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• W2108539917 abstract "Research Article| October 01, 2007 Quantification of soil erosion rates related to ancient Maya deforestation Flavio S. Anselmetti; Flavio S. Anselmetti 1Geological Institute, Swiss Federal Institute of Technology, ETH, 8092 Zurich. Switzerland Search for other works by this author on: GSW Google Scholar David A. Hodell; David A. Hodell 2Department of Geological Sciences, University of Florida, Gainesville, Florida 32611, USA Search for other works by this author on: GSW Google Scholar Daniel Ariztegui; Daniel Ariztegui 3Section of Earth Sciences, University of Geneva, 1205 Geneva, Switzerland Search for other works by this author on: GSW Google Scholar Mark Brenner; Mark Brenner 4Department of Geological Sciences, University of Florida, Gainesville, Florida 32611, USA Search for other works by this author on: GSW Google Scholar Michael F. Rosenmeier Michael F. Rosenmeier 5Department of Geology and Planetary Sciences, University of Pittsburgh, Pittsburgh, Pennsylvania 15260, USA Search for other works by this author on: GSW Google Scholar Geology (2007) 35 (10): 915–918. https://doi.org/10.1130/G23834A.1 Article history received: 26 Feb 2007 rev-recd: 21 May 2007 accepted: 25 May 2007 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Flavio S. Anselmetti, David A. Hodell, Daniel Ariztegui, Mark Brenner, Michael F. Rosenmeier; Quantification of soil erosion rates related to ancient Maya deforestation. Geology 2007;; 35 (10): 915–918. doi: https://doi.org/10.1130/G23834A.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract We used seismic and sediment core data to quantify soil erosion rates for the past ∼6000 yr in the closed catchment of Lake Salpetén, in the tropical lowlands of northern Guatemala. The region was affected by ancient Maya land use from before ca. 1000 B.C. to A.D. 900. This period of human impact coincided with deposition in the lake of a detrital unit (Maya Clay) as much as 7 m thick that contrasts sharply with the relatively organic-rich gyttja deposited both before and after Maya occupation of the watershed. The greatest soil loss, with mean sustained values of ∼1000 t/km2yr−1, occurred in the Middle and Late Preclassic Periods (700 B.C. to A.D. 250), associated with relatively low Maya population densities. Soil erosion slowed during the period of maximum population density in the Late Classic Period (A.D. 550–830), indicating a decoupling between human population density and soil erosion rate. The most rapid soil loss occurred early during initial land clearance, suggesting that even low numbers of people can have profound impacts on lowland tropical karst landscapes. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2108539917 title "Quantification of soil erosion rates related to ancient Maya deforestation" @default.
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