Cladoceran and diatom evidence of lake-level fluctuations from a Finnish lake and the effect of acquatic-moss layers on microfossil assemblages

We studied Holocene lake-level fluctuations from a small lake, Iso Lehmälampi, southern Finland, utilizing cladoceran and diatom analyses. We report data from a sediment core (A) taken from the deepest part of the lake (8.1 m) where two layers of moss, mixed with gyttja, were found. These layers wer...

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Veröffentlicht in:Journal of paleolimnology 1999-10, Vol.22 (3), p.277-290
Hauptverfasser: Sarmaja-korjonen, Kaarina, Alhonen, Pentti
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Sprache:eng
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