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Beyond the radiocarbon limit in Australian archaeology and Quaternary research

Published online by Cambridge University Press:  02 January 2015

John Chappell ,
John Head  and
John Magee
John Chappell
Affiliation:
Division of Archaeology & Natural History, Research School of Pacific & Asian Studies, Australian National University, Canberra ACT 0200, Australia
John Head
Affiliation:
Division of Archaeology & Natural History, Research School of Pacific & Asian Studies, Australian National University, Canberra ACT 0200, Australia
John Magee
Affiliation:
Division of Archaeology & Natural History, Research School of Pacific & Asian Studies, Australian National University, Canberra ACT 0200, Australia
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Extract

Allen (1994) and Allen & Holdaway (1995), noticing the pattern in early radiocarbon dates from Australia, have advanced the notion their limit records the human settlement of the continent. A critical analysis of context and content in those carbon determinations leads to a different view. The results may be disconcerting for every region which builds its late Pleistocene chronologies on radiocarbon!

Type
Papers
Information
Antiquity , Volume 70 , Issue 269 , September 1996 , pp. 543 - 552
Copyright
Copyright © Antiquity Publications Ltd. 1996

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References

Allen, J. 1994. Radiocarbon determinations, luminescence dating and Australian archaeology, Antiquity 68: 339–43.Google Scholar
Allen, J. & Holdaway, S.. 1995. The contamination of radiocarbon determinations in Australia, Antiquity 69: 101–12.Google Scholar
Bard, E., Hamelin, B., Fairbanks, R. G., Zindler, A., Mathieu, G. & Arnold, M.. 1990. U/Th and 14C ages of corals from Barbados and their use for calibrating the 14C time scale beyond 9000 years BP, Nuclear Instruments & & Physics Research B52: 461–8.Google Scholar
Baynes, A. 1995. The question ‘why did the Australian megafauna become extinct’ is unanswerable. Abstracts, Taphonomy Symposium, Department of Anthropology & Archaeology, ANU, Canberra, April 1995: 12–14.Google Scholar
Bowler, J. M. & Wasson, R. J.. 1983. Glacial age environments of inland Australia, in Vogel, J. C. (ed.), Lare Cainozoic environments of the Southern Hemisphere: 183–208. Rotterdam: Balkema.Google Scholar
Chappell, J. 1995. Upper Quaternary sea-levels, coral terraces, oxygen isotopes and deep-sea temperatures, Journal of Geography (Japan) 103: 828–40.Google Scholar
Chappell, J., Broecker, W. S., Polach, H. A. & Thom, B. G.. 1974. Problem of dating upper Pleistocene sea-levels from coral reef areas, Second International Coral Reef Symposium 2: 563–71.Google Scholar
Chappell, J. & Polach, H. A.. 1972. Some effects of partial recrystallisation on C-14 dating of late Pleistocene corals and molluscs, Quaternary Research 2: 244–52.Google Scholar
Chappell, J. & Polach, H. A.. 1991. Post-glacial sea-level rise from a coral record at Huon Peninsula, Papua New Guinea, Nature 349: 147–9.Google Scholar
Chappell, J. & Shackleton, N. J.. 1986. Oxygen isotopes and sea-level, Nature 324: 137–40.Google Scholar
Colhoun, E. A., Van De Geer, G. & Mook, W. G.. 1982. Stratigraphy, pollen analysis, and paleoclimatic interpretation of Pulbeena Swamp, northwestern Tasmania, Quaternary Research 18: 108–26.CrossRefGoogle Scholar
Curtis, C.D. & Krinsley, D.. 1965. The detection of minor diagenetic alteration in shell material, Geochimica Cosmochimica Acta 29: 71–84.Google Scholar
Edwards, R. L., Beck, J. W., Burr, G. S., Donahue, D. J., Chappell, A.J.M., Bloom, A. L., Druffel, M.E.R. & Taylor, F. W.. 1993. A large drop in atmospheric 14C/12C and reduced melting in the Younger Dryas, documented with 230Th ages of corals, Science 260: 962–8.Google Scholar
Gillespie, R., Dlucokencky, E., Sparks, R. J., Wallace, G., Prosser, I. P. & Chappell, J.. 1992. Alluvial sediments: AMS dating at Lanyon and Wangrah Creek, Radiocarbon 34 (1): 21–8.Google Scholar
Gillespie, R., Magee, J. W., Luly, J.C., Dlugokencky, E., Sparks, R. J. & Wallace, G.. 1991. AMS radiocarbon dating in the study of arid environments: examples from Lake Eyre, South Australia, Palaeogeography, Palaeoclimatology, Palaeoecology 84: 333–8.Google Scholar
Head, M. J. 1979. Structure and properties of fresh and degraded wood: their effects on radiocarbon activity measurements. Unpublished MSc. thesis, Australian National University, Canberra.Google Scholar
Head, M. J. 1980. Structural characteristics of fossil wood, Institute for Conservation of Cultural Materials Bulletin 6: 17–23.Google Scholar
Hiscock, P. 1990. How old are the artifacts in Malakunanja II?, Archaeology in Oceania 25: 122–4.Google Scholar
Huntley, D. J., Hutton, J. T. & Prescott, J. R.. 1994. Further luminescence dates from the dune sequence in the southeast of South Australia, Quaternary Science Reviews 13: 201–8.Google Scholar
Mcdougall, I., Polach, H. A. & Stipp, J. J.. 1969. Excess radiogenic argon in young subaerial basalts from the Auckland volcanic field, New Zealand, Geochimica Cosmochimica Acta 33: 1485–1520.CrossRefGoogle Scholar
Magee, J. W., Bowler, J. M., Miller, G. H. & Williams, G.D.L.. 1995. Stratigraphy, sedimentology, chronology and palaeo-hydrology of Quaternary lacustrine deposits at Madigan Gulf, Lake Eyre, South Australia, Palaeogeography, Palaeo-climatology, Palaeoecology 113: 3–42.Google Scholar
Marshall, J. F. & Thom, B. G.. 1976. The sea-level in the Last Interglacial, Nature 263: 120–21.Google Scholar
Meltzer, D. J. & Mead, J. I.. 1985. Dating late Pleistocene extinctions, in Mead, J. I. & Meltzer, D. J. (ed.), Environments and extinctions: man in late glacial North America: 145–73. Orono (ME): University of Maine Center for the Study of Early Man.Google Scholar
Roberts, R. G., Jones, R. & Smith, M. A.. 1990a. Thermoluminescence dating of a 50,000-year-old human occupation site in northern Australia, Nature 345: 153–6.Google Scholar
Roberts, R. G., Jones, R. & Smith, M. A.. 1990b. Stratigraphy and statistics at Malakunanja II: reply to Hiscock, Archaeology in Oceania 25: 125–9.Google Scholar
Roberts, R. G., Jones, R., Spooner, N. A., Head, M. J., Murray, A. S. & Smith, M. A.. 1994. The human colonisation of Australia: optical dates of 53,000 and 60,000 years bracket human arrival at Deaf Adder Gorge, Northern Territory, Quaternary Geochronology, Quaternary Science Reviews 13: 575–83.Google Scholar
Roy, P. S., Zhuang, W.-Y., Birch, G. F. & Cowell, P. J.. 1992. Quaternary geology and placer mineral potential of the Forster-Tuncurry shelf, southeastern Australia. Department of Mineral Resources, New South Wales. Geological Survey Report GS 1992: 201,Google Scholar
Shackleton, N.J. 1987. Oxygen isotopes, ice volume and sea-level, Quaternary Science Reviews 6: 183–90.CrossRefGoogle Scholar
Stuiver, M., Long, A. & Kra, R. S. (ed.). 1993. Calibration 1993, Radiocarbon 35 (1).Google Scholar
Stuiver, M. & Polach, H. A.. 1977. Discussion, reporting of 14C data, Radiocarbon 19: 355–63.Google Scholar
Thom, B. G. 1973. The dilemma of high interglacial sea-levels during the Last Glaciation, Progress in Physical Geography 5: 170–246.Google Scholar
Zhu, Z., Marshall, J. F. & Chappell, J.. 1994. Effects of differential tectonic uplift on late Quaternary coral reef diagenesis, Australian Journal of Earth Sciences 41: 463–74.Google Scholar