Lama Guanicoe (Muller, 1776) body size in continental Patagonia and Tierra del Fuego

被引:6
|
作者
L'Heureux, Gabriela Lorena [1 ]
Fernandez, Jimena Cornaglia [2 ]
机构
[1] CONICET IMHICIHU, Buenos Aires, DF, Argentina
[2] FHumyAr UNR, Rosario, Argentina
关键词
Guanaco; Osteometry; Body size; Environmental variables; Latitudinal gradient; Bergmann's rule; South America; BERGMANNS RULE; ISLAND RULE; MAMMALS; POPULATIONS; EVOLUTION; GUANACOS;
D O I
10.1016/j.geobios.2015.02.007
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Lama guanicoe (Muller, 1776) is one of the most important South American large mammal species for both biologists, ecologists and archaeologists, and body size of modern and prehistoric populations of guanaco has been one of the most studied parameters. In this paper, we evaluate the latitudinal differences in body size of different modern populations of guanaco from Argentinean Patagonia based on osteometric data of their long bones. The osteological sample is made of 110 fully-fused individuals drawn from three different guanaco populations from continental and insular Patagonia covering the latitudinal interval from S40 degrees to S54.5 degrees. Quantitative data for the four long bones selected are analyzed with univariate and multivariate parametric statistical techniques. Apparently consistent with Bergmann's rule, results show that guanaco specimens from S53-54.5 degrees are bigger on average than those from S48-52 degrees which are, in turn, bigger than those from S40 degrees. We observe a high and significant covariation between different environmental variables (maximum .temperature, net primary production, and winter precipitation) and body size of the guanaco populations. Nevertheless, when the temporal factor is incorporated into the analysis of this geographical gradient of body size the scenario becomes more complex. We conclude that the current clinal pattern observed in Patagonia is the result of several microevolutionary and biogeographic processes related to an adjustment of body size to different environmental and ecological drivers and to the consequences of isolation in Tierra del Fuego that occurred around the Pleistocene-Holocene transition. (C) 2015 Elsevier Masson SAS. All rights reserved.
引用
收藏
页码:239 / 248
页数:10
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