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- W2038973323 abstract "Abstract Despite growing evidence for environmental oscillations during the last glacial–interglacial transition from high latitude, terrestrial sites of the North Pacific rim, oxygen-isotopic records of these oscillations remain sparse. The lack of data is due partially to the paucity of lakes that contain carbonate sediment suitable for oxygen-isotopic analysis. We report here the first record of oxygen-isotopic composition in diatom silica (δ 18 O Si ) from a lake in that region. δ 18 O Si increases gradually from 19.0 to 23.5‰ between 12,340 and 11,000 14 C yr B.P., reflecting marked climatic warming at the end of the last glaciation. Around 11,000 14 C yr B.P., δ 18 O Si decreases by 1.7‰, suggesting a temperature decrease of 3.5–8.9 °C at the onset of the Younger Dryas (YD) in southwestern Alaska. Climatic recovery began ca. 10,740 14 C yr B.P., as inferred from the increase of δ 18 O Si to a maximum of 23.9‰ near the end of the YD. Our data reveal that a YD climatic reversal in southwestern coastal areas of Alaska occurred, but the YD climate did not return to full-glacial conditions." @default.
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- W2038973323 date "2003-05-01" @default.
- W2038973323 modified "2023-09-25" @default.
- W2038973323 title "A biogenic-silica δ<sup>18</sup>O record of climatic change during the last glacial–interglacial transition in southwestern Alaska" @default.
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- W2038973323 doi "https://doi.org/10.1016/s0033-5894(03)00056-5" @default.
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