For GDB1 and GDB3 however, the number of multi-grain measurements is low (n = 6 and 5 respectively) and the calculated CAM De s might not be significant because of the scatter in these samples.
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Across the Gap: Geochronological and Sedimentological Analyses from the Late Pleistocene-Holocene Sequence of Goda Buticha, Southeastern Ethiopia.
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