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University of California Press and AmericanOrnithologists' Union are collaborating with JSTOR to digitize, preserve and extend access to Ornithological Monographs.ABSTRACT. The distribution of Andean wetland habitats in the Pleistocene and present is reviewed and considered in relation to the known distribution of waterbirds. Analysis based on suture zones, disjunctions, core areas for endemic taxa, and phylogenetic relationships suggests evolutionary processes closely tied to events in the Pleistocene. The distributions of species that prefer barren habitats suggest a center of origin in the glacial Lake Michin on the Bolivian Altiplano. Other glacial refugia that gave rise to new taxa were Lake Atacama in Chile, Lake Junin in Peru, and the large lakes that previously were present in the Bogota area, Colombia. Semi-open refugia along the Andean slopes had slight evolutionary significance. The inhabitants of Andean marsh habitats are generally poorly differentiated, morphologically, from lowland counterparts, and most probably they immigrated to the area in postglacial time. The colonization of the Andes was almost unidirectional, from the southern lowlands, which has resulted in a strong northward reduction of taxa adapted to barren habitats. The previous lakes of the Bogota area received propagules from other directions, including from North America, but the many marsh birds in this area have not shown adaptive shifts in response to vacant niches in barren habitats.RESUMEN. Se revee la distribucion de los habitats pantanosos de los Andes tanto durante el pleistoceno como en la actualidad y se los considera en relaci6n con la distribucion conocidas de aves acuaticas. Analisis basados en zonas de sutura, disjunci6n, areas centrales para grupos taxon6micos endemicos y relaciones filogeneticas, sugieren procesos de evolution cercanamente relacionados con sucesos del pleistoceno. La distribuci6n de especies que prefieren habitats esteriles hace suponer que el lago glacial Michin, en el altiplano boliviano, ha sido el centro de origen (de las mismas). Otros refugios glaciales, como el lago de Atacama en Chile, la laguna de Junin en Peru y los grandes lagos que se encontraban anteriormente en el area de Bogota, Colombia, tambien brindaron origen a nuevos grupos taxon6micos. Refugios semidescubiertos en las laderas de los Andes tienen escaso significado a nivel de evoluci6n. Los habitantes de los habitats pantanosos andinos generalmente presentan pocas diferencias morfologicas respecto a sus contrapartes en las tierras bajas, y probablemente han emigrado hacia el area luego de la 6poca glacial. La colonizaci6n de los Andes fue casi unidireccional desde las tierras bajas del sur, lo cua...