Date: February 23, 2016
Source: University of York
Researchers at the University
of York have been part of the first
comprehensive study of how Zanzibar
was formed, charting the extinction of various animals from the island.
In a collaborative project between
environmental scientists and archaeologists, a team charted the history of sea
level change by examining mangrove sediments, and conducting analysis on animal
remains found in Kuumbi
Cave -- an important
archaeological site.
Focusing on evidence from three distinct
time periods -- the end of the last Ice Age, the stage when Zanzibar became an
island 11,000 years ago, and the time of being an island -- researchers found
that numerous large mammals had disappeared by the latter stage.
Analysing over 6000 bone specimens, it
was found that large fauna such as zebra, buffalo, waterbuck and gazelle were
present in the time of island formation. However, after sea levels had risen
and the island had been inhabited by coastal cultures, they disappeared. Other
small fauna, such as porcupines and hares, were also no longer present.
Insights into sea level changes, combined
with archaeological data on the history of the island's fauna through
excavation, has never been done before in charting Zanzibar 's history. This unique
interdisciplinary approach provides a new, accurate account of the island's
prehistory and defaunation.
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