THE KEILOR FOSSIL SKULL: GEOLOGICAL EVIDENCE OF ANTIQUITY 81 
elevation may represent eustatic fall in sea level caused by decreas- 
ing temperatures towards the end of the Riss-Wirm interglacial 
phase. 
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Hall, T. S., 1909. Victorian Hill and Dale. Pp. 160, 39 illustrations. Melbourne: 
Thomas C. Lothian. 
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Pritchard, G. B., 1899. On the Occurrence of Diprotodon australis Owen near 
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Selwyn, A. R. C., 1854. Report on the Geology, Palaeontology and Mineralogy 
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