These

examples show the complexities of managing forests and the likelihood of persisting forest refugia in the context of changing agricultural populations. Soil loss associated with deforestation and erosion this website was one of the most consequential environmental impacts associated with population expansion in the Maya lowlands. Excavations in over 100 localities (e.g., karst depressions, lakes) indicate increased erosion regionally between 1000 BC and AD 250 (Preclassic Period) and again between AD 550 and 900 (Late Classic; Beach et al., 2006). Increased erosion in lake basins of the Petén between 1000 BC and AD 900 is represented by a massive detrital unit designated the “Maya Clay” (Deevey et al., 1979, Anselmetti et al., 2007 and Mueller et al., 2009) that is highly reflective seismically and distinctive BIBF 1120 in vitro from sediments (organic-rich gyttja) above and below (Anselmetti et al., 2007). Sedimentation rates were high throughout this interval and highest between 700 BC and AD 250 (Anselmetti et al., 2007 and Mueller

et al., 2009). Terraces were used throughout the region to mitigate erosion (Fig. 3) and stabilized some areas prior to the Late Classic Period (Caracol, Murtha, 2002). It is during this period (400 BC–AD 250) that increased sedimentation rates transformed many of the perennial wetlands and shallow lakes into seasonal swamps across the Maya lowlands (Dunning et al., 2002). Many of these hydrological changes were detrimental because they altered recharge and increased eutrophication in shallow seasonal wetlands (Dunning et al., 2012), but deeper and moister soils along the margins of wetlands and rivers provided opportunities for agricultural intensification during the Classic Period,

as did floodplain sediments once sea-level stabilized and facilitated the expansion of wetland field agricultural systems (Beach et al., 2009, Luzzadder-Beach et al., 2012, Siemens and Puleston, 1972, Turner, 1974 and Turner and Harrison, 1981) or modest alteration of naturally occurring dry locations in pericoastal wetlands (Antonie et al., 1982 and Pohl et al., 1996). The widespread collapse of Classic Maya polities between AD 800 and 1000 was messy and multicausal. There are no simple explanations, and the complex processes involved require analysis as Depsipeptide datasheet a coupled natural and human system (Scarborough and Burnside, 2010 and Dunning et al., 2012). Indeed, the “collapse” may be better characterized as a major societal reorganization (McAnany and Gallareta Negrón, 2010), because Maya populations and some cultural traditions (e.g., writing and a derivative calendar) persisted through the Postclassic Period and conquest (AD 1000–1520). The Classic Maya collapse was first and foremost a political failure with initial effects on the elite sector (kings and their courts) that ultimately undermined the economy and stimulated the decentralization of Maya civic-ceremonial centers and the reorganization of regional populations.