The area west of Makassar Strait, sometimes …
Years: 7101BCE - 6958BCE
The area west of Makassar Strait, sometimes called Sundaland, encompasses the areas of the Asian continental shelf that was exposed during the last ice age.
It includes the Malay Peninsula on the Asian mainland, the large islands of Borneo, Java, and Sumatra, and their surrounding islands.
It consists of a web of watered plains, because the seas have been some one hundred and fifty feet, or fifty meters, lower than they are now.
The stone tools used by hunting and gathering societies across Southeast Asia during this period of lowered sea levels show a remarkable degree of similarity in design and development.
Some scholars (e.g., Oppenheimer) locate the origin of the Austronesian languages in Sundaland and its upper regions.
Genetic research reported in 2008 indicates that the islands, which are the remnants of Sundaland, were likely populated as early as fifty thousand years ago.
The sea levels rise in about 7000 BCE to form the islands of Sundaland, home to many Asian mammals including elephants, monkeys, apes, tigers, tapirs, and rhinoceros.
Locations
Topics
- Neolithic Revolution
- Boreal Period
- Neolithic Subpluvial, or Holocene climatic optimum, or Holocene Wet Phase
