Kienel: Late Weichselian to Holocene Diatom Succession in a Sediment Core
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Figure 3A: Relative abundance of euplanktonic diatom taxa - Lama Lake PG IIII (NE Norilsk, W Siberia),
distinctive maximum of C. ocellata (*), unique in the sequence and associated with frequent
Aulacoseira subarctica (*), marked DAZ-4, From DAZ-S to DAZ-8, Cyclotella comensis
dominated the assemblages, C. radiosa (*) became frequent in co-occurrence with Aulacoseira
islandica only in DAZ-S, In DAZ-6, Cyclotella comensis showed the highest abundance in the
sequence, though strongly fluctuating, A uniform ratio of taxa in the planktonic group (mainly
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Figure 3A: Relative abundance of euplanktonic diatom taxa - Lama Lake PG IIII (NE Norilsk, W Siberia),
distinctive maximum of C. ocellata (*), unique in the sequence and associated with frequent
Aulacoseira subarctica (*), marked DAZ-4, From DAZ-S to DAZ-8, Cyclotella comensis
dominated the assemblages, C. radiosa (*) became frequent in co-occurrence with Aulacoseira
islandica only in DAZ-S, In DAZ-6, Cyclotella comensis showed the highest abundance in the
sequence, though strongly fluctuating, A uniform ratio of taxa in the planktonic group (mainly
