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walk from the sea, the lack of marine shells from early cultural deposits in this cave supports the concept that there was a substantial land shelf around the time of the Last Glacial Maximum, when estimates place sea levels at 130 m below present or possibly lower. The appearance of marine shells in middens in other caves on Lipuun Point from c. 7000 [[Before Present and especially in later periods, suggests increasing focus on marine resources in the area in general; the abandonment of the Tabon

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