Turee Creek Group

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Sub-units^[1]

UnderliesWyloo Group (Unconformably)

Turee Creek Group
Stratigraphic range: Siderian, possibly into the Rhyacian, 2400 Ma^[1] Pha. Proterozoic Archean Had. ↓
Type	Group
Unit of	Mount Bruce Supergroup^[2]
Sub-units	^[1] Kazput Formation Koolbye Formation Kungarra Formation
Underlies	Wyloo Group (Unconformably)
Overlies	Hamersley Group
Thickness	4 km (2.5 mi)^[3]
Lithology
Primary	Siltstone
Other	Sandstone, Diamictite, Dolomite, Chert
Location
Region	Western Australia
Country	Australia

The Turee Creek Group, is a geologic group in Western Australia, and is a part of the wider Mount Bruce Supergroup. It preserves a number of fossils dating back to the Siderian period, some of which are amongst the oldest known microfossil communities.

The Turee Creek Group is made up of three formations. The basal-most formation within the group is the Kungarra Formation, which is primarily composed of siltstone, with a layer of diamictite rock in the upper sections of the formation, which go under the name of the "Meteorite Bore Member". This is overlain by the middle Koolbye Formation, which is the thinnest of the three, and is predominately composed of sandstone. Finally, the upper-most formation within the group is the Kazput Formation, with dolomite and sandstone at its base, which then turns into just sandstone further towards the top.^[2] The group itself is overlain by the basalt composed Wyloo Group, and is underlain by the banded iron dominated Hamersley Group. Alongside the latter group, the Turee Creek Group is a part of the Mount Bruce Supergroup.^[2]

Dating

Through U-Pb dating of zircon samples collected from the base and top of the group, the group was confidentially placed into the Siderian period, although its true deposition age is still contended.^[1]

Zircon samples from the base of the group recovered a date of 2449±3 Ma,^[4] whilst samples from the top of the group recovered a date of 2209±15 Ma.^[5] Although, other studies have put forward other dates, for example in 2017, a deposition date of 2445±0 Ma – 2420±0 Ma was recovered from zircon crystals based on Detrital zircon geochronology,^[6] hinting at a general deposition age of 2400±0 Ma when combining all the dates.^[1]

Fossils

The Turee Creek Group contains a small number of important fossil localities, although the exact placement of a majority of these localities in relations to the formal formations remains difficult to figure out, but some studies note that even then all researchers agree that the following localities are within the Turee Creek Group.^[1]

Kazput Reef Complex

The Turee Creek Group is home to many stromatolites and thrombolites, with the most well known stromatolite–thrombolite locality being in the Kazput Syncline. This locality, known as the "Kazput Reef Complex" and only discovered in 2016,^[7] is composed of a 350 m (1,150 ft) thick and 15 km (9.3 mi) long dolomitic microbialite reef complex, which has been purposed to be a part of either the upper Kazput Formation or lower Kungarra Formation, with the latter seeming more likely in recent studies.^[8] Dating of the area has recovered a date between 2400±0 Ma – 2300±0 Ma, which would make the Kazput Reef Complex the oldest known Proterozoic reef complex yet, predating previous examples by some 300±0 Ma – 500±0 Ma.^[7]

The Kazput Reef Complex contains up to five distinct facies associations, which are as follows, in ascending age:

Association A: The basal-most facies of the reef complex, it is composed of thin-bedded dololutite–dolarenite, and contains abundant local stromatolites, which are dome-like in shape. It can get up to 55 m (180 ft) thick in known outcroppings, as the lower sections are not exposed.^[7]
Association B: This facies is primarily composed of more thin-bedded dololutite–dolarenite, in which there are inter-bedded columnar and strati-form stromatolites, thin-bedded thrombolite-like microbialites, and unique horizontally branching stromatolites throughout, which were all deposited in a shallow marine environment. Oncolite beds can also be found within this facies up to 29 cm (11.4 in) thick, with the facies itself getting up to 85 m (279 ft) thick also.^[7]
Association C: This facies is predominately composed of tightly packed club-shaped to columnar stromatolites, which were deposited in deeper waters, deepening the further up you go. This facies can get up to 90 m (300 ft) thick.^[7]
Association D: This facies is dominated by microbialites, which have a unique clotted structure. It is also the thinnest, only getting up to 40 m (130 ft) in some sections.^[7]
Association E: This top-most facies is mostly composed of more bedded dololutite–dolarenite, as well as thin-bedded ironstone, grey shale and black chert. It is also the thickest facies, getting up to 150 m (490 ft) thick in some areas.^[7] This facies also contains a number of microfossils embedded within the black chert layers, numbering up to eighteen distinct morphologies, and two distinct microfossil communities.^[1]

