continuous climatic impact on Holocene human population in the Rocky Mountains
Ancient cultural changes have often been linked to abrupt climatic events, but the potential that climate can exert a persistent influence on human populations has been debated. Here, independent population, temperature, and moisture history reconstructions from the Bighorn Basin in Wyoming (United...
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| Veröffentlicht in: | Proceedings of the National Academy of Sciences - PNAS 2013-01, Vol.110 (2), p.443-447 |
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| container_title | Proceedings of the National Academy of Sciences - PNAS |
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| creator | Kelly, Robert L. Surovell, Todd A. Shuman, Bryan N. Smith, Geoffrey M. |
| description | Ancient cultural changes have often been linked to abrupt climatic events, but the potential that climate can exert a persistent influence on human populations has been debated. Here, independent population, temperature, and moisture history reconstructions from the Bighorn Basin in Wyoming (United States) show a clear quantitative relationship spanning 13 ka, which explains five major periods of population growth/decline and ∼45% of the population variance. A persistent ∼300-y lag in the human demographic response conforms with either slow (∼0.3%) intrinsic annual population growth rates or a lag in the environmental carrying capacity, but in either case, the population continuously adjusted to changing environmental conditions. |
| doi_str_mv | 10.1073/pnas.1201341110 |
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Here, independent population, temperature, and moisture history reconstructions from the Bighorn Basin in Wyoming (United States) show a clear quantitative relationship spanning 13 ka, which explains five major periods of population growth/decline and ∼45% of the population variance. 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Here, independent population, temperature, and moisture history reconstructions from the Bighorn Basin in Wyoming (United States) show a clear quantitative relationship spanning 13 ka, which explains five major periods of population growth/decline and ∼45% of the population variance. A persistent ∼300-y lag in the human demographic response conforms with either slow (∼0.3%) intrinsic annual population growth rates or a lag in the environmental carrying capacity, but in either case, the population continuously adjusted to changing environmental conditions.</description><subject>Anthropology</subject><subject>basins</subject><subject>Biological Sciences</subject><subject>Carbon Radioisotopes - analysis</subject><subject>carrying capacity</subject><subject>Climate</subject><subject>Climate change</subject><subject>Climate models</subject><subject>Cultural change</subject><subject>Demographics</subject><subject>Demography</subject><subject>Depopulation</subject><subject>Environment</subject><subject>Environmental conditions</subject><subject>environmental factors</subject><subject>History, Ancient</subject><subject>human population</subject><subject>Human populations</subject><subject>Humans</subject><subject>Hydrology</subject><subject>Models, Theoretical</subject><subject>Paleoclimatology</subject><subject>Population Dynamics</subject><subject>Population growth</subject><subject>Population growth rate</subject><subject>Population size</subject><subject>Radiocarbon dating</subject><subject>Rain</subject><subject>Rocky Mountain region</subject><subject>Social Sciences</subject><subject>Temperature</subject><subject>variance</subject><subject>Wyoming</subject><issn>0027-8424</issn><issn>1091-6490</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNqFkb1vFDEQxS0EIkegpgIs0dBsMv72NkgoAoIUQAJSW16fnfOxay_rXaT89_h0xxFoqFy83zzPvIfQUwJnBBQ7H5MtZ4QCYZwQAvfQikBLGslbuI9WAFQ1mlN-gh6VsgWAVmh4iE4oo1KBZiv0yeU0x7TkpWDXx8HO0eE4jNbNOCd8mfvsfPJ4sww24TGPS1-RqsSE543HX7L7fos_5iXNNqbyGD0Iti_-yeE9Rdfv3n67uGyuPr__cPHmqrGSkLlxQQDXhHrFeIDOiQ46kKCcdFIH1dZ7RHDCdSLQjlEnRbsOrV5767rQuo6dotd733HpBr-uK86T7c041QumW5NtNH8rKW7MTf5pmOBCKVkNXh0Mpvxj8WU2QyzO971NvmZhiAZWA2WK_B-lirGaq9YVffkPus3LlGoSlZJagJZcVOp8T7kplzL5cNybgNnVana1mj-11onnd8898r97rMCzA7CbPNpVP2o4v6Nvy5ynI8CpEExDW_UXez3YbOzNFIu5_lr_l1B30ERT9gusqLtn</recordid><startdate>20130108</startdate><enddate>20130108</enddate><creator>Kelly, Robert L.</creator><creator>Surovell, Todd A.</creator><creator>Shuman, Bryan N.</creator><creator>Smith, Geoffrey M.</creator><general>National Academy of Sciences</general><general>National Acad Sciences</general><scope>FBQ</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QG</scope><scope>7QL</scope><scope>7QP</scope><scope>7QR</scope><scope>7SN</scope><scope>7SS</scope><scope>7T5</scope><scope>7TK</scope><scope>7TM</scope><scope>7TO</scope><scope>7U9</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>H94</scope><scope>M7N</scope><scope>P64</scope><scope>RC3</scope><scope>7X8</scope><scope>7S9</scope><scope>L.6</scope><scope>5PM</scope></search><sort><creationdate>20130108</creationdate><title>continuous climatic impact on Holocene human population in the Rocky Mountains</title><author>Kelly, Robert L. ; 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| subjects | Anthropology basins Biological Sciences Carbon Radioisotopes - analysis carrying capacity Climate Climate change Climate models Cultural change Demographics Demography Depopulation Environment Environmental conditions environmental factors History, Ancient human population Human populations Humans Hydrology Models, Theoretical Paleoclimatology Population Dynamics Population growth Population growth rate Population size Radiocarbon dating Rain Rocky Mountain region Social Sciences Temperature variance Wyoming |
| title | continuous climatic impact on Holocene human population in the Rocky Mountains |
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