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- W1601785637 abstract "A varve chronology extending back to 1900 with dated stratigraphic markers has been established for deep-water sediment in the northern part (neck) of meromictic Fayetteville Green Lake and correlated to a similar chronology established earlier in the deeper southern end of the lake (main basin). Precise estimates of net annual varve sedimentation rates are given for each year between 1938 and 1977 for the neck. These rates are 27% higher than those previously reported in the main basin and range between 454 and 1090 g m−2 yr.−1. Varve sedimentation rates have significantly increased throughout the lake during the last 30 years with no changes in the relative ratio of varve sedimentation rates in the neck and the main basin although there is considerable year-to-year variation in this ratio. Higher varve sedimentation rates occur in shallower portions of the permanently stratified water, probably because resuspension is unlikely in this low-energy environment. Because of basin morphometry and meromixis, sediment focusing creates higher varve sedimentation rates in relatively shallow water near the upper limit of the permanently stratified water rather than in the deepest water." @default.
- W1601785637 created "2016-06-24" @default.
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- W1601785637 date "1984-05-01" @default.
- W1601785637 modified "2023-09-23" @default.
- W1601785637 title "Fayetteville Green Lake, New York, U.S.A." @default.
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- W1601785637 doi "https://doi.org/10.1016/0009-2541(84)90068-8" @default.
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