The excavators of Cuddie Springs reject humans as the primary cause of megafauna extinctions. They conclude that the 10,000 years of co-habitation of humans and megafauna at Cuddie Springs suggests that climate changes that began before the human colonisation of Australia were responsible for the megafauna extinctions. Wroe and Field (2006) cite the staggered extinctions that have been occurring since at least 130,000 years ago and the fact that megafauna in Tasmania do not occur after 46,000 years ago but people only arrived across a land bridge at 37,000 years ago. This staggered decline, mostly occurring in contexts independent of humans, is linked to environmental evidence for increasingly arid and erratic conditions since 400–300,000 years ago. The large body size of the megafauna suggests low fecundity and low population densities which have been argued to have made them especially susceptible to extinction due to habitat loss from increasing aridity (Wroe and Field 2006).
The 10,000 years of co-habitation of humans and megafauna at Cuddie Springs that is the foundation of Wroe and Field’s argument has been the subject of intense critical examination. This critique has identified a number of details that weaken the integrity of the association between humans and megafauna. First are the finds themselves, such as relatively large number of grinding stones in Pleistocene-age layers (Fullagar and Field 1997), as well as tula-adze-like flakes (David 2002). The Pleistocene grinding stones are notable because they imply a broad-spectrum plant-processing economy much earlier than previously known in Australia (Fullagar and Field 1997). These finds are anomalous because in other parts of Australia they are restricted to late Holocene contexts (Gillespie and David 2001). Amongst the megafauna bone layers there is a tooth of a crocodile (Pallimnarchus sp.) that became extinct long before 40,000 years ago (Gillespie and David 2001). The tooth is also exfoliated and heavily mineralised and the preservation is not consistent with other bone and teeth in the same level. There are stone artefacts with hair and blood adhering, but in the same layers there are megafauna bones with not even traces of protein remaining (Brook, et al. 2006; Coltrain, et al. 2004; Dodson, et al. 1993; Garling 1998).
These inconsistent finds suggest that the process of site formation may have involved some mixing of materials of different ages. This leads to the second important detail, the stratigraphy. Cuddie Springs is unusual in having a dense deflation pavement that separates recent materials (such as cow bones) from the Pleistocene layers. The layers above the pavement contains cow bones mixed with megafauna bones but the layers below contain no cow bones. (Field and Dodson 1999). David (2002) has asked where the rocks in this pavement come from in a stone-poor riverine plain, and suggested that they may been carried by Aboriginal people from a gibber plain 4km from the site or by farmers during the late 19th or early 20th century to create a firm footing for people or cattle. Gillespie and Brook (2006) also suggest that the stone artefacts in the pavement are unusually dense for a Pleistocene archaeological site and may have been transported during well construction or represent an in situ but late Holocene archaeological site overlaying disturbed Late Pleistocene sediments. There is a long history of European activity at Cuddie Springs, with a well dug in 1876, ten metres from the 1990s excavation and trenches dug by the Australian Museum in 1933. These events likely caused disturbance of the stratigraphy. Gillespie and Brook add that cattle visiting the well may have pushed stone artefacts through the pavement into the Pleistocene layers during waterlogged conditions. Tracing the origins of the pavement is crucial to understanding the integrity of the Pleistocene layers.
Several authors have suggested that the Pleistocene stone artefacts and megafauna bones may have derived from separate contexts that have become mixed by underground water flow. Because it is a ground-fed spring and a site that is periodically inundated by rain, sediment at Cuddie Springs is highly likely to have been moved by water. The depth of the historic well suggests that the ground water level may have been near the level of the Pleistocene layers (Gillespie and Brook 2006). Gillespie and David (2001) suggest that the upright orientation of an unarticulated Genyornis femur in the Pleistocene layers at Cuddie Springs might be explained by sediment movement by water flow is responsible for. This suggests that the megafauna bones might derive from much older sediments and have been reworked into the stone artefact bearing layers. A more direct link between the stone artefacts and the bones would be cut marks on the bones, but there are ‘few cut marks on any bones’ at Cuddie Springs (Field, et al. 2001: 698). Evidence favour of an intact Pleistocene deposit comes from analysis of Rare Earth Elements (REE) in the megafauna bones. The REE contents of the bones suggests that each depositional unit contains fauna with a discrete chemical signature and, therefore, a discrete and distinct postdepositional history, arguing against any postdepositional movement and mixing of bone between stratigraphic horizons (Trueman, et al. 2005). Gillespie and Brook (2006) comment that this still does not exclude an off-site origin of the bones (i.e. death of the animal) and subsequent fluvial transportation to Cuddie Springs. Field et al. (2006) dispute the proposal that flood movement caused the combination of megafauna and stone artefacts. They report that the sediments enclosing the bones and stones are fine-grained silts and clays resulting from a low-energy flow of water. They argue that if floods were responsible then larger sediments such as sands and gravels would have been found also.
