Gregory John Retallack (born 8 November 1951) is an Australian paleontologist, geologist, and author who specializes in paleopedology, the study of fossil soils. He is a professor emeritus at University of Oregon and his research is primarily concerned with the fossil record of soils though Earth history. His research has included investigations into climate change, the extinction of dinosaurs, and the origins of upright walking humans. Retallack has controversially claimed that Ediacaran-era fossils represent terrestrial lichens as opposed to the consensus view that they present marine organisms including animals. He has written two books on paleopedology, and has appeared in numerous media shows.
A fossil collector since a young age, Retallack was outspoken concerning federal seizure in 1993 of Sue (dinosaur) the skeleton of Tyrannosaurus rex excavated by Pete Larson.
Work
Evolution of life on land
Oligocene fossil soils of well-drained woodlands (red bands) and swamps (black spots) in the Painted Hills, Oregon
Retallack's research focuses on the study of paleosols (fossilized soils) to reconstruct ancient environments. In 1973, he proposed that paleosols preserved beneath fossil plant horizons could provide data on ancient plant communities that plant fossils alone could not reveal. He has applied this approach to various stages of evolutionary history, offering hypotheses that sometimes challenge established scientific understanding.
Research findings
Retallack has used paleosols to investigate several major extinction and evolutionary events. Regarding climate change, he argued that the coevolution of grasslands and grazers over the past 50 million years drove global cooling via carbon biosequestration. In the field of human evolution, Retallack's fieldwork in Kenya concerning Proconsulidae (primates ancestral to humans) led him to suggest that the evolutionary transition to an upright stance occurred in woodland environments rather than in open savannas. Regulation of global temperature by the balance of plants and animals has been called the Proserpina Principle.
He has also applied this methodology to mass extinction events. Studying the Cretaceous-Paleogene boundary in Montana, he hypothesized that acid rain resulting from an extraterrestrial impact contributed to the extinction of dinosaurs. Similarly, his work in Antarctica on the Permian-Triassic boundary led to the hypothesis that the mass extinction was driven by a greenhouse gas crisis caused by methane released from coal intrusions during massive volcanic events (flood basalts). Furthermore, he has proposed a "woodland hypothesis" regarding the Devonian transition of vertebrates from fish to amphibians.
In 2013, Retallack identified supposed fossils in Paleoproterozoic paleosols from South Africa, which he named Diskagma. He identified the species as a fungus comparable to the living Geosiphon. Dated to 2.2billion years old, these fossils would push back the record of life on land significantly from the previously accepted record of 1.2billion years
Retallack's work interpreting the Avalon and White Sea assemblages of the Ediacaran biota as lichens has been challenged. His proposal that Ediacaran fossils were preserved in subaerial paleosols, and thus not marine fossils, has been supported by a minority of researchers but not other paleontologists. Nature called it a "controversial claim" in a news report, in which paleontologist Guy Narbonne said "[I]t quickly became clear that there are simpler explanations for the features Retallack had validly noted, and most of us moved on to more promising explanations." Despite a majority of Ediacaran researchers who reject his claims based on a body of research, Retallack continues to test his position.
In 2020, Retallack and other researchers claimed to have found Dickinsonia fossils from Bhimbetka rock shelters, India. However, in 2023 other researchers found that the material was actually the decayed remnants of a beehive.
He served as the president and vice president of the Cordilleran Section of the Paleontological Society, of the Oregon Academy of Sciences, and of the University of Oregon Chapter of the Society of Sigma Xi.
Awards and honors
Retallack has been honored for his research, including the Stillwell Award of the Geological Society of Australia, for best paper in the society journal in 1977, Ingerson Award of the Geochemical Society in 2015, and the Antarctica Service Medal of the U.S. National Science Foundation in 1999. He has been an invited lecturer throughout the U.S., and also to Germany, England, China, Thailand and India.
Retallack, G. J. (2008). "Rocks, views, soils and plants at the temples of ancient Greece". Antiquity. 82 (317): 640–657. doi:10.1017/s0003598x00097283. S2CID15115738.
↑Retallack, G. J.; Bestland, E. A.; Fremd, T. J. (2000). Eocene and Oligocene paleosols and environmental change in central Oregon. Boulder, Colorado: Geological Society of America Special Paper 344. ISBN978-0-8137-2344-0.
↑Retallack, G. J. (1973). "Stratigraphy, palaeobotany and environmental analysis of an area around Pittwater, north of Sydney, N.S.W.". BSC Honours Thesis, University of New England. Armidale, New South Wales.
↑Retallack, G. J. (1977). "Triassic palaeosols in the upper Narrabeen Group of New South Wales. Part II: Classification and reconstruction". Journal of the Geological Society of Australia. 24 (1–2): 19–35. doi:10.1080/00167617708728964.
↑Retallack, G. J. (1997). "Palaeosols in the upper Narrabeen Group of New South Wales as evidence of Early Triassic palaeoenvironments without exact modern analogues". Australian Journal of Earth Sciences. 44 (2): 185–201. Bibcode:1997AuJES..44..185R. doi:10.1080/08120099708728303.
↑Retallack, G. J. (2013). "Global cooling by grasslands in the geological past and near future". Annual Review of Earth and Planetary Sciences. 41: 5.1–18. doi:10.1146/annurev-earth-050212-124001.
↑Retallack, G. J. (2007). "Paleosols". In Henke, W.; Tattersall, I. (eds.). Handbook of paleoanthropology, Volume 1. Principles, methods and approaches. Vol.1. Berlin: Springer Verlag. pp.383–408.
↑Retallack, G. J. (2004). "End-Cretaceous acid rain as a selective extinction mechanism between birds and dinosaurs". In Currie, P. J.; Koppelhus, E. B.; Shugar, M. A.; Wright, J. L. (eds.). Feathered dragons: studies on the transition from dinosaurs to birds. pp.35–64.
12Retallack, G. J.; Krull, E. S.; Thackray, G. D.; Parkinson, D. (2013). "Problematic urn-shaped fossils from a Paleoproterozoic (2.2 Ga) paleosol in South Africa". Precambrian Research. 235: 71–87. Bibcode:2013PreR..235...71R. doi:10.1016/j.precamres.2013.05.015.
↑Peter Byrne (24 April 2014). "Early Life in Death Valley". Quanta Magazine. Retrieved 8 May 2014. Reprinted in ScientificAmerican.com