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- W1965497303 abstract "In south-central Chile, the Río Ignao nonglacial deposit with a minimal radiocarbon age of 56,000 +2000, −1700 yr shows the following sequence of pollen assemblages, starting with the oldest: Gramineae (zone 1), Gramineae- Corynabutilon-Lomatia-Ovidia (zone 2), Nothofagus-Embothrium -Gramineae (zone 3A), Nothofagus -Gramineae-Tubuliflorae (zone 3B and D), and Nothofagus-Drimys -Myrtaceae (zone 3A). This sequence implies an initial dry and rather cold climate that later became wetter and somewhat warmer, reached a warm peak, and ultimately became colder and drier. At the warmest time, the Andean tree line is estimated to have been about 900 m lower and average January (summer) temperature about 3–4°C colder than at present. The Río Ignao deposit is believed to represent an early interstade of the last glaciation, known in southern Chile as the Llanquihue Glaciation." @default.
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- W1965497303 date "1976-06-01" @default.
- W1965497303 modified "2023-09-26" @default.
- W1965497303 title "Palynology and Depositional Environment of the Río Ignao Nonglacial Deposit, Province of Valdivia, Chile" @default.
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- W1965497303 doi "https://doi.org/10.1016/0033-5894(76)90054-5" @default.
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