EARLY DISPERSAL OF MAN ON ISLANDS OF THE INDONESIAN ARCHIPELAGO - FACTS AND CONTROLS

Citation
F. Aziz et al., EARLY DISPERSAL OF MAN ON ISLANDS OF THE INDONESIAN ARCHIPELAGO - FACTS AND CONTROLS, Anthropological science, 103(4), 1995, pp. 349-368
Citations number
65
Categorie Soggetti
Anthropology
Journal title
ISSN journal
09187960
Volume
103
Issue
4
Year of publication
1995
Pages
349 - 368
Database
ISI
SICI code
0918-7960(1995)103:4<349:EDOMOI>2.0.ZU;2-6
Abstract
Sea barriers are an effective means of limiting the dispersal of terre strial vertebrates. Fossil evidence shows, however, that land mammals have colonized islands. The island faunas are impoverished, and from t he faunal composition it can be learned that only large mammals with g ood swimming and/or floating capacities could settle on these islands. Such mammals include elephants, deer, and hippos. In some cases paleo ecological conditions on islands have led to the development of faunas with dwarf species. It is generally accepted that man was established on islands in the Neolithic. There is, however, an increasing amount of evidence that in some cases, migration of hominids across sea barri ers initially occurred much earlier. The presence of flowery Palaeolit hic industry on Sardinia (Italy) points to a Middle Pleistocene coloni zation of this island. Other islands in the Mediterranean, like Crete and Cyprus, were colonized only in the Neolithic. This proves that the distance of the island to the coast of the mainland was not the only limiting factor on colonization of islands by early Man. Other factors such as food supply also play a role. On Sardinia a hare-like mammal Prolagus existed. This animal had a high reproduction rate and could h ave served as a continuous food supply for a hunter-gatherer populatio n. On the islands of S.E. Asia we find giant rats. These mammals could have served as a food supply for Palaeolithic Man. On Flores artifact s are found in association with a Middle Pleistocene fauna. Palaeontol ogical evidence shows a faunal turnover in the Middle Pleistocene on b oth Sardinia (Italy) and Flores (Indonesia).