Abstract

Northern lakes, for which we have little long-term data, are predicted to experience profound impacts with greenhouse warming. In order to assess the usefulness of chrysophytes as paleoenvironmental indicators, stomatocysts were enumerated from the surface sediments of 51 Alaskan lakes distributed along a strong climatic gradient. A total of 142 cyst morphotypes were described using light microscopy, of which 13 are believed to be new forms. Principal components analysis of the stomatocyst assemblages showed a limited amount of variation (Λ1= 0.11, Λ2= 0.09). However, redundancy analysis identified total phosphorus (TP), sodium (Na), and altitude (ALT) as significant variables in terms of their ability to describe the distribution of stomatocysts. Major ion and nutrient concentrations were also found to be strong predictors of diatom variation from the same lake set. In comparison to the diatom assemblages from the same lakes, the cysts were less abundant and showed a lower amount of species variation. Reasons for the lack of variation may be due to the predominance of unornamented and collective category cysts (i. e. cysts which cannot be differentiated under the light microscope).

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