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Australia: The Land Where Time Began |
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Abrupt Change in Vegetation in Southeast Australia Following Megafaunal Extinction in the Late Quaternary Coinciding with the spread of humans across the Australian Continent there was a substantial mass extinction of the marsupial megafauna (Bowler et al., 2003) across the continent between about 50,000-45,000 years ago (Roberts et al., 2001; Grün et al., 2010). There were also large shifts in the vegetation types across Australia at about this time, though it is uncertain if these changes resulted from the use of fire by the humans (Turney et al., 2008) - which then contributed to the extinction event - or whether the loss of the megafauna grazers (Rule et al., 2012; Flannery, 1990) resulted in the vegetation changes. In this paper the authors1 reconstruct past vegetation changes that occurred in southeast Australia by the use of the stable carbon isotopic composition of wax n-alkanes produced by higher plants and the used of the accumulation rates of levoglucosan, a biomarker, to determine the levels of biomass burning from a well-dated sediment core obtained offshore from the Murray-Darling Basin. Their results indicated that the abundance of C4 plants was 60-70 %, which is generally high from 58-44 ka, and the abundance of these C4 plants declined to 30 % by 43 ka and there was an increase in the burning of biomass. The transient shift in the vegetation continued for 3,000 years following the period of human colonisation and directly following the extinction of the megafauna that occurred between 48.9-43.6 ka (1). The authors1 concluded that in this region the extinction of the megafauna was not caused by the vegetation shift. They1 suggest their data are consistent with the hypothesis that the vegetation change was the consequence of large marsupial browser extinction, and these vegetation changes led to the fire-prone nature of the Australian landscape.
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Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading |