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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>2</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/cpd-2-535-2006</doi>
	<article_url>http://www.clim-past-discuss.net/2/535/2006/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/2/535/2006/cpd-2-535-2006.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/2/535/2006/cpd-2-535-2006.pdf</fulltext_pdf>
	<start_page>535</start_page>
	<end_page>562</end_page>
	<publication_date>2006-08-18</publication_date>
	<article_title content_type="html">Detecting human impacts on the flora, fauna, and summer monsoon of Pleistocene Australia</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. H. Miller</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. W. Magee</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>M. L. Fogel</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>M. K. Gagan</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">INSTAAR and Dept. of Geological Sciences, University of Colorado, Boulder, CO 80309-0450, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Earth and Marine Sciences, Australian National University, Canberra, ACT 0200, Australia</affiliation>
		<affiliation numeration="3" content_type="html">Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Road, Washington, DC 20015, USA</affiliation>
		<affiliation numeration="4" content_type="html">Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia</affiliation>
	</affiliations>
	<abstract content_type="html">All of Australia&apos;s largest mammalian vertebrates became extinct 50 to 45 ka
(thousand years ago), shortly after human colonization. Between 60 and 40 ka
Australian climate was similar to present and not changing rapidly.
Consequently, attention has turned toward plausible human mechanisms for the
extinction, with proponents for over-hunting, ecosystem change, and
introduced disease. To differentiate between these options we utilize
isotopic tracers of diet preserved in eggshells of two large, flightless
birds to track the status of ecosystems before and after human colonization.
&amp;delta;&lt;sup&gt;13&lt;/sup&gt;C preserved in their eggshells monitor a bird&apos;s dietary
intake in the weeks to months before egg-laying. More than 500 dated
eggshells from central Australia of the Australian emu (&lt;I&gt;Dromaius novaehollandiae&lt;/I&gt;), an opportunistic,
dominantly herbivorous feeder, provide a continuous 140 kyr dietary &amp;delta;&lt;sup&gt; 13&lt;/sup&gt;C reconstruction. More than 350 dated eggshells from the same region
of the heavier, extinct, giant bird &lt;I&gt;Genyornis newtoni&lt;/I&gt; define its dietary intake from 140 ka
until its extinction about 50 ka. Additional dietary records for both
species were developed from two distant regions. Dromaius eggshell dietary  &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C
reveals an unprecedented reduction in the bird&apos;s food resources
about 50 ka, coeval in all three regions, suggesting conversion at that time
of a tree/shrub savannah with occasionally rich grasslands to the modern
desert scrub. We speculate that ecosystem collapse across the arid and
semi-arid zones is a consequence of systematic burning by early humans.
Genyornis diet everywhere is more restricted than in co-existing Dromaius, implying a more
specialized feeding strategy. These data suggest that generalist feeders,
such as Dromaius, were able to adapt to a changed vegetation regime, whereas more
specialized feeders, such as Genyornis, became extinct. The altered vegetation may
have also impacted Australian climate. Changes in the strength of climate
feedbacks linked to vegetation and soil type (moisture recycling, surface
roughness, albedo) may have weakened the penetration of monsoon moisture
into the continental interior under the new ecosystem. Climate modeling
suggests such a shift may have reduced monsoon rain in the interior by as
much as 50%.</abstract>
	<references>
	</references>
</article>

