Climate Variation and the Rise and Fall of an Andean Civilization
Identifieur interne : 000658 ( Istex/Corpus ); précédent : 000657; suivant : 000659Climate Variation and the Rise and Fall of an Andean Civilization
Auteurs : Michael W. Binford ; Alan L. Kolata ; Mark Brenner ; John W. Janusek ; Matthew T. Seddon ; Mark Abbott ; Jason H. CurtisSource :
- Quaternary Research [ 0033-5894 ] ; 1997.
Abstract
Paleolimnological and archaeological records that span 3500 years from Lake Titicaca and the surrounding Bolivian–Peruvian altiplano demonstrate that the emergence of agriculture (ca. 1500 B.C.) and the collapse of the Tiwanaku civilization (ca. A.D. 1100) coincided with periods of abrupt, profound climate change. The timing and magnitude of climate changes are inferred from stratigraphic evidence of lake-level variation recorded in14C-dated lake-sediment cores. Paleo-lake levels provide estimates of drainage basin water balance. Archaeological evidence establishes spatial and temporal patterns of agricultural field use and abandonment. Prior to 1500 B.C., aridity in the altiplano precluded intensive agriculture. During a wetter period from 1500 B.C. to A.D. 1100, the Tiwanaku civilization and its immediate predecessors developed specialized agricultural methods that stimulated population growth and sustained large human settlements. A prolonged drier period (ca. A.D. 1100–1400) caused declining agricultural production, field abandonment, and cultural collapse.
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DOI: 10.1006/qres.1997.1882
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A.D. 1100) coincided with periods of abrupt, profound climate change. The timing and magnitude of climate changes are inferred from stratigraphic evidence of lake-level variation recorded in14C-dated lake-sediment cores. Paleo-lake levels provide estimates of drainage basin water balance. Archaeological evidence establishes spatial and temporal patterns of agricultural field use and abandonment. Prior to 1500 B.C., aridity in the altiplano precluded intensive agriculture. During a wetter period from 1500 B.C. to A.D. 1100, the Tiwanaku civilization and its immediate predecessors developed specialized agricultural methods that stimulated population growth and sustained large human settlements. A prolonged drier period (ca. A.D. 1100–1400) caused declining agricultural production, field abandonment, and cultural collapse.</div></front></TEI><istex><corpusName>elsevier</corpusName><author><json:item><name>Michael W. 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Kolata, Ed.</ce:note-para></ce:article-footnote><ce:dochead><ce:textfn>Regular Article</ce:textfn></ce:dochead><ce:title>Climate Variation and the Rise and Fall of an Andean Civilization</ce:title><ce:author-group><ce:author><ce:given-name>Michael W.</ce:given-name><ce:surname>Binford</ce:surname><ce:cross-ref refid="QR971882A0"><ce:sup>a</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Alan L.</ce:given-name><ce:surname>Kolata</ce:surname><ce:cross-ref refid="QR971882A1"><ce:sup>b</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Mark</ce:given-name><ce:surname>Brenner</ce:surname><ce:cross-ref refid="QR971882A2"><ce:sup>c</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>John W.</ce:given-name><ce:surname>Janusek</ce:surname><ce:cross-ref refid="QR971882A3"><ce:sup>d</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Matthew T.</ce:given-name><ce:surname>Seddon</ce:surname><ce:cross-ref refid="QR971882A3"><ce:sup>d</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Mark</ce:given-name><ce:surname>Abbott</ce:surname><ce:cross-ref refid="QR971882A4"><ce:sup>e</ce:sup></ce:cross-ref><ce:cross-ref refid="QR971882FN1"><ce:sup>1</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Jason H.</ce:given-name><ce:surname>Curtis</ce:surname><ce:cross-ref refid="QR971882A5"><ce:sup>f</ce:sup></ce:cross-ref></ce:author><ce:affiliation id="QR971882A0"><ce:label>a</ce:label><ce:textfn>Graduate School of Design, Harvard University, 48 Quincy Street, Cambridge, Massachusetts, 02138</ce:textfn></ce:affiliation><ce:affiliation id="QR971882A1"><ce:label>b</ce:label><ce:textfn>Department of Anthropology, University of Chicago, 1126 East 59th Street, Chicago, Illinois, 60637</ce:textfn></ce:affiliation><ce:affiliation id="QR971882A2"><ce:label>c</ce:label><ce:textfn>Department of Fisheries and Aquatic Sciences, University of Florida, 7922 N.W. 71st Street, Gainesville, Florida, 32653</ce:textfn></ce:affiliation><ce:affiliation id="QR971882A3"><ce:label>d</ce:label><ce:textfn>Department of Anthropology, University of Chicago, 1126 East 59th Street, Chicago, Illinois, 60637</ce:textfn></ce:affiliation><ce:affiliation id="QR971882A4"><ce:label>e</ce:label><ce:textfn>Limnological Research Center, 220 Pillsbury Hall, 310 Pillsbury Drive S.E. University of Minnesota, Minneapolis, Minnesota, 55455</ce:textfn></ce:affiliation><ce:affiliation id="QR971882A5"><ce:label>f</ce:label><ce:textfn>Department of Geology, University of Florida, Gainesville, Florida, 32611</ce:textfn></ce:affiliation><ce:footnote id="QR971882FN1"><ce:label>1</ce:label><ce:note-para>Present address: Department of Geosciences, University of Massachusetts, Amherst, MA 01003-5820.