“…Today the region receives between 900 and 1,250 mm of rainfall per year, supporting diverse vegetation communities (42) (fir and pine, 2,500-3,300 m asl, pine and oak; Ͻ2,500 m asl, agricultural crops, grasses, and secondary vegetation). Extensive paleoenvironmental research within the Pátzcuaro Basin provides a record of landscape change throughout the Holocene (13,19,41,(43)(44)(45)(46)(47)(48)(49)(50) including three episodes of landscape instability: Unit II, 3,600-2,800 B.P. ; Unit IV, 2,500-1,200 B.P.…”