Warrawoona Group
Today, Warrawoona Group is a topic of great interest and relevance in modern society. Its impact can be seen in our daily lives, from the way we communicate to the way we carry out our daily activities. Warrawoona Group has captured the imagination of people of all ages, cultures and backgrounds, and has generated intense debate in different areas. In this article, we will thoroughly explore the impact of Warrawoona Group on our lives, analyzing its importance, its benefits and challenges, and the different points of view that exist around this topic that is so relevant today.
| Warrawoona Group | |
|---|---|
| Stratigraphic range: Paleoarchean ~ | |
 Warrawoona and Western Australia showing geological classification | |
| Type | Geological group |
| Unit of | Pilbara Supergroup |
| Lithology | |
| Primary | Chert |
| Other | Archean felsic volcanic rocks |
| Location | |
| Coordinates | 21°42′S 118°0′E / 21.700°S 118.000°E |
| Region | Western Australia |
| Country |  Australia |
| Extent | Pilbara craton |
| Type section | |
| Named for | Warrawoona |
| Named by | Arthur Hugh Hickman |
| Year defined | 1983 |
  Warrawoona Group (Australia)  Warrawoona Group (Western Australia) | |
The Warrawoona Group is a geological unit in Western Australia containing putative fossils of cyanobacteria cells. Dated 3.465 Ga, these microstructures, found in Archean chert, are considered to be the oldest known geological record of life on Earth.[1][2][3]
Description
The fossils in this group were discovered by Arthur Hugh Hickman in 1983 in Warrawoona, 21°42′S 118°0′E / 21.700°S 118.000°E, a region on the Pilbara craton in the northern part of Pilbara province.
Whether or not the fossils were authentic was disputed in the past, as abiotic processes could not be ruled out.[4][5] Currently the fossils are thought to be of biological origin, however there is no conclusive evidence of fossilized organisms in the formation, and whether the lines in the rock are fossilized stromatolites.[6]
The rocks also include felsic volcanic rocks.[7]
See also
- North Pole, WA for similar issues
- Origin of life
- Timetable of the Precambrian
- Geology of Australia
- Fig Tree Formation
References
- ^ Skrzypczak, A.; Derenne, S.; Robert, F.; Binet, L.; Gourier, D.; Rouzard, J.-N.; Clinard, C. (March 2004). Characterization Of The Organic Matter In An Archean Chert (Warrawoona, Australia) (PDF). 35th Lunar and Planetary Science Conference. League City, TX. Bibcode:2004LPI....35.1241S.
- ^ Derenne, S.; Robert, F.; Skrzypczak-Bonduelle, A.; Gourier, D.; Binet, L.; Rouzaud, J.-N. (July 2008). "Molecular evidence for life in the 3.5 billion year old Warrawoona chert". Earth and Planetary Science Letters. 272 (1–2): 476–480. Bibcode:2008E&PSL.272..476D. doi:10.1016/j.epsl.2008.05.014.
- ^ Schopf, J. W.; Packer, B. M. (September 1986). "Newly discovered early Archean (3.4–3.5 Ga Old) microorganisms from the Warrawoona Group of Western Australia". Origins of Life and Evolution of the Biosphere. 16 (3–4): 339–340. Bibcode:1986OrLi...16..339S. doi:10.1007/BF02422059. S2CID 39363922.
- ^ Brasier, M. D.; Green, O. R.; Jephcoat, A. P.; Kleppe, A. K.; Van Kranendonk, M. J.; Lindsay, J. F.; Steele, A.; Grassineau, N. V. (March 2002). "Questioning the evidence for Earth's oldest fossils". Nature. 416 (6876): 76–81. Bibcode:2002Natur.416...76B. doi:10.1038/416076a. PMID 11882895. S2CID 819491.
- ^ Hofmann, H. J. (June 2004). "Archean Microfossils and Abiomorphs". Astrobiology. 4 (2): 135–136. Bibcode:2004AsBio...4..135H. doi:10.1089/153110704323175115. PMID 15253835.
- ^ Wacey, D.; Kilburn, M. R.; Saunders, M.; Cliff, J.; Brasier, M. D. (August 2011). "Microfossils of sulphur-metabolizing cells in 3.4-billion-year-old rocks of Western Australia". Nature Geoscience. 4 (10): 698–702. Bibcode:2011NatGe...4..698W. doi:10.1038/ngeo1238.
- ^ DiMarco, Michael J.; Lowe, Donald R. (August 1989). "Stratigraphy and sedimentology of an early Archean felsic volcanic sequence, eastern Pilbara Block, Western Australia, with special reference to the Duffer Formation and implications for crustal evolution". Precambrian Research. 44 (2): 147–169. Bibcode:1989PreR...44..147D. doi:10.1016/0301-9268(89)90080-6.
Further reading
- Buick, R.; Groves, D. I.; Dunlop, J. S. R.; Lowe, D. R. (February 1995). "Abiological origin of described stromatolites older than 3.2 Ga: Comment and Reply". Geology. 23 (2): 191–192. Bibcode:1995Geo....23..191B. doi:10.1130/0091-7613(1995)023<0191:AOODSO>2.3.CO;2.
- Condie, K. C. (1981). Archean Greenstone Belts. Vol. 3. New York City: Elsevier Scientific Publishing Company. ISBN 0-444-41854-7.