Stable isotope (delta C-13 and delta N-15) signatures of sedimented organic matter as indicators of historic lake trophic state

We explored the use of carbon and nitrogen isotopes (delta(13)C and delta(1 5)N) in sedimented organic matter (OM) as proxy indicators of trophic state change in Florida lakes. Stable isotope data from four Pb-210-dated sedime nt cores were compared stratigraphically with established proxies for histo rical trophic state (diatom-inferred limnetic total phosphorus, sediment C/ N ratio) and indicators of cultural disturbance (sediment total P and Ra-22 6 activity). Diatom-based limnetic total P inferences indicate a transition from oligo-mesotrophy to meso-eutrophy in Clear Lake, and from eutrophy to hypereutrophy in Lakes Parker, Hollingsworth and Griffin. In cores from al l four lakes, the carbon isotopic signature of accumulated OM generally tra cks trophic state inferences and cultural impact assessments based on other variables. Oldest sediments in the records yield lower diatom-inferred tot al limnetic P concentrations and display relatively low delta(13)C values. In the Clear, Hollingsworth and Parker records, diatom-inferred nutrient co ncentrations increase after ca. AD similar to 1900, and are associated stra tigraphically with higher delta(13)C values in sediment OM. In the Lake Gri ffin core, both proxies display slight increases before 1900, but highest v alues occur over the last similar to 100 years. As Lakes Clear, Hollingswor th and Parker became increasingly nutrient-enriched over the past century, the delta(15)N of sedimented organic matter decreased. This reflects, in pa rt, the increasing relative contribution of nitrogen-fixing cyanobacteria t o sedimented organic matter as primary productivity increased in these wate rbodies. The Lake Griffin core displays a narrow range of both delta(13)C a nd delta(15)N values. Despite the complexity of carbon and nitrogen cycles in lakes, stratigraphic agreement between diatom-inferred changes in limnet ic total P and the stable isotope signatures of sedimented OM suggests that delta(13)C and delta(15)N reflect shifts in historic lake trophic state.