AustArch: A Database of 14C and Luminescence Ages from Archaeological Sites in Australia
Alan Williams, Sean Ulm, 2014. https://doi.org/10.5284/1027216. How to cite using this DOI
Data copyright © Alan Williams unless otherwise stated
This work is licensed under the ADS Terms of Use and Access.
Primary contact
Alan
Williams
Fenner School of Environment and Society
Australian National University
Canberra
ACT 0200
Australia
Resource identifiers
- ADS Collection: 1661
- DOI:https://doi.org/10.5284/1027216
- How to cite using this DOI
| Record ID | 20103 |
|---|---|
| Site | Cuddie Springs |
| IBRA Region | Mulga Lands |
| Longitude | 147.2 |
| Latitude | -30.2 |
| Site Type | Open site |
| Lab Code | Not given |
| Age | 45300 |
| Error | 1900 |
| Material | Tooth enamel |
| Context | SU 6A |
| Method | U-series |
| Open or closed site | Open |
| Directly related to occupation? | U |
| Source | Grun et al., 2010 (Full bibliographic references are available from the Downloads page) |
| Notes | A well-known open site containing Aboriginal archaeological material over a megafauna bone bed. Unit 5 - 8 includes a wide variety of megafauna remains (including Diprotodon and Genyornis sp.) between c. 28,000BP - >30,000 BP. Artefacts occur from unit 6 in association with megafauna remains - the origins of these artefacts form the basis of human/climate megafauna extinction debate. The majority of the archaeological assemblage occurs in unit 5 and includes horsehoof cores, small single and multi platform cores and flakes, from silcrete, quartz, quartzite, chert, conglomerate, feldspar porphory, and sandstone. Unit 5 forms the upper of three bone beds present to depths of 4 m in at this site. This sample was an attempt at dating tooth enamel from several of the megafauna species within units 6A-12. Grun et al's data raised questions about the age of SU 6. This sample was identified as 2037. |