The possibility of mixed Pleistocene deposits is also suggested by some interpretations of the chronology of the site, a third focus of the critiques (figure 6). So far, there are 20 radiocarbon dates and seven luminescence dates published for Cuddie Springs (Gillespie and Brook 2006). Statistical analysis by Gillespie and Brook (2006) of the 16 radiocarbon dates from the Pleistocene layers (ranging from 28 to 33,000 years ago) suggest that they do not increase in age as depth increases. They interpret this to mean that the sediments have been disturbed since they were first deposited. The luminescence dates also suggest mixing, with Roberts et al. (2001) finding that the sediments sampled for dating have multiple palaeodose populations, suggesting that sediments in the same sample were deposited at different times, rather than all at the same time. As mentioned above, the megafauna bones contain undetectable amounts of protein, so direct dating of the bones has so far been unsuccessful (Clarke 1999; Coltrain, et al. 2004).
The uniqueness archaeological and palaeontological finds from Cuddie Springs and its unusual stratigraphy have attracted especially detailed critiques that cast doubt on the integrity of the human-megafauna coexistence. Despite these problems, Cuddie Springs is uniquely significant as a major focus of research into the question of how the Australian megafauna became extinct.
Brook, B., R. Gillespie and P. Martin 2006 Megafauna mix-up [Fresh evidence indicates that humans were responsible for the extinction of Australia's megafauna.]. Australasian Science (2000) 27(5):35-37.
Brook, B. W. and D. M. J. S. Bowman 2002 Explaining the Pleistocene megafaunal extinctions: Models, chronologies, and assumptions. PNAS 99(23):14624-14627.
Clarke, S. J. 1999 The application of the amino acid racemisation geochronological technique to the Australian megafaunal locality, Cuddie Springs. Unpublished BSc Hons Thesis, University of Wollongong.
Coltrain, J. B., J. Field, R. Cosgrove and J. O'Connell 2004 Stable isotope and protein analyses of Cuddie Springs Genyornis [Research Reports.]. Archaeology in Oceania 39(1):50-51.
David, B. 2002 Landscapes, Rock-art and the Dreaming: an archaeology of preunderstanding. Leicester University Press, London.
Dodson, J. R., R. Fullagar, J. H. Furby and I. P. Prosser 1993 Humans and megafauna in a Late Pleistocene environment at Cuddie Springs, northwestern New South Wales. Archaeology in Oceania 28:93-99.
Duncan, J. 2001 Megafauna at Keilor and the timing of their extinction. Australian Archaeology 53:16-22.
Field, J. and J. R. Dodson 1999 Late Pleistocene megafauna and archaeology from Cuddie Springs, southeastern Australia. Proceedings of the Prehistoric Society 65:275-301.
Field, J., H., R. Fullagar and G. Lord 2001 A large area archaeological excavation at Cuddie Springs. Antiquity 75(290):696.
Field, J., S. Wroe and R. Fullagar 2006 BLITZKRIEG: Fact and Fiction at Cuddie Springs. Australasian Science 27(6):28.
Field, J. H., J. R. Dodson and I. P. Prosser 2002 A Late Pleistocene vegetation history from the Australian semi-arid zone. Quaternary Science Reviews 21(8-9):1023-1037.
Fullagar, R. and J. Field, H. 1997 Pleistocene seed-grinding implements from the Australian arid zone. Antiquity 71(272):300.
Garling, S. J. 1998 Megafauna on the menu? Haemoglobin crystallisation of blood residues from stone artefacts at Cuddie Springs. . In A Closer Look, Archaeological Methods Series 6, edited by R. Fullagar, pp. 29-48. Sydney University, Sydney.
Gillespie, R. and B. W. Brook 2006 Is there a Pleistocene archaeological site at Cuddie Springs? Archaeology in Oceania 41(1):1-11.
Gillespie, R. and B. David 2001 The importance, or impotence, of Cuddie Springs. Australasian Science 22(9):42.
Trueman, C., N. G. , J. Field, H. , J. Dortch, B. Charles and S. Wroe 2005 Prolonged coexistence of humans and megafauna in Pleistocene Australia. Proceedings of the National Academy of Sciences of the United States of America 102(23):8381.
White, J. P. and T. F. Flannery 1995 Late Pleistocene fauna at Spring Creek, Victoria: A re-evaluation. Australian Archaeology 40:13-16.
Wroe, S. and J. Field 2006 A review of the evidence for a human role in the extinction of Australian megafauna and an alternative interpretation. Quaternary Science Reviews 25(21-22):2692-2703.