Franke 1991 acta cong orn int christchurch

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ACTA XX CONGRESSUS INTERNATIONALIS ORNITHOLOGICI

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DISJUNCT BIRD DISTRIBUTIONS ALONG THE WEST SLOPE OF THE PERUVIAN ANDES IRMA FRANKE Museo de Historia Natural, Universidad Nacional de San Marcos, Casilla 14-0434, Lima 14, Peru

ABSTRACT. Within the steppe-like western slope ol the Peruvian Andes lores! patches (dry cloud lores!) occur lrom Ecuador to 13º8. Eight siles were studied between Huamba and Zárate. A total ol 124 taxa were used to analyze disjunctions. Species numbers decrease from N to S along a gradient of decreasing rainlall. Group 1 taxa (102 species and subspecies) occur from Ecuador south. Nine distributional limits exist. Group 2 taxa (22 species and subspecies) include endemics. Five areas of taxon replacement were identified. The major replacement area is near the Rio Santa Valley. Birds now living in dry cloud lorests along the western Andes originated north of this region. Distribution gaps have played an Importan! role in the history of the taxa. Keywords: Zoogeography, disjunction, Andes, dry cloud lorests, Peru.

INTRODUCTION

The Pacific slope of the Peruvian Andes is dominated by arid, steppe-like vegetation types. However, many small forest patches occur in this dry zone between 2400 and 3000 m, forming the richest communities of the western slope of the Peruvian Andes (Koepcke, H.W. 1961, Valencia & Franke 1980, Franke & Valencia 1984). In northern Peru these dry cloud forests occupy extensive and relatively continuous areas, but further south they occur in increasingly smaller and more isolated patches, to about 13ºS (Koepcke, H.W. 1961, Valencia 1990). These disjunct forests are thought to represent fragments of a formerly more continuous forest zone (Koepcke, M. 1958; Koepcke, H.W. 1961 ). The floristic and faunistic affinities between west slope and east slope forests, as well as the existence of low passes in northern Peru, especially the Porculla Pass (2145 m), led to the hypotheses that east slope species (1) crossed the low passes to the west, and (2) dispersed southward through the forest belt (Koepcke, M. 1958, 1961 b, Koepcke, H.W. 1961, Simpson 1975). Biogeographers accept the idea that the Andean montane forests were more continuous when depressed altitudinally during cool, humid glacial periods. At such times temperate and subtropical zones were located along less dissected lower slopes. Conversely, the upward shift of climatic zones during interglacial periods led to increasing fragmentation of montane vegetation (Haffer 1987), thus isolating bird populations and playing a role in speciation along the western Peruvian Andes.

METHODS

Field studies were made at 8 dry cloud forest sites between 2500 and 3000 m, from 4º41 'S, near the Ecuadorian border, to 11 º55'S in central Peru: (1) Huamba, Department of Piura (4º41 'S, 2900 m); (2) Chiñama, Lambayeque (6º06'S, 2550 m); (3) Llaguén, La Libertad (7º42'S, 2600 m); (4) Cochabamba, Ancash (9º27'S, 2800 m);


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