Evidência contestando o deflorestamento como causa do colapso da antiga cidade maia de Copan, Honduras

quarta-feira, janeiro 20, 2010


Evidence disputing deforestation as the cause for the collapse of the anciente Maya polity of Copan, Honduras


  • Cameron L. McNeil a,1

  • David A. Burneyb, and 

  • Lida Pigott Burneyc



  • Author Affiliations
      1. aDepartment of Anthropology, Lehman College, The City University of New York, Bronx, NY 10468;


      2. bNational Tropical Botanical Garden, Kalaheo, HI 96741; and


      3. c Makauwahi Cave Reserve, Kalaheo, HI 96741


      1. Edited by Joyce Marcus, University of Michigan, Ann Arbor, MI, and approved November 5, 2009 (received for review May 1, 2009)
        Abstract
        Archaeologists have proposed diverse hypotheses to explain the collapse of the southern Maya lowland cities between the 8th and 10th centuries A.D. Although it generally is believed that no single factor was responsible, a commonly accepted cause is environmental degradation as a product of large-scale deforestation. To date, the most compelling scientific evidence used to support this hypothesis comes from the archaeological site of Copan, Honduras, where the analysis of a sediment core suggested a dramatic increase in forest clearance in the Late Classic period (A.D. 600–900). By contrast, in the work presented here, the authors’ analysis of a longer sediment core demonstrates that forest cover increased from A.D. 400 to A.D. 900, with arboreal pollen accounting for 59.8–71.0% of the pollen assemblage by approximately A.D. 780–980. The highest levels of deforestation are found about 900 B.C. when, at its peak, herb pollen made up 89.8% of the assemblage. A second, although less pronounced, period of elevated deforestation peaked at approximately A.D. 400 when herb pollen reached 65.3% of the assemblage. The first deforestation event likely coincided with the widespread adoption of agriculture, a pattern found elsewhere in Mesoamerica. The second period of forest clearance probably was associated with the incursion of Maya speakers into the Copan Valley and their subsequent construction of the earliest levels of the Copan Acropolis. These results refute the former hypothesis that the ancient Maya responded to their increasingly large urban population by exhausting, rather than conserving, natural resources.



        • archaeology
        •  
        • Mesoamerica
        •  
        • historical ecology
        •  
        • sustainability
        • palynology
        Footnotes
      • 1To whom correspondence should be addressed. E-mail:cameron.mcneil@lehman.cuny.edu.
      • Author contributions: C.L.M. designed research; C.L.M. performed research; C.L.M., D.A.B., and L.P.B. analyzed data; and C.L.M. wrote the paper.
        The authors declare no conflict of interest.
      • This article is a PNAS direct submission.
      • See Commentary on page 953.
      • This article contains supporting information online at www.pnas.org/cgi/content/full/0904760107/DCSupplemental.
      • * The pollen spectrum of the 155-cm level is distinctly different from that of other sections of the sediment core. In this level, 16.1% of the pollen remains unidentified, and Mimosa spp. pollen accounts for 18.6% of the terrestrial pollen assemblage. Comparison of this grain with samples ofMimosa spp. pollen from Mesoamerica has led to the determination that it is likely to be Mimosa albida Humb. & Bonpl. ex Willd., a shrub.
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        PDF grátis deste artigo aqui.