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Diatom assemblages and water depth in Lake 239 (Experimental Lakes Area, Ontario): implications for paleoclimatic studies

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Abstract

Diatom assemblages in surface sediments were sampled along three transects in Lake 239, from the Experimental Lakes Area (NW Ontario), and analyzed in order to explore the relationship between modern species distributions and water depth. Approximately 170 diatom species were identified in surficial sediments at lake depths from 2 to 30 m. The species composition varied with sample depth but remained highly similar across all three transects. The main patterns of variation in the diatom assemblages across transects, derived from a detrended correspondence analysis (DCA), showed that assemblages were highly correlated (r = 0.97 to 0.98). At depths > 8 m the pattern of predominantly benthic composition changed to a planktonic assemblage dominated by Cyclotella stelligera. This depth currently corresponds to the depth of 1% light penetration as assessed from extinction coefficient measurements. Diatom species diversity increases with the switch to the near-shore benthic taxa in all three transects. Additionally, there is a large decrease in the ratio of chrysophyte scales to diatoms at depths < 8 m. Light transmission data from wet and dry periods over the last 35 years suggests that during dry periods the extent of the littoral zone should change by over 2 m. We suggest that cores along a transect from 8 to 14 m should provide a highly sensitive location for detailed paleoclimatic study.

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Authors and Affiliations

  1. Paleoecological Environmental Assessment and Research Lab (PEARL), Queen’s University, Kingston, ON, K7L 3N6, Canada

    Melissa T. Moos, Kathleen R. Laird & Brian F. Cumming

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  1. Melissa T. Moos
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  2. Kathleen R. Laird
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  3. Brian F. Cumming
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Correspondence to Melissa T. Moos.

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T. Moos, M., Laird, K. & Cumming, B.F. Diatom assemblages and water depth in Lake 239 (Experimental Lakes Area, Ontario): implications for paleoclimatic studies. J Paleolimnol 34, 217–227 (2005). https://doi.org/10.1007/s10933-005-2382-8

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  • DOI: https://doi.org/10.1007/s10933-005-2382-8

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