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Fire Effects on Nitrogen Cycling in Native and Restored Calcareous Wetlands


Fire is an important natural process and management tool in the Florida Everglades, but few studies have examined its effects on nutrients; nitrogen (N) in particular has received little attention across the whole Everglades system. In this study, we investigated fire effects on the N cycle in both a high-phosphorus (P) restored wetland and a low-P reference calcareous wetland (marl prairie) in the Hole-in-the-Donut region of the southern Everglades. Potential N mineralization, denitrification, extracellular enzyme activities, and periphyton N2 fixation rates were measured immediately (two days), one month, and one year after a prescribed burn. Results showed differing responses of N cycle processes between the two sites: N availability increased immediately after the fire at the low-P reference site, but did not increase immediately at the high-P restored site. We also saw a greater increase in denitrification immediately after the fire in the reference site (118% increase) compared to only 20% increase in the restored site. Periphyton N2 fixation in the restored site tended to be stimulated, but was inhibited in the reference site after the fire. The underlying mechanisms for these changes are not clear, but fire residues (ash and char) may directly and indirectly affect the N cycle. These findings have implications for management of fire intensity in natural and P-impacted sites.


Fire has great influences on nutrient cycles in ecosystems by changing the form, distribution, and amount of nutrient, as well as by changing plant species composition (Raison 1979, Bissett and Parkinson 1980, Dumontet et al. 1996, Grogan et al. 2000, Brown et al. 2004, Certini 2005). The effect of fire on the nitrogen (N) cycle is highly important because N, like phosphorus (P), is often a limiting nutrient for primary productivity. Compared to P, the N cycle is more complex and involves various processes. For example, N can be easily lost through denitrification, ammonification, and volatilization. Since N is important for plants, many studies have focused on the available N status before and after fire, trying to understand the effects of the fire on subsequent primary production.

Fire can affect nutrient cycles within a system in various ways. Combustion differentially affects elemental composition of fuel through volatilization of carbon compounds and N as ammonia (NH3) and nitrogen oxides (NOx), while P compounds largely remain in the ash and char residues (Hogue and Inglett 2012). The transfer of heat to the soil increases soil temperature and affects the physical, chemical, and biological soil properties (Neary et al. 1999). For example, elevated temperatures can kill soil microbes, decompose organic matter, and change N forms (Raison 1979).

The particulate residues left by fire are also an important pathway for nutrients to return back to or redistribute in the ecosystem after the fire (Zackrisson et al. 1996, Qian et al. 2009). Fire residues contain small amounts of inorganic and organic N that directly serve as a N source (Qian et al. 2009, Hogue and Inglett 2012). Both ash and charcoal can also exert an indirect influence on N availability through modification of the pH and the cation exchange capacity (Raison 1979, Glaser et al. 2002). Indirectly, P in fire residues can also stimulate N processes, such as N2 fixation and nitrification, and N mineralization, especially in P-limited ecosystems (Eisele et al. 1990; White and Reddy 1999, 2000). Charcoal with its great adsorptive surface can also enhance nitrification, leading to elevated nitrate levels (Zackrisson et al. 1996; Wardle et al. 1998; DeLuca et al. 2002, 2006).

Studies on prescribed fire have mostly focused on forests, grasslands, and prairies (Ojima et al. 1994, Blair 1997, Grogan et al. 2000, Castaldi and Aragosa 2002, Zackrisson et al. 2004), while comparatively few have focused on wetlands (Battle and Golladay 2003). However, fire and hydrology together are important elements in wetland management (Lockwood et al. 2003) where fire is used to control the spread of invasive species in both coastal and inland wetlands (Kirby et al. 1988). For example, the Florida Everglades is regarded as a fire-dependent landscape (Beckage et al. 2005), and reestablishing a more natural hydrology and fire regime is a key component of successful restoration (Lockwood et al. 2003).

Numerous fire projects have been conducted in a diversity of landscapes across the Everglades, such as the River of Grass prescribed fire plan for the wet prairie and sawgrass marsh ecosystems, the Pinelands burn plan, the mangrove-marsh ecotone fire project, and the fire project in Water Conservation Area 2A (WCA 2A) of the northern Everglades (Spier and Snyder 1998, Beckage et al. 2005, Qian et al. 2009). However, while most of these projects have focused on restoring native plant species, little is known about the fire effects on nutrient biogeochemistry, let alone on the N cycle that has been ignored across the whole Everglades ecosystem (Miao and Sklar 1998, Miao and Carstenn 2006, Qian et al. 2009, Inglett et al. 2011).

