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Lake Zirahuen (101° 44' W, 19° 26' N), located in a volcanically active region at the boundary of the two major modern climatic systems (the intertropical convergence zone and the subtropical high pressure zone) and in a region with a history of human occupation of several thousand years, provides the opportunity to investigate climatic variations, the history of vegetation and the volcanic and anthropogenic impact in central Mexico. In this paper, we present a preliminary model of lacustrine evolution of Zirahuen Lake for the last 17000 cal yr BP, based on the analysis of vertical and lateral variations of this sedimentary deposit, using two sediment cores

Registro sedimentario de los últimos ca. 17000 años del lago de Zirahuén, Michoacán, México