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These subAndean moist forests are bound by the Andes to the west and the Ucayali River to the east – both of which are formidable barriers to the dispersal of many species. The northern delineation follows the transition of the distinct flooded várzea forests of the Marañon River, and the linework for this section originated from LANDSAT imagery. The northernmost finger of these lowland forests extends into the Cenepa River Valley to the montane forest transition. Southern linework follows the extension of the Andean Cordillera to where it meets the confluence of the Tambo River and Urubamba River – thus forming the Ucayali. We have differentiated this ecoregion from the surrounding lowland forests due to species endemism, particularly butterfly (Brown 1987) due to its current (interfluvial and montane) and past isolation as a Pleistocene refuge (Prance 1987). Delineation of this ecoregion and linework for the montane transition areas follow the Instituto Geográfico Nacional (1987) map classification of "Amazonian tropical forest".
Instituto Geográfico Nacional. 1987. Ecoregiones del Peru. Map 1:5,000,000. Atlas del Peru, Lima, Peru. Prance, G. 1987. Phytogeographic support for the theory of Pleistocene forest refuges in the Amazon Basin, based on evidence from distribution patterns in Caryocaracaceae, Chrysobalanaceae, Dichapetalaceae, and Lecythidaceaea. Acta Amazonica 3. Pp 5-28. Brown, K.S. 1987. Biogeography and evolution of Neotropical Butterflies. Pages 66-104 in T. Whitemore, and G. Pranceeditors, Biogeography and Quaternary History in Tropical America. Oxford Science Publications. Reviewed by: In process For more general information on this ecoregion, go to the WildWorld version of this description. All text by World Wildlife Fund © 2001 | |