. The Canowindra site was rediscovered by paleontologist Alex Ritchie in 1993, and over 3000 fish fossils have been catalogued and stored at the Australian Museum in Sydney[2] and the local Age of Fishes Museum in Canowindra. Antiarch placoderms make up the majority of specimens recovered; Bothriolepis and Remigolepis are the most abundant fossils, followed by the arthrodire Groenlandaspis. About 20 sarcopterygian (lobe-finned fish) fossils have also been found, including new taxa such as Canowindra, Mandageria,[2] Cabonnichthys,[3] Soederberghia[4] and Gooloogongia.[5] Fossils are preserved as natural moulds in the hard sandstone, filled by a mixture of sandstone, clay, and rare fragments of remaining bone. The detail of preservation is high, with individual armor plates, scales, and the internal structures of major bones all visible in latex casts produced from the moulds.[2][6][4]
The Mandagery Sandstone is part of the Hervey Group, a cluster of deformed Paleozoic sediments located near the center of the Lachlan Fold Belt in New South Wales. It is mostly fine-grained red orthoquartzite sandstone, arranged into a number of short sequences. Towards the top of each sequence, the red sandstone is supplanted by thin beds of white sandstone and red siltstone. Cross-bedding and mudcracks indicate that the sandstone was deposited close to the shore.[7]
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