To bridge the gap between our knowledge of fire, the N cycle, and wetland restoration, a case study on the N responses to fire at restored and reference wetlands was conducted in the Everglades National Park. Based on the literature, we proposed the following hypotheses: 1) fire would increase N availability, in particular that of nitrate; 2) higher nitrate levels would lead to increased denitrification rates; and 3) fire would increase N2 fixation because of the possible elevation of available P after fire.


Study Site and Sampling Methods

The study site was located in the Hole-in-the-Donut (HID) of Everglades National Park, Florida, USA (Figure 1). Two sampling sites were selected in this study. One site was used extensively for agriculture with subsequent nutrient enrichment and was restored by topsoil removal (Res2000; Inglett and Inglett 2013), while the other was a native marl prairies ecosystem that had not been disturbed by humans (Reference; Figure 1). Plant species at Res2000 were dominated by Andropogon spp., Muhlenbergia spp., and Baccharis halimfolia L.; while the dominant species at the reference site included Muhlenbergia spp. and Cladium jamaicense (Crantz). The removal of soil in the restored sites resulted in comparatively shallower soil depth (average 2.3 cm) in these areas relative to that of the reference site (average 10.3 cm).

Figure 1

Location of the study site within the Everglades National Park in South Florida, USA.

At each of the Res2000 and Reference sites, two locations corresponding to high and low elevation areas were selected. At each of these four locations, three treatment (burned) and three control (unburned) 10 m × 30 m plots were identified. Fire encroachment into the control areas was prevented by removing the vegetation within a 2-meter buffer zone surrounding each of the plots. Within each sampling plot, a 2 m × 2 m grid system was devised (75 grid cells) and used to randomly sample each of the plots before and after the fire.

The prescribed fire occurred on 4 May 2010. Based on prescription parameters, all fire weather observations taken during the firing period were either in preferred or acceptable ranges except for shaded fine dead fuel moistures. Recorded relative humidity was lowest in the morning with a value of 55%, which was within the preferred range of 45% to 75%. In the afternoon, at the hottest hour of the day, the heat index value was 36 °C. Wind direction was predominantly from the south or south southeast, but occasionally switched to all directions except north. Exposed fine dead fuel moistures were lowest at noon with values of 8%, which was within the acceptable range of 5% to 10%. The prescribed fire was completed through a combination of burning out from control lines, burning around research plots, and aerial ignition. Observed head fire rates of spread near the research plots ranged from 5 m min−1 to 10 m min−1, depending on the density and continuity of grassy fuels. Flame lengths from grassy fuels were usually 2.5 m to 3.6 m.

We collected samples one month before the fire (8 to 10 April 2010), and two days (6 and 7 May 2010), one month (10 and 11 June 2010), and one year (25 and 26 May 2011) after the fire. Samples of surface soil (0 cm to 5 cm or to the bedrock) were taken using a sharpened steel tube, and periphyton biomass samples were taken by hand. All samples were sealed in plastic bags and kept on ice until their return to the laboratory, where the samples were refrigerated at 4 °C until subsequent analysis.

Periphyton samples were kept intact (periphyton mat) and inspected to remove large organic debris (plant litter) and soil. Soil samples were sieved to remove roots and rock fragments greater than 2 mm diameter. Fresh periphyton was used to determine nitrogenase activity, while sieved soil samples were used in the determination of all soil microbial and enzyme related parameters. A subsample of sieved soil was oven dried at 105 °C for three days and ground using a mortar and pestle for moisture content and total nutrient determinations. Periphyton moisture content and nutrients were determined using the sample used for nitrogenase activity, which was oven dried at 65 °C for three days and ball milled.

Biogeochemical Analysis

Extractable inorganic nitrogen. Extractable and exchangeable NH4+ and NO3 was determined by extracting soil samples (1 g dry weight equivalent) with 25 ml of 2.0 M KCl for 1 h (Mulvaney 1996). The samples were then centrifuged and the supernatant filtered through Whatman 41 and analyzed for NH4-N (EPA method 350.1 [USEPA 2012]) and NO3-N (EPA method 353.2 [USEPA 2012]). Microbial biomass C and N (MBC and MBN, respectively) were determined using the chloroform fumigation-extraction technique (Brookes et al. 1985). The extraction efficiency factors for MBC and MBN in the study were 0.37 and 0.42, respectively.

