Pollen analysis of late-Holocene amberat deposits from two caves near
the forest-steppe ecotone in northern Patagonia documents a major shif
t from Austrocedrus-Nothofagus forest to steppe shrub assemblages some
time after 1800 and before 1300 BP. The probable explanation of the r
eduction of tree taxa calls for either drier summers or intensified la
nd use or a combination of both.