Decadally resolved lateglacial radiocarbon evidence from New Zealand Kauri
The Last Glacial-Interglacial Transition (LGIT; 15,000-11,000 cal BP) was characterized by complex spatiotemporal patterns ofclimate change, with numerous studies requiring accurate chronological control to decipher leads from lags in global paleoclimatic, -environmental and archaeological records....
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| Aineistotyyppi: | Journal article |
| Julkaistu: |
Cambridge University Press
2016
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