Denitrification enzyme assay (DEA). This method was modified from Smith and Tiedje (1979), using the acetylene block technique (yielding N2O production) and adding sufficient NO3 and carbon source. Triplicate, 5 g wet soil samples were sealed with rubber septa stoppers in 30 ml tubes; 3 ml distilled deionized (DDI) water were added to the tube and purged with N2 to maintain anaerobic conditions. Two milliliters of acetylene gas (C2H2; approximately 10% headspace) was injected into the tubes to block the conversion from N2O to N2, and the tubes were then shaken for 1 h to disperse the gas. After shaking, a DEA solution (0.202 g KNO3 L−1, 0.25 g chloramphenicol L−1, and 0.360 g C6H12O6 L−1) purged with oxygen-free N2 gas was added to the tubes. Samples were shaken and incubated at room temperature. Headspace gas was collected at 1 h intervals for about 5 h. The potential denitrification rate was calculated from the steepest portion of curve produced when cumulative N2O evolution was plotted against time. The sampled gas was injected in a Shimadzu GC-14-A ECD gas chromatograph (Shimadzu Corporation, Kyoto, Japan) equipped with an electron capture detector (ECD) and Porapak Q column (Waters Associates, Inc., Milton, Massachusetts, USA). The operation temperatures for the column, injection port, and detector were set at 70 °C, 120 °C, and 230 °C, respectively. A 10 ppm standard concentration gas (Scott Specialty Gases, Inc., Plumsteadville, Pennsylvania, USA) was used to calibrate the measurement, and results were reported as N2O-N produced per gram of dry weight soil, per hour.

Extracellular enzyme activities. Two N-related enzymes, (i.e., N-acetyl-β-D-glucosaminidase [NAG, EC] and Leucine aminopeptidase [LAP, EC]), were measured using fluorogenic enzyme substrate (Hoppe 1983). Methods were modified from Sinsabaugh et al. (1997) to optimize the substrate concentrations in soil samples with fluorogenic substrates 4-Methylumbelliferyl N-acetyl-β-D-glucosaminide (MUF-N) for NAG, and L-leucine 7-amido-4-methyl coumarin (AMC) for LAP. Enzyme substrates MUB-N and AMC produce fluorochrome methylumbelliferone (MUF) and aminomethylcoumarin (AMC) once they are hydrolyzed by the enzyme NAGase and LAPase, respectively. The fluorescence of samples and standards was measured at an excitation of 350 nm and an emission of 450 nm using a Bio-Tek Model FL600 fluorometric plate reader (Bio-Tek Instruments, Inc., Winooski, Vermont, USA). The potential enzyme activity was expressed in µmol MUF g−1 dw h−1 released or µmol AMC g−1 dw h−1 released.

Nitrogenase activity (N 2 fixation). We used the acetylene reduction (AR) assay described by Liao and Inglett (2012). Wet periphyton (5 g) was placed into 42 ml, screw-capped culture tubes (KimaxTM, Kimble Chase Life Sciences and Research Products LLC, Vineland, New Jersey, USA) with an open-top cap containing a teflon-lined, silicone septa (0.125 cm thick). Acetylene gas (generated by adding water to CaC2 in an evacuated serum bottle) was added to each tube (4 ml; 10% headspace) and the tubes were gently shaken to evenly distribute the gas in the sample. Tubes containing samples and blanks containing only injected C2H2 were incubated at a constant temperature (27 °C) for up to three hours under either light (900 µmol m−2 s−1 photosynthetically active radiation [PAR]) or dark conditions. After incubation, tubes were vigorously shaken to equilibrate gas phases, and gas samples (4 ml) were taken from each tube and stored in evacuated 3.5 ml Exetainers™ (Labco International, Houston, Texas, USA.) Gas samples were analyzed for ethylene using a GC-8A (Shimadzu Corp., Kyoto, Japan) gas chromatograph equipped with a flame ionization detector (110 °C) and a Porapak N column (80 °C). Two standard gases (1 ppm and 10 ppm) were used to calibrate the measurement. Nitrogenase was then expressed as nmol C2H4 g−1 dw h−1.

Statistical Analysis

Data were analyzed with JMP v.8© statistical software (SAS Institute, Inc., Cary, North Carolina, USA). For pre-fire data, one-way analysis of variance (ANOVA) was used to compare the difference in measured parameters between the restored and reference sites. For post fire data, the factors of site and sampling time were fixed and separate one-way analyses for the different sites and dates were performed. Regressions between different parameters were performed using the linear least-squares method. All results were reported as significant when P < 0.05. Data were log transformed when necessary to improve normality.


