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- W2071931475 abstract "Six new radiocarbon ages and a pollen sequence are provided for Laguna Stibnite, a small lake on the Taitao Peninsula, Chile (latitude 46°25'S, longitude 74°24'W). The sediments record a late-glacial to present sequence, with a basal age of 14 335 ± 145 yr BP (Q-2840). The radiocarbon ages provide the basis for a sound chronology in a region of Chile where few palynological studies have been made and where previous radiocarbon ages are ambiguous. The chronology from Laguna Stibnite supports the acceptance of a radiocarbon chronology based on wood fragments (rather than bulk analysis) at a site near Puerto Edén further south in the Chilean Channels (49°08'S). These data from Laguna Stibnite provide evidence for an early deglaciation (before 14 000 yr BP) in this region of southern Chile. The sequence provides no evidence for a climatic reversal between 11 000 yr BP and 10 000 yr BP, the so-called Younger Dryas chron." @default.
- W2071931475 created "2016-06-24" @default.
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- W2071931475 date "1993-01-01" @default.
- W2071931475 modified "2023-10-06" @default.
- W2071931475 title "Late quaternary chronology of the Taitao Peninsula, southern Chile" @default.
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- W2071931475 doi "https://doi.org/10.1002/jqs.3390080208" @default.
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