|
Eisenmann V,. (1982). Le cheval: Passé, présent et avenir. Bull Inf Mus Nat Hist Naturelle, 30, 29–34.
|
|
Ewart Jc,. (1903). The wild horse. Nature, 68, 271–274.
|
|
Fedak Ma, S. H. (1979). Reappraisal of energetics of locomotion shows identical cost in bipeds and quadrupeds including ostrich and horse. Nature, 282, 713–716.
|
|
Hoyt Df, T. C. (1981). Gait and the energetics of locomotion in horses. Nature, 292, 239–240.
|
|
Pocock Rj,. (). The coloration of the Quaggas. Nature, 68, 356–357.
|
|
Welsh Da,. (1973). The life of Sable Island's wild horses. Nature Canada, 2, 7–14.
|
|
Goodall J. (1964). Tool-using and aimed throwing in a community of free-living chimpanzees. Nature, 201, 1264.
|
|
Sugiyama Y. (1994). Tool use by wild chimpanzees. Nature, 376, 327.
|
|
OUSTALET E. (1882). Une nouvelle espèce de zèbre,. La Nature, 10, 12–14.
|
Marean, C. W., & Gifford-Gonzalez, D. (1991). Late Quaternary extinct ungulates of East Africa and palaeoenvironmental implications. Nature, 350(6317), 418–420.
Abstract: UNGULATE communities of two East African savannas, the Serengeti and Athi-Kapiti Plains, are dominated by wildebeest (Connochaetes taurinus) supplemented by zebra (Equus burchelli), topi (Damaliscus lunatus), hartebeest (Alcelaphus buselaphus), buffalo (Syncerus caffer) eland (Taurotragus oryx) and gazelles (Gazella grand and G. thomsoni)1-3. Before this research, little was known of East African large mammal communities in the Late Pleistocene and early to middle Holocene. We document an extinct impala-sized alcelaphine antelope that is numerically dominant in Late Pleistocene archaeofaunal assemblages from the Athi-Kapiti Plains. The extinct giant buffalo Pelorovis antiquus is present, and a number of arid-adapted regionally extinct species are common. The small alcelaphine is rare in northern Tanzania, but regionally extinct arid-adapted species are present in Late Pleistocene deposits. These data indicate that as recently as 12,000 years ago, the large mammal community structure of East African savannas was very different and dry grasslands and arid-adapted ungulates expanded at least as far south as northern Tanzania during the Last Glacial Maximum.
|
