Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Parmularius"'
Autor:
Haruo Saegusa, Berhane Asfaw, Shigehiro Katoh, Hideo Nakaya, Reiko T. Kono, Gen Suwa, Yonas Beyene, Awoke Amzaye
Publikováno v:
Journal of Vertebrate Paleontology. 23:901-916
Mammalian fossils of the Konso Formation (southwestern Main Ethiopian Rift) derive from stratigraphic intervals dated to between 2.0 Ma and younger than 1.3 Ma. Systematic paleontological collecting resulted in almost 8,000 identifiable mammalian spe
Autor:
Lillian M. Spencer
Publikováno v:
Journal of Human Evolution. 32:201-228
Detailed reconstructions of vegetation structure are critical to understanding morphological and behavioral adaptations of Plio-Pleistocene African hominids, Savanna grassland habitats are often postulated as being influential in the evolution of man
Publikováno v:
Journal of Vertebrate Paleontology
Journal of Vertebrate Paleontology, Society of Vertebrate Paleontology, 2001, 21 (2), pp.335-346
Scopus-Elsevier
Journal of Vertebrate Paleontology, Society of Vertebrate Paleontology, 2001, 21 (2), pp.335-346
Scopus-Elsevier
International audience; The Australopithecus-bearing sites of Koro Toro in central Chad yielded at least 9 species of bovids (Ruminantia: Bovidae). They all belong to genera found in North and/or East Africa, but three new species are named. Kobus ko
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::577692ea371ad94eee30ae77247a66dd
https://shs.hal.science/halshs-00068080
https://shs.hal.science/halshs-00068080
Autor:
E. S. Vrba
Publikováno v:
Biological Journal of the Linnean Society. 11:207-228
Cladistic principles are applied to a group of antelope species, three-quarters of which are extinct. Only cranial and mandibular characters are used. The present phylogenetic hypothesis suggests diat the Alcelaphini are monophyletic; that the genera
Autor:
William G. Chaloner, M.C. Boulter
Publikováno v:
Review of Palaeobotany and Palynology. 10:61-78
This is a preliminary account of the fossil plants which occur in the uppermost clays infilling the sink holes in the limestone of the Southern Pennines of Derbyshire, England. The plants are of Late Tertiary age, most probably Pliocene, and are of m