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Lithology, pollen, macrofossils, and stable carbon isotopes from an intermontane basin bog site in southern New Zealand provide a detailed late-glacial and early Holocene vegetation and climate record. Glacial retreat occurred before 17,000 cal yr b.p., and tundra-like grassland–shrubland occupied the basin shortly after. Between 16,500 and 14,600 cal yr b.p., a minor regional expansion of forest...
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