The Gogo Formation in the Kimberley region of Western Australia is a Lagerstätte that exhibits exceptional preservation of a Devonian reef community. The formation is named after Gogo Station, a cattle station where outcrops appear and fossils are often collected from, as is nearby Fossil Downs Station.
Stratigraphic range: Frasnian
|Underlies||Virgin Hills Formation|
|Overlies||Unconformity with Prices Creek Group|
|Thickness||Up to 700 m (2,300 ft)|
|Location||Kimberley, Western Australia|
|Named for||Gogo Station|
|Thickness at type section||~425 m (1,394 ft)|
The reef, which now stands up abruptly in the western Australian desert (as the Windjana Limestone), was first identified in 1940 by paleontologist Curt Teichert, who discovered the first fossil fish from the region. It has been described for the layman by the driving force behind collecting expeditions at the Gogo Reef for the last two decades, John Long, of Museum Victoria in Melbourne, in Swimming in Stone: the Amazing Gogo Fossils of the Kimberley (Fremantle: Fremantle Arts Centre) 2007.
Unweathered sections of the Gogo Formation are made of siltstone, shale and calcarenite with numerous limestone concretions. These concretions are resistant to weathering, producing extensive nodule fields on the ground in areas where the surrounding rock has eroded away.
The Gogo sediments represent deep, hypoxic seafloor deposits in the vicinity of a large tropical reef composed primarily of algae and stromatoporoids during the Frasnian faunal stage of the Late Devonian. Associated stratigraphic units which comprise this ancient reef system are the Windjana Formation (the actual reef structures), Pillara Limestone (reef platform) and the Sadler Formation (fore-reef deposits).
The formation was deposited in the Frasnian (late Devonian).
The fossils of the Gogo Formation display three-dimensional soft-tissue preservation of tissues as fragile as nerves and embryos with umbilical cords. Over fifty species of fish have been described from the formation, and arthropods (including phylocarids and eurypterids) are similarly well-preserved. Nautiloids, goniatites and tentaculids are also known from the formation, but their soft tissue is not preserved.
The calcareous concretions formed around objects from the shallow reef areas which sank into the deep anoxic basins. The concretions sometimes contain the remains of fish, whose bodies are often preserved complete in three-dimensions due to rapid encasement and the slow rate of decay in the oxygen-poor surroundings. By repeated baths in a dilute acid solution, the matrix is dissolved away via a process of acid etching to reveal delicate fish fossils, some retaining impressions of soft tissues.
Among others, these fossils have been recovered from the Gogo Formation:
- "The Fossil Emblem of Western Australia" Accessed 16 August 2012.
- "Australian Stratigraphic Names Database". Australian Government Geoscience Australia. 29 September 2010. Retrieved 28 March 2011.
- Gogo Reef Formation
- Long, J. A.; Trinajstic, K. (2010). "The Late Devonian Gogo Formation Lägerstatte of Western Australia: Exceptional Early Vertebrate Preservation and Diversity". Annual Review of Earth and Planetary Sciences. 38: 255. Bibcode:2010AREPS..38..255L. doi:10.1146/annurev-earth-040809-152416.
- Ian Rolfe, W. D. (1966). "Phyllocarid Crustacean Fauna of European Aspect from the Devonian of Western Australia". Nature. 209 (5019): 192. Bibcode:1966Natur.209..192R. doi:10.1038/209192a0.
- Tetlie, O. E.; Braddy, S. J.; Butler, P. D.; Briggs, D. E. G. (2004). "A New Eurypterid (Chelicerata: Eurypterida) from the Upper Devonian Gogo Formation of Western Australia, with a Review of the Rhenopteridae". Palaeontology. 47 (4): 801. doi:10.1111/j.0031-0239.2004.00390.x.
- "Aussie fish fossil gives birth to history" Accessed 29 May 2008.
- Locality 47, No. 10 Bore Area at Fossilworks.org
- Locality No. 20, Stromatoporoid Camp Area at Fossilworks.org
- Paddys Valley at Fossilworks.org