Abstract
In the rainshadow of the Andean Cordillera in northern Patagonia (ca 39° to 43°S) the steep west-to-east decline in precipitation is reflected by a dramatic gradient from rainforest through open woodlands to shruband bunchgrass-dominated steppe. A recent trend towards aridification of Patagonia and consequent westward expansion of xeric communities into the western rainforest district has been a persistent theme in the ecological literature for nearly 50 years. Specifically, it has been suggested that the xeric trees Austrocedrus chilensis and Nothofagus antarctica are extending their ranges westward and replacing the mesic Nothofagus dombeyi which dominates the rainforests. This hypothesis was investigated by analyzing stand age structures and patterns of tree radial growth along a west-to-east gradient of post-fire stands dominated by Nothofagus dombeyi and Austrocedrus chilensis.
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