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- W150416635 abstract "Fine-interval (~29–35 14C year) diatom analysis of a sediment core from northern Lake Victoria provides a long-term context for recent environmental changes in the lake, which include increased water column stability, a switch from Aulacoseira- to Nitzschia-dominated diatom assemblages, and an overall increase in cyanobacteria relative to diatoms. The sediment record indicates that similar events have occurred abruptly and repeatedly in the lake since ~7.2 14C ka, apparently due to climatically driven disruptions of mixing regimes. Holocene fluctuations in the fossil diatom assemblages display strong periodicities (~500, ~1100, ~1400, and ~2,350~2,550 calendar year cycles) which point to global-scale forcing mechanisms. This paleolimnological record suggests that Lake Victoria and its algal communities are inherently unstable, and that future environmental and fishery management models should consider the lake’s sensitivity to climatic changes." @default.
- W150416635 created "2016-06-24" @default.
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- W150416635 date "1998-01-01" @default.
- W150416635 modified "2023-09-26" @default.
- W150416635 title "Ancient Analogues for Recent Environmental Changes at Lake Victoria, East Africa" @default.
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- W150416635 doi "https://doi.org/10.1007/978-94-017-1437-2_3" @default.
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