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- W2103085334 abstract "Littlefield Lake is in a late stage of marl lake evolution characterized by reduced rates of carbonate precipitation. Long and short term carbonate budgets show that the volume of calcite in the lake basin is 3–7 times that expected from annual calcium depletion in the epilimnetic water. This Holocene decrease in carbonate production is also recorded as a gradual increase in the amount of organic and carbonate material in cores from the deep lake basin. Late-stage reduction in carbonate production is evidently a natural consequence of lakeward progradation of littoral marl benches, encroachment of terrestrial vegetation, and reduced colonization by carbonate-producing lake macrophytes." @default.
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- W2103085334 date "1986-11-01" @default.
- W2103085334 modified "2023-09-26" @default.
- W2103085334 title "Littlefield Lake, Michigan: Carbonate budget of Holocene sedimentation in a temperate-region lacustrine system1" @default.
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- W2103085334 doi "https://doi.org/10.4319/lo.1986.31.6.1301" @default.
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