10 Extinctions and Speciation During the Quaternary
Friday, 25 July 2003
8:00 AM - 12:00 PM
FAUNAL EXTINCTION AND DRAMATIC ECOSYSTEM CHANGE IN THE LATE QUATERNARY OF SEMI-ARID AUSTRALIA
Paper number: 10-9
Program: SYMPOSIA
Time: 10:30 AM – 10:50 AM
Authors
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Marilyn FogelCarnegie Institute of Washington, Washington, DC
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John W. MageeAustralian National Univ, Canberra, ACT, N/A
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Simon J. ClarkeCarnegie Institute of Washington, Washington, DC
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Stephen B. DeVogelUniv of Colorado, Boulder, CO
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Michael GaganAustralian National Univ, Canberra, ACT, N/A
Abstract
A 130,000-year record of dietary input and potential water sources for both birds has been reconstructed from stable C and O isotopes in more than 1000 individuals from south-central Australia, each dated by 14C, luminescence and/or racemization. Prior to 50 ka Dromaius diet was highly variable, ranging from 100% C-3 to 100% C-4. However, immediately after 50 ka, Dromaius diet shifted dramatically. C-4 plant contribution to their diet never exceeded 50% (n=200) after 50 ka, whereas more than half the samples older than 50 ka contain >50% C4 dietary sources. The dietary C input of Genyornis changed very little through the extinction window, although dramatic changes in d18O at the time of extinction imply great environmental stress. At Lake Eyre, Genyornis’ diet included a significant component of C-4 grass throughout the fossil record. We attribute the observed changes in Dromaius diets to reflect a fundamental rearrangement of the plant ecosystems favoring C-3 plants in semi-arid central Australia. As a generalist, Dromaius was able to adjust its feeding strategy to the changed environmental conditions, but Genyornis and other large herbivores were not. The coincidence in time of megafauna extinction and ecosystem collapse shortly after the arrival of modern humans, and the lack of similar changes during dramatic climate change earlier in the Quaternary, suggests there may be a causal link.