Fire effects on extractable inorganic nitrogen. Both restored and reference sites showed an increase in extractable NOx-N and NH4-N two days after the fire (Figure 2). The increase of extractable inorganic N was greater at the reference site (i.e., approximately twice that of the control plots) compared to the restored site (i.e., only 20% to 40% higher than the control plots); and only at the reference site was the difference statistically significant (P < 0.05). At longer time scales (one month to one year after the fire), the extractable NOx-N remained higher in the burn plots than in the control plots for the reference site (Figure 2), but the extractable NH4-N at both restored and reference sites dropped to levels below that of the control plot one month after the fire (Figure 2).

Figure 2

Changes of the extractable NOX-N and NH4-N of the soil in the burn plots and control plots in the restored wetlands (Res2000) and reference wetlands two days, one month, and one year after the fire. The black bar represents the value before fire. The star (*) denotes significant difference between the burn plots and control plots (P < 0.05).

Fire effects on extracellular enzyme activities. The two N-related enzymes (i.e., LAP and NAG) responded to the fire similarly at each specific site, but responded differently between sites (Figure 3). In the restored site, the LAP and NAG did not change appreciably up to one month after the fire, but after one year, they increased by 20% and 40%, respectively, relative to the control plots. In contrast with the restored site, the enzyme activities in the burn plots at the reference site were significantly greater than those in the control plots immediately (two days) after the fire, but after one month, the enzyme activities returned to or even fell below the control levels.

Figure 3

Changes of LAP and NAG in the burn plots and control plots in the restored wetlands (Res2000) and reference wetlands two days, one month, and one year after the fire. The black bar represents the value before fire.

Fire effects on denitrification. Both the restored and reference sites showed similar responses of denitrification (measured as DEA) to the fire (Figure 4). Immediately after the fire, approximately 20% higher DEA rates were observed in the burn plots compared to the control plots at the restored site. For the reference site, the DEA rates at the burn plots were up to twice the values in the control plots. After one year, DEA rates in the burn plots had returned to the levels in control plots.

Figure 4

Changes of denitrification enzyme activities (DEA) in the burn plots and control plots in the restored wetlands (Res2000) and reference wetlands two days, one month, and one year after the fire. The black bar represents the value before fire.

Fire effects on periphyton N 2 fixation. The responses of periphyton N2 fixation to the fire differed between the restored and reference sites. At the restored site, N2 fixation rates slightly decreased immediately after the fire, but then increased to as high as twice those in the control plots one year after the fire. In contrast, at the reference site, the rates fell below the control levels after one year (Figure 5).

Figure 5

Changes of N2 fixation rates in the burn plots and control plots in the restored wetlands (Res2000) and reference wetlands two days, one month, and one year after the fire. The black bar represents the value before fire.


Responses of Nitrogen Availability to the Fire

Most studies consistently suggest that fire can increase the availability of soil NH4 + and NO3 (Wan and Lao 2001). NH4 + is a direct product of the combustion, which is adsorbed by the soil, thus increasing the concentration of NH4 +. In this project, higher extractable NH4-N was observed two days after the fire in the burn plots at both restored and reference sites. The release of NH4 + from organic matter could also be further oxidized to NO2 and then NO3 (Hobbs and Schimel 1984, Blank and Zamudio 1998). Covington et al. (1991) found that NO3 was not immediately affected, but one year after burning, concentrations had become dramatically higher than the pre-fire level. In this study, however, both the restored and reference sites saw an immediate increase in NOx-N two days after the fire, and in the reference site, the increased NOx-N lasted for one year.

The elevation of N availability may be the result of deposition of ash with high concentrations of nutrients. Grogan et al. (2000) investigated the effect of natural ash deposition on post-fire ecosystem N cycling by removing the surface ash layer from field plots within one week of a wildfire in a Californian Bishop pine (Pinus muricata D. Don) forest. They characterized the influence of ash on plant, soil, and microbial N pools during the first growing season after fire and found that ash deposition during wildfires can enhance soil N availability to plants and facilitate ecosystem N retention. A recent explanation for the increase of the available N in forest ecosystems was the influence of charcoal on soil N dynamics and, in particular, nitrification (DeLuca et al. 2006). In their study, DeLuca and Sala (2006) found that charcoal significantly increased nitrification and the NO3 concentration in the soils. Despite these studies, there are few reports on wetland ecosystems. Qian et al. (2009) simulated fire in the Water Conservation Area (WCA)-2A in the Everglades through muffle furnace combustion but focused only on the effects of ash on phosphorus. Hogue and Inglett (2012) characterized fire residues (ashes) created by both muffle furnace and flame combustion, observing an increase of available N in char residues after the simulated fire.

In addition, burning can increase extractable P through combustion and heating of organic matter, and pH increases caused by ash also can cause the release of ortho-P bound by iron and aluminum (DeBano and Klopatek 1988). Hogue and Inglett (2012) showed that charcoal formed after burning at low temperature in the HID marl prairie ecosystem contained more bicarbonate extractable P. For the low-P reference site, the addition of P through ash or charcoal could stimulate N mineralization and further increase N availability, similar to the results of White and Reddy (1999, 2000) and Inglett et al. (2007) in which P loading led to increased N mineralization in Everglades wetland soil.

Previous studies of the effects of fire on N mineralization in prairie and grasslands have resulted in conflicting results, with fire either causing a decrease (Ojima et al. 1994; Blair 1997; Turner et al. 1997, 2007), an increase (Aranibar et al. 2003, Boerner and Brinkman 2003), or having no effect on N mineralization (Raison 1979). The results depend on different ecosystems and fire behavior; accordingly, various mechanisms were proposed to explain the observations. For example, Bell and Binkley (1989) pointed out that N mineralization from soil organic matter is enhanced after fire due to elevated soil temperature, while Vance and Henderson (1984) concluded that N mineralization decreased after a burn because of the poor substrate quality. Stock and Lewis (1986) also considered that these conflicting results may be attributed to the use of different methods to determine N mineralization. In this study, we measured potential soil N mineralization (PMN) using a 10-day anaerobic incubation method. We saw slightly increased PMN after the fire at the low-P reference site compared to the high-P restored site, although the responses were not significant (data not shown).

Effects of Fire on Extracellular Enzyme Activities

It is important to study the effects of fire on the activity of soil microorganisms and enzyme systems because these are responsible for mineralization processes and nutrient availability (Saa et al. 1993). Moreover, microbial biomass and enzyme activities are affected by management practices and can be used as sensitive indicators of ecological stability (Ajwa et al. 1999, Vazquez et al. 2003). The two N-related enzymes measured in this study, LAP and NAG, are inducible enzymes that are synthesized or activated when needed. LAP activities were significantly positively related with PMN (Figure 6), indicating that LAP activity can be used as a reliable index of N mineralization in soils. NAG activity, in this study, decreased one month after the fire in the restored and reference sites.

Figure 6

(A) Correlation between nitrogen mineralization (measured as potentially mineralizable nitrogen, PMN) and Leucine aminopeptidase (LAP), and (B) correlation between extractable nitrite/nitrate (Ext. NOX-N) and denitrification (measured as potentially denitrification rates DEA) two days, one month, and one year after the fire in the restored (Res2000) and reference wetlands.

These results agreed with Boerner et al. (2008) who observed reductions in chitinase activity after fire in North American forest ecosystems. They considered these reductions to be the result of the deposition of more labile organic matter following fire. Other than nutrients, the response of N acquisition enzymes could depend on fire intensity or severity (Boerner et al. 2000). For example, during low-severity fires (as in grassland type systems like the HID), little heat is transferred downward, minimizing the direct effect of heat on microbial death and, thus, resulting in no significant short-term change in the enzyme activities.

Fire Effects on Denitrification

Few studies have focused on the influence of fire on denitrification. Our results showed that there was no significant difference in potential DEA rates between the burned and control plots, which was similar to the results of Castaldi and Aragosa (2002) in that DEA did not change significantly immediately after fire (i.e., seven days after the fire) in a Mediterranean shrubland. They considered that other factors, such as water content, would affect denitrification more than the fire. In this study, the slight increase of DEA two days after the fire could be caused by the increase of NO3 content, especially for the reference site in which a significantly positive correlation between NOX-N and DEA was observed (Figure 6). No significant correlation existed between the NOX and DEA in the restored sites (Figure 6), which may have been reflective of the higher N demand in the soils of these areas.

Fire Effects on Periphyton N2 Fixation

It is anticipated that P inputs will have a stimulatory effect on N2 fixation by periphyton (Inglett