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Identifying sources of organic matter in sediments of shallow lakes using multiple geochemical variables

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Abstract

We analyzed 210Pb-dated sediment cores from four relatively shallow lakes (zmax < 10 m) in the Upper Ocklawaha River Basin, Florida, USA to compare primary producer community structure before and after anthropogenic impacts. We measured physical and chemical sediment variables including density, organic matter (OM), water-soluble phosphorus, polyphosphate (Poly-P), total P (TP), total carbon to total nitrogen mass ratios of OM (TC:TN), biogenic silica (diatoms, sponge spicules), total amorphous silica, and stable carbon and nitrogen isotope ratios of bulk OM. Principal component analysis showed that diatom biogenic silica, TC:TN, Poly-P and TP displayed discernible stratigraphic changes associated with the shift in the primary producer community. We applied k-means cluster analysis to these variables to identify macrophyte-derived, transitional, and phytoplankton-derived sediments. Our approach provides an objective method for identifying sediment sources that may be applied to shallow lakes in other regions. The four study lakes shifted from a macrophyte-dominated state to a transitional state before major anthropogenic disturbances, and became phytoplankton-dominated after ~1950.

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Acknowledgments

We thank the late Martha Love and Brandy DeArmond for administrative and technical assistance. Financial support was provided in part by the St. Johns River Water Management District, the University of Florida Foundation, Carl S. Swisher Endowment, and the University of Florida Land Use and Environmental Change Institute (LUECI).

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Correspondence to William F. Kenney.

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Kenney, W.F., Brenner, M., Curtis, J.H. et al. Identifying sources of organic matter in sediments of shallow lakes using multiple geochemical variables. J Paleolimnol 44, 1039–1052 (2010). https://doi.org/10.1007/s10933-010-9472-y

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  • DOI: https://doi.org/10.1007/s10933-010-9472-y

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