Birdrong Sandstone
Birdrong Sandstone | |
---|---|
Stratigraphic range: Hauterivian-Barremian ~ | |
Type | Geological formation |
Unit of | Barrow Group |
Underlies | Muderong Shale, Windalia Radiolarite & Tamala Limestone |
Overlies | Kockatea Shale, Forestier Claystone & Zeepaard Formation |
Thickness | Up to 79 m (259 ft) |
Lithology | |
Primary | Sandstone |
Other | Glauconite |
Location | |
Coordinates | 27°42′S 114°12′E / 27.7°S 114.2°E |
Approximate paleocoordinates | 52°54′S 70°00′E / 52.9°S 70.0°E |
Region | Western Australia |
Country | Australia |
Extent | Carnarvon Basin |
The Birdrong Sandstone is an Early Cretaceous (Hauterivian to Barremian)[1] geologic formation of the Barrow Group in Western Australia. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.[2]
Description
[edit]The Birdrong Sandstone has a maximum thickness of 79 metres (259 ft). The formation overlies the Kockatea Shale, Forestier Claystone and Zeepaard Formation and is overlain by the Muderong Shale, Windalia Radiolarite and Tamala Limestone.[3] At its type section at Mardathuna Station, northeast of Carnarvon, the Birdrong Sandstone begins with a fluvial phase of deposition, followed by deltaic and shallow marine facies.[4]
Fossil content
[edit]The following fossils were reported from the formation:
See also
[edit]References
[edit]- ^ Agnolin et al., 2010, p.258
- ^ Weishampel et al., 2004, pp.517-607
- ^ Birdong Sandstone at ASUD
- ^ Birdrong Sandstone in the Paleobiology Database
Bibliography
[edit]- Agnolin, Federico L.; Ezcurra, Martin D.; Pais, Diego F.; Salisbury, Steven W. (2009), "A reappraisal of the Cretaceous non-avian dinosaur faunas from Australia and New Zealand: evidence for their Gondwanan affinities", Journal of Systematic Palaeontology, 8 (2): 257–300, doi:10.1080/14772011003594870
- Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (2004), The Dinosauria, 2nd edition, Berkeley: University of California Press, pp. 1–880, ISBN 0-520-24209-2, retrieved 2019-02-21