Jl. Prado et Mt. Alberdi, The mammalian record and climatic change over the last 30,000 years in thePampean Region, Argentina, QUATERN INT, 57-8, 1999, pp. 165-174
A changing pattern of mammal distribution in response to climatic variation
s is proposed. It is based on mammal records from archaeological and palaeo
ntological sites of late Pleistocene-Holocene age. We hypothesize that majo
r faunistic changes may be linked to climatic events, and consequently we c
ompare the distribution of the most climate-sensitive mammals with models b
ased on isotopic and pollen analyses. The lower part of the Lujan Formation
, dated to ca. 30,000 yr BP (brown zone of the Guerrero Member), is represe
nted by a mammal community that indicates a warm and humid environment. The
interval between 28,000 and 13,000 yr BP is characterized by mammals adapt
ed to cold and dry habitats. A transition from temperate and semi-arid to m
ore humid conditions occurred between 12,000 and 8500 yr BP. From 9000 to 7
500 yr BP, the faunal record reveals a dry episode. Between 7500 and 5000 y
r BP, mammals reflect a humid climate. Mammal communities from the Late Hol
ocene indicate a predominantly humid environment, with some arid phases. (C
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