Late quaternary turnover of mammals in Borneo: the zooarchaeological record
The Quaternary has been a period of repeated, oscillating patterns of climate change. Global fluctuations in sea level affected the island status of Borneo, which was probably joined to continental Asia for more than half of the last 250,000 years. Alternating connection and isolation, coupled with...
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Veröffentlicht in: | Biodiversity and conservation 2010-02, Vol.19 (2), p.373-391 |
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