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Regional continuity in Australasian Pleistocene hominid evolution
American Journal of Physical Anthropology
|July 1, 1981
Summary
Fossil analysis of Homo erectus Sangiran 17 suggests regional continuity in Australasia during the Pleistocene. This finding supports a dynamic model of gene flow and selection maintaining regional variation in ancient human populations.
Area of Science:
- Paleoanthropology
- Human Evolution
- Pleistocene Archaeology
Background:
- The Indonesian Homo erectus specimen Sangiran 17 provides crucial insights into early human populations.
- Understanding regional morphological variation is key to reconstructing hominid dispersal and evolution.
Purpose of the Study:
- To reconstruct the Indonesian Homo erectus specimen Sangiran 17.
- To investigate regional morphological continuity in Australasia during the middle and late Pleistocene.
- To compare Sangiran 17 with other hominid specimens, such as those from Kow Swamp, Australia.
Main Methods:
- Reconstruction of the Sangiran 17 Homo erectus specimen.
- Comparative morphological analysis with late Pleistocene hominid specimens from Kow Swamp.
- Application of the "center and edge" hypothesis and a dynamic model of geneflow and selection.
Main Results:
- The Sangiran 17 specimen exhibits features suggesting regional morphological continuity in Australasia.
- A morphological clade is identified through comparison with Kow Swamp males.
- The "center and edge" hypothesis and geneflow models explain regional variation and clinal equilibrium.
Conclusions:
- Regional morphological continuity existed in Australasia during the middle and late Pleistocene.
- A dynamic interplay of geneflow and selection likely maintained long-standing clinal equilibria in ancient hominid populations.
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