文摘
Elevated mercury concentrations have been reportedin fish and wildlife from the Everglades in recentyears. The hypothesis that eutrophication caused bythe impact of phosphorous- (P) rich agriculturalrunoff stimulated methylmercury accumulation wasput forward because eutrophication had beenshown to be a cause for methylmercury accumulationin other ecosystems. We tested this hypothesis byobtaining total mercury (HgT) concentrationsandaccumulation rates and estimating the potential formicrobial methylation and methylmercury degradation in peat soils collected along a P gradient in waterconservation area 2A (WCA-2A). A negative correlation observed between HgT and Pconcentrationsin soils (r2 = 0.64) was explained byincreased peataccretion rates in a nutrient-enriched area (7.1-7.5 mmyr-1) as compared to an unenriched area(1.92-2.50 mm yr-1), estimated using lead-210 andcesium-137 dating. Total Hg accumulation rates (post-1964)were comparable for the enriched and unenriched sites(29-30 and 29-37 µg m-2yr-1, respectively). Thus,calculations of HgT accumulation rates areconfounded by differences in peat accretion rates inthe Everglades. Potential rates for both methylation(2.3-48.6 ng g-1day-1) and demethylation(6.5-113.2ng g-1 day-1) werehigher in samples from WCA-2A than in samples collected in an area of the Evergladesthat had never been exposed to nutrients. However,trends suggesting the relationships of theseactivities to the P gradient in WCA-2A were notdetected, and methylation to demethylation ratios didnot correlate with soil P concentrations. The resultssuggest that (i) nutrient-enriched agricultural runofforiginating upstream of WCA-2A did not contributesignificantly to HgT built up in the northernEvergladesand (ii) eutrophication did not affect the potentialfor net methylmercury formation in peatsoils.