Microfossils

Within the Kazput Reef Complex, microfossils of varying shapes and sizes had been also recovered, numbering up to eighteen distinct morphotypes, two of which were previously unknown, and gave evidence to the fact that microbial communities were already quickly diversifying after the end of the Archean.^[1] These microfossils can be split into two distinct communities, which are as follows:

Nodular Black Cherts: This microfossil community is primarily composed of long filamentous microfossils, filamentous rosettes, unicellular forms of one size distribution, and large collapsed spherical aggregates. These were mostly like preserved in-situ, and within a deep water environment.^[1]
Bedded Black Cherts: This microfossil community was found within and around clasts of bedded black cherts, and is predominately composed of more unicellular forms varying in size, short degraded filaments, as well as star-shaped and umbrella-shaped rosettes. Around the clasts there are also large branching filamentous microfossils, with the clasts themselves most likely being transported from somewhere else, likely a shallow water environment, and may represent the oldest phototrophic microfossil community currently known in the world.^[1]^[8]

References

1 2 3 4 5 6 7 8 9 Barlow, Erica Victoria; Kranendonk, Martin Julian Van (August 9, 2018). "Snapshot of an early Paleoproterozoic ecosystem: Two diverse microfossil communities from the Turee Creek Group, Western Australia" (PDF). Geobiology. 16 (5): 449–475. Bibcode:2018Gbio...16..449B. doi:10.1111/gbi.12304. eISSN 1472-4669. ISSN 1472-4677. LCCN 2003201710. OCLC 52805553. PMID 30091832. S2CID 51939442. Retrieved December 28, 2025.
1 2 3 Martin, David McB. (February 1999). "Depositional setting and implications of Paleoproterozoic glaciomarine sedimentation in the Hamersley Province, Western Australia". Geological Society of America Bulletin. 111 (2): 189–203. doi:10.1130/0016-7606(1999)111<0189:DSAIOP>2.3.CO;2.
↑ Smith, R. E.; Perdrix, J. L.; Parks, T. C. (1 February 1982). "Burial Metamorphism in the Hamersley Basin, Western Australia". Journal of Petrology. 23 (1): 75–102. doi:10.1093/petrology/23.1.75.
↑ Barley, M. E.; Pickard, A. L.; Sylvester, P. J. (January 1997). "Emplacement of a large igneous province as a possible cause of banded iron formation 2.45 billion years ago". Nature. 385 (6611): 55–58. doi:10.1038/385055a0.
↑ Martin, D. McB.; Li, Z. X.; Nemchin, A. A.; Powell, C. McA. (1 November 1998). "A pre-2.2 Ga age for giant hematite ores of the Hamersley Province, Australia?". Economic Geology. 93 (7): 1084–1090. doi:10.2113/gsecongeo.93.7.1084.
↑ Krapež, Bryan; Müller, Stefan G.; Fletcher, Ian R.; Rasmussen, Birger (June 2017). "A tale of two basins? Stratigraphy and detrital zircon provenance of the Palaeoproterozoic Turee Creek and Horseshoe basins of Western Australia". Precambrian Research. 294: 67–90. doi:10.1016/j.precamres.2017.03.020.
1 2 3 4 5 6 7 Barlow, E.; Van Kranendonk, M. J.; Yamaguchi, K. E.; Ikehara, M.; Lepland, A. (July 2016). "Lithostratigraphic analysis of a new stromatolite–thrombolite reef from across the rise of atmospheric oxygen in the Paleoproterozoic Turee Creek Group, Western Australia". Geobiology. 14 (4): 317–343. doi:10.1111/gbi.12175.
1 2 Soares, G.G.; Van Kranendonk, M.J.; Belousova, E.; Thomson, S. (January 2019). "Phosphogenesis in the immediate aftermath of the Great Oxidation Event: Evidence from the Turee Creek Group, Western Australia". Precambrian Research. 320: 193–212. doi:10.1016/j.precamres.2018.10.017.

Turee Creek Group

Dating

Fossils

Kazput Reef Complex

Microfossils

See also

References

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