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Figure 4: Local diatom assemblage zones in compilation with lithology, chronozones and pollen assemblage
zones (* mark location of relative maximum abundances) - Lama Lake PG 1111 (NE Norilsk, W Siberia).
easily drift and occur in the plankton, The life form of such species is often described as
, tychoplanktonic' (see extensive review in Voigt, 1997),
The proportions of the life form groups (based on relative species abundances) in the diatom
assemblages, especially the ratio of euplanktonic to non-planktonic diatom taxa (Ep/Np), can be