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	<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>5</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/cpd-5-771-2009</doi>
	<article_url>http://www.clim-past-discuss.net/5/771/2009/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/5/771/2009/cpd-5-771-2009.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/5/771/2009/cpd-5-771-2009.pdf</fulltext_pdf>
	<start_page>771</start_page>
	<end_page>796</end_page>
	<publication_date>2009-03-04</publication_date>
	<article_title content_type="html">Putting the rise of the Inca Empire within a climatic and land management context</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>A. J. Chepstow-Lusty</name>
			<email>a.lusty@aliceadsl.fr</email>
		</author>
		<author numeration="2" affiliations="3">
			<name>M. R. Frogley</name>
		</author>
		<author numeration="3" affiliations="4">
			<name>B. S. Bauer</name>
		</author>
		<author numeration="4" affiliations="5">
			<name>M. J. Leng</name>
		</author>
		<author numeration="5" affiliations="6">
			<name>K. P. Boessenkool</name>
		</author>
		<author numeration="6" affiliations="2,7">
			<name>C. Carcaillet</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>A. A. Ali</name>
		</author>
		<author numeration="8" affiliations="8">
			<name>A. Gioda</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut Français d&apos;Etudes Andines (IFEA), Lima, Peru</affiliation>
		<affiliation numeration="2" content_type="html">Centre for Bio-Archaeology and Ecology, Université Montpellier 2, Montpellier, France</affiliation>
		<affiliation numeration="3" content_type="html">Department of Geography, University of Sussex, Brighton, UK</affiliation>
		<affiliation numeration="4" content_type="html">Department of Anthropology, The University of Illinois at Chicago, Illinois, USA</affiliation>
		<affiliation numeration="5" content_type="html">NERC Isotope Geoscience Laboratory, Nottingham, UK</affiliation>
		<affiliation numeration="6" content_type="html">School of Earth, Ocean and Planetary Sciences, University of Cardiff, Cardiff, UK</affiliation>
		<affiliation numeration="7" content_type="html">Paleoenvironments and Chronoecology, Institut de Botanique, Montpellier, France</affiliation>
		<affiliation numeration="8" content_type="html">Universidad San Marcos and IRD, Lima, Peru</affiliation>
	</affiliations>
	<abstract content_type="html">The rapid expansion of the Inca from the Cuzco area of highland Peru
      produced the largest empire in the New World between
      ca. AD 1400–1532. Although this meteoric rise may in part be
      due to the adoption of innovative societal strategies, supported by
      a large labour force and standing army, we argue that this would not
      have been possible without increased crop productivity, which was linked to
      more favourable climatic conditions. A multi-proxy, high-resolution
      1200-year lake sediment record was analysed at Marcacocha,
      12 km north of Ollantaytambo, in the heartland of the Inca
      Empire. This record reveals a period of sustained aridity that began
      from AD 880, followed by increased warming from AD 1100 that lasted
      beyond the arrival of the Spanish in AD 1532. These increasingly
      warmer conditions allowed the Inca and their predecessors the
      opportunity to exploit higher altitudes from AD 1150, by constructing
      agricultural terraces that employed glacial-fed irrigation, in
      combination with deliberate agroforestry techniques. There may be some
      important lessons to be learnt today from these strategies for
      sustainable rural development in the Andes in the light of future
      climate uncertainty.</abstract>
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