</ce:note-para></ce:footnote></ce:author-group><ce:date-received day="7" month="5" year="1996"></ce:date-received><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>Paleolimnological and archaeological records that span 3500 years from Lake Titicaca and the surrounding Bolivian–Peruvian altiplano demonstrate that the emergence of agriculture (ca. 1500 B.C.) and the collapse of the Tiwanaku civilization (ca. A.D. 1100) coincided with periods of abrupt, profound climate change. The timing and magnitude of climate changes are inferred from stratigraphic evidence of lake-level variation recorded in<ce:sup>14</ce:sup>C-dated lake-sediment cores. Paleo-lake levels provide estimates of drainage basin water balance. Archaeological evidence establishes spatial and temporal patterns of agricultural field use and abandonment. Prior to 1500 B.C., aridity in the altiplano precluded intensive agriculture. During a wetter period from 1500 B.C. to A.D. 1100, the Tiwanaku civilization and its immediate predecessors developed specialized agricultural methods that stimulated population growth and sustained large human settlements. A prolonged drier period (ca. A.D. 1100–1400) caused declining agricultural production, field abandonment, and cultural collapse.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Climate Variation and the Rise and Fall of an Andean Civilization</title></titleInfo><titleInfo type="alternative" lang="en" contentType="CDATA"><title>Climate Variation and the Rise and Fall of an Andean Civilization</title></titleInfo><name type="personal"><namePart type="given">Michael W.</namePart><namePart type="family">Binford</namePart><affiliation>Graduate School of Design, Harvard University, 48 Quincy Street, Cambridge, Massachusetts, 02138</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Alan L.</namePart><namePart type="family">Kolata</namePart><affiliation>Department of Anthropology, University of Chicago, 1126 East 59th Street, Chicago, Illinois, 60637</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Mark</namePart><namePart type="family">Brenner</namePart><affiliation>Department of Fisheries and Aquatic Sciences, University of Florida, 7922 N.W. 71st Street, Gainesville, Florida, 32653</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">John W.</namePart><namePart type="family">Janusek</namePart><affiliation>Department of Anthropology, University of Chicago, 1126 East 59th Street, Chicago, Illinois, 60637</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Matthew T.</namePart><namePart type="family">Seddon</namePart><affiliation>Department of Anthropology, University of Chicago, 1126 East 59th Street, Chicago, Illinois, 60637</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Mark</namePart><namePart type="family">Abbott</namePart><affiliation>Limnological Research Center, 220 Pillsbury Hall, 310 Pillsbury Drive S.E. University of Minnesota, Minneapolis, Minnesota, 55455</affiliation><description>Present address: Department of Geosciences, University of Massachusetts, Amherst, MA 01003-5820.</description><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Jason H.</namePart><namePart type="family">Curtis</namePart><affiliation>Department of Geology, University of Florida, Gainesville, Florida, 32611</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="Full-length article"></genre><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">1997</dateIssued><copyrightDate encoding="w3cdtf">1997</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Paleolimnological and archaeological records that span 3500 years from Lake Titicaca and the surrounding Bolivian–Peruvian altiplano demonstrate that the emergence of agriculture (ca. 1500 B.C.) and the collapse of the Tiwanaku civilization (ca. A.D. 1100) coincided with periods of abrupt, profound climate change. The timing and magnitude of climate changes are inferred from stratigraphic evidence of lake-level variation recorded in14C-dated lake-sediment cores. Paleo-lake levels provide estimates of drainage basin water balance. Archaeological evidence establishes spatial and temporal patterns of agricultural field use and abandonment. Prior to 1500 B.C., aridity in the altiplano precluded intensive agriculture. During a wetter period from 1500 B.C. to A.D. 1100, the Tiwanaku civilization and its immediate predecessors developed specialized agricultural methods that stimulated population growth and sustained large human settlements. A prolonged drier period (ca. A.D. 1100–1400) caused declining agricultural production, field abandonment, and cultural collapse.</abstract><note>A. Kolata, Ed.</note><note type="content">Section title: Regular Article</note><relatedItem type="host"><titleInfo><title>Quaternary Research</title></titleInfo><titleInfo type="abbreviated"><title>YQRES</title></titleInfo><genre type="journal">journal</genre><originInfo><dateIssued encoding="w3cdtf">199703</dateIssued></originInfo><identifier type="ISSN">0033-5894</identifier><identifier type="PII">S0033-5894(00)X0054-3</identifier><part><date>199703</date><detail type="volume"><number>47</number><caption>vol.</caption></detail><detail type="issue"><number>2</number><caption>no.</caption></detail><extent unit="issue pages"><start>125</start><end>250</end></extent><extent unit="pages"><start>235</start><end>248</end></extent></part></relatedItem><identifier type="istex">668725AC52BDA2247F08CF75E230B04E8C9DE2FF</identifier><identifier type="DOI">10.1006/qres.1997.1882</identifier><identifier type="PII">S0033-5894(97)91882-2</identifier><accessCondition type="use and reproduction" contentType="copyright">©1997 University of Washington</accessCondition><recordInfo><recordContentSource>ELSEVIER</recordContentSource><recordOrigin>University of Washington, ©1997</recordOrigin></recordInfo></mods></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
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