ABSTRACT
Few studies have examined long-term ecological effects of sustained low-level nutrient enhancement on wetland biota. To determine sustained effects of phosphorus (P) addition on Everglades marshes we added P at low levels (5, 15, and 30 microg L(-1) above ambient) for 5 yr to triplicate 100-m flow-through channels in pristine marsh. A cascade of ecological responses occurred in similar sequence among treatments. Although the rate of change increased with dosing level, treatments converged to similar enriched endpoints, characterized most notably by a doubling of plant biomass and elimination of native, calcareous periphyton mats. The full sequence of biological changes occurred without an increase in water total P concentration, which remained near ambient levels until Year 5. This study indicates that Everglades marshes have a near-zero assimilative capacity for P without a state change, that ecosystem responses to enrichment accumulate over time, and that downstream P transport mainly occurs through biota rather than the water column.
Subject(s)
Ecosystem , Food Chain , Phosphorus/analysis , Phosphorus/metabolism , Water Pollutants/analysis , Water Pollutants/metabolism , Animals , Florida , Water/chemistry , Water SupplyABSTRACT
Direct evidence for autotrophic ammonia oxidation is documented for the first time in a deep-sea hydrothermal plume. Elevated NH(4) (+) concentrations of up to 341+/-136 nM were recorded in the plume core at Main Endeavour Field, Juan de Fuca Ridge. This fueled autotrophic ammonia oxidation rates as high as 91 nM day(-1), or 92% of the total net NH(4) (+) removal. High abundance of ammonia-oxidizing bacteria was detected using fluorescence in situ hybridization. Ammonia-oxidizing bacteria within the plume core (1.0-1.4x10(4) cells ml(-1)) accounted for 7.0-7.5% of the total microbial community, and were at least as abundant as methanotrophs. Ammonia-oxidizing bacteria were a substantial component of the particle-associated communities (up to 51%), with a predominance of the r-strategist Nitrosomonas-like cells. In situ chemolithoautotrophic organic carbon production via ammonia oxidation may yield 3.9-18 mg C m(-2) day(-1) within the plume directly over Main Endeavour Field. This rate was comparable to that determined for methane oxidation in a previous study, or at least four-fold greater than the flux of photosynthetic carbon reaching plume depths measured in another study. Hence, autotrophic ammonia oxidation in the neutrally buoyant hydrothermal plume is significant to both carbon and nitrogen cycling in the deep-sea water column at Endeavour, and represents another important link between seafloor hydrothermal systems and deep-sea biogeochemistry.
Subject(s)
Ammonia/metabolism , Betaproteobacteria/isolation & purification , Chemoautotrophic Growth , Nitrosomonas/isolation & purification , Seawater/microbiology , Betaproteobacteria/classification , Betaproteobacteria/genetics , Hot Temperature , In Situ Hybridization, Fluorescence , Nitrosomonas/classification , Nitrosomonas/genetics , Oxidation-ReductionABSTRACT
Three in situ methods of visualizing the cbbL gene in intact cells of nitrifying bacteria at different physiological states (dormant and metabolically active) were compared after epifluorescence microscopy and image analysis. FISH alone showed the weakest signal intensity. Direct in situ PCR, incorporating labeled nucleotides, showed the greatest sensitivity but also the greatest background. The combination of unlabeled in situ PCR followed by FISH showed relatively high sensitivity, along with the lowest background and highest specificity. Although functional gene expression was not examined in this study, visualization of the potential for carbon fixation in heterogeneous cultures of nitrifying bacteria was demonstrated.
