What to make of the ‘Murchison Cement’?A re-examination of a megafaunal fossil site in the Mid West, Western Australia

Abstract The ‘Murchison Cement’ is a term that has been informally used since the 1960s to describe numerous stratigraphic units in the middle catchment of the Murchison and Greenough Rivers, in Mid West Western Australia. The significance of these deposits relates to their embedded artefact and megafaunal assemblages, uncovered by investigations from the Franco-Australian Quaternary Project (FAQP) during the 1970s. Researchers still debate the contemporaneity of the archaeological and megafaunal material within these deposits because of the complex nature of the depositional environment. This paper questions the practicality of the term Murchison Cement and reports on a new megafaunal fossil and possible artefact find at Ballinu (Ballinyoo) Spring. Preliminary sedimentological and micromorphological analyses show similarities in the sediment directly associated with the fossil and some of the artefacts archived from the FAQP. Initial luminescence analyses of silicified sediments associated with the fossil indicate a depositional age of ~56 kya, with evidence of reworking at approximately 14 kya. Whilst late Pleistocene human occupation in the region is indicated, the contemporaneity with megafaunal fossils remains uncertain.

[1]  A. Murray,et al.  Luminescence dating of quartz using an improved single aliquot regenerative-dose protocol , 2000 .

[2]  M. Aitken,et al.  An Introduction to Optical Dating: The Dating of Quaternary Sediments by the Use of Photon-Stimulated Luminescence , 1998 .

[3]  A. Goudie The Chemistry of World Calcrete Deposits , 1972, The Journal of Geology.

[4]  D. Nash,et al.  Silica and carbonate relationships in silcrete-calcrete intergrade duricrusts from the Kalahari of Botswana and Namibia , 1998 .

[5]  E. Fitzpatrick,et al.  Micromorphology of Soils , 1984 .

[6]  W. Huff X-ray Diffraction and the Identification and Analysis of Clay Minerals , 1990 .

[7]  Paul F. Green,et al.  Estimating the component ages in a finite mixture , 1990 .

[8]  K. Wyrwoll The sedimentology, stratigraphy and paleoenvironmental significance of a late Pleistocene alluvial fill: Central coastal areas of Western Australia , 1984 .

[9]  G. W. Brindley,et al.  X-Ray diffraction procedures for clay mineral identification , 1980 .

[10]  J. Prescott,et al.  Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths and long-term time variations , 1994 .

[11]  J. Raynal,et al.  Walga Rock and Billibilong Spring: Two Archaeological Sequences from the Murchison Basin, Western Australia , 1983 .

[12]  G. Laslett,et al.  STATISTICAL-MODELS FOR MIXED FISSION-TRACK AGES , 1993 .

[13]  K. Wyrwoll Late Quaternary climates of Western Australia: evidence and mechanisms , 1979 .

[14]  R. Gowland,et al.  The abrasion of modern and archaeological bones by mobile sediments: the importance of transport modes , 2011 .

[15]  G. Laslett,et al.  OPTICAL DATING OF SINGLE AND MULTIPLE GRAINS OF QUARTZ FROM JINMIUM ROCK SHELTER, NORTHERN AUSTRALIA: PART I, EXPERIMENTAL DESIGN AND STATISTICAL MODELS* , 1999 .

[16]  B. Singer A Quaternary geomagnetic instability time scale , 2013 .

[17]  Z. Jacobs,et al.  Timing and dynamics of Late Pleistocene mammal extinctions in southwestern Australia , 2010, Proceedings of the National Academy of Sciences.