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occurred. Evidence of this event is obvious in the Kiliman-
jaro record (Figure 2c) as a sharp but short-lived depletion in
18 O, which suggests an abrupt and extreme cooling episode
[Thompson et al., 2002]. Evidence for this abrupt change is
also seen in numerous climatic, biological, and archeological
records from around the world, including several from the
tropics [Staubwasser and Weiss, 2006]. Many tropical paleo-
climate records, especially those located in the African/Asian
Figure 2
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