Oxygen isotopes in fresh water biogenic opal ‐ Northeastern US Alleröd‐Younger Dryas temperature shift

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Abstract
The first oxygen isotope analysis of biogenic opal from lake sediments, from the Alleröd/Younger Dryas transition in a core from Linsley Pond, Connecticut, gives an average estimate of a 6°C drop in temperature during the Younger Dryas. This shift represents temperatures during the bloom season, and may be less than the winter temperature drop. The sharp transition itself, with a duration of about 200 years, suggests that the temperature decrease may have been as large as 12°C. Previous estimates of the Alleröd/Younger Dryas temperature shifts are controversial, and range from 3–20°C, suggesting that further interdisciplinary research on the same samples is warranted.