Journal of Paleolimnology

, Volume 33, Issue 1, pp 53–71 | Cite as

The use of sedimentary algal pigments to infer historic algal communities in Lake Apopka, Florida

  • Matthew N. Waters
  • Claire L. Schelske
  • William F. Kenney
  • Andrew D. Chapman
Article
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Abstract

The primary producer community of Lake Apopka, a large (125 km2), shallow (mean depth, 1.7 m), polymictic Florida lake, shifted from macrophyte dominance to phytoplankton dominance in the 1940s. Today, frequent wind resuspension of highly organic, unconsolidated sediments supports a meroplanktonic community that is predominantly diatoms, but during calm periods the algal community is dominated by planktonic cyanobacteria. Sedimentary algal pigments (chlorophyll derivatives and carotenoids) and chemical proxies for nutrient enrichment (polyphosphate, total phosphorus and biogenic silica) in three sediment cores were used to investigate historic changes in primary producers. Sediments were separated into three stratigraphic zones using multivariate statistical techniques. Stratigraphic zonation was established in each core although sediment deposition at one site was insufficient to adequately resolve temporal changes. These results show the importance of selecting suitable sites for paleolimnological studies. The oldest zone represents macrophyte-derived sediments, and the two overlying zones represent phytoplankton-derived sediments deposited since the 1940s. Algal pigments in the most recent sediment zone show little degradation, which might be due to the presence of viable meroplankton in the sediment. After the initial primary producer shift from macrophytes to phytoplankton, the lake experienced a short period of cyanobacterial dominance followed by a period of benthic diatom abundance before being replaced by the present algal community consisting of cyanobacteria and meroplanktonic diatoms. Chlorophyll derivatives and carotenoids were highly correlated with total phosphorus. Historic trends inferred from the data include algal and cyanobacterial productivity that increased with increased phosphorus loading. The study demonstrates that valid paleolimnological proxies for historic eutrophication are available in loosely consolidated sediments of shallow, subtropical lakes.

Keywords

Biogenic silica Cyanobacteria Diatoms Eutrophication Phosphorus Polyphosphate 
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Copyright information

© Springer 2005

Authors and Affiliations

  • Matthew N. Waters
    • 1
    • 2
  • Claire L. Schelske
    • 1
    • 3
  • William F. Kenney
    • 1
    • 3
  • Andrew D. Chapman
    • 1
    • 4
  1. 1.Department of Fisheries and Aquatic SciencesUniversity of FloridaUSA
  2. 2.Department of Environmental Sciences and EngineeringUniversity of North CarolinaChapel HillUSA
  3. 3.Department of Geological Sciences, Land Use and Environmental Change InstituteUniversity of FloridaGainesvilleUSA
  4. 4.GreenWater Labs/BCI Engineers & Scientists, Inc.PalatkaUSA

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