The Geography of MammalsK. Paul, Trench, Trübner & Company, Limited, 1899 - 335 páginas |
Dentro del libro
Página 15
... Pliocene period . This shows , we think , very conclusively that what small resemblance there is between the mammals of the Oriental and Ethio- pian Regions is due rather to a similarity in their origin , than to any sort of direct ...
... Pliocene period . This shows , we think , very conclusively that what small resemblance there is between the mammals of the Oriental and Ethio- pian Regions is due rather to a similarity in their origin , than to any sort of direct ...
Página 35
... pliocene or pleistocene fauna may be expected . As in South America , these extinct animals appear in many cases to have attained a size far surpassing that of their degenerate descendants . None of the remains hitherto found in ...
... pliocene or pleistocene fauna may be expected . As in South America , these extinct animals appear in many cases to have attained a size far surpassing that of their degenerate descendants . None of the remains hitherto found in ...
Página 61
... Pliocene times , members of this genus and its allied forms were found both in North America and also throughout the Old World from France to China . This gives us direct evidence of the former much wider extension of the family of ...
... Pliocene times , members of this genus and its allied forms were found both in North America and also throughout the Old World from France to China . This gives us direct evidence of the former much wider extension of the family of ...
Página 80
... Pliocene . Finally , the later Pliocene is apparently represented by the Pampas " formation of Argentina and Uruguay . Our knowledge of the extinct mammal - faunas of these beds is mainly due to the efforts of the Argentine ...
... Pliocene . Finally , the later Pliocene is apparently represented by the Pampas " formation of Argentina and Uruguay . Our knowledge of the extinct mammal - faunas of these beds is mainly due to the efforts of the Argentine ...
Página 82
William Lutley Sclater, Philip Lutley Sclater. 50 PLATE 111 . 20 REGIONS . period . At the beginning of Pliocene time , during. 30 713 AZILDAN ION 80 10 O 20 10 10 30 40 60 ION VAXJalusten Hoberg & Ima.
William Lutley Sclater, Philip Lutley Sclater. 50 PLATE 111 . 20 REGIONS . period . At the beginning of Pliocene time , during. 30 713 AZILDAN ION 80 10 O 20 10 10 30 40 60 ION VAXJalusten Hoberg & Ima.
Otras ediciones - Ver todas
Términos y frases comunes
Africa animals Ant-eater Antarctic Antelopes Arctatlantis Arctic Armadilloes Asia Atlantic Australian Region Bats beds belong Borneo boundary Bovida Cape Carnivora Celebes Cetaceans Chimpanzee Chiroptera closely allied coast confined considerable number contains Deer distinct districts Eastern Edentates endemic Ethiopian Region Europe existing extends extinct fauna forests forms genera genus geographical distribution greater number Indian Sub-region inhabitants Insectivores islands known Lemurs Macacus Madagascar mainland Malagasy Malagasy Sub-region Malay Peninsula Malayan MAMMAL-FAUNA mammalian mammals Marsupials Monkeys Monotremes mountains naturalists Nearctic Region nearly Neotropical Region North northern number of genera number of species occur Ocean Old World Opossum Order Oriental Region Otaria Pacific Palearctic Region Papuan Sub-region Patagonia peculiar genera Phalanger Phocida Pinnipeds Pliocene present range recent remarkable represented Rodents Sea-regions SECTION Shrews single species Sirenian South America Southern Squirrels Sub-family Sumatra SUMMARY AND DEDUCTIONS Tapirs three genera total number tropical Ungulata Ungulates Viverride Western whole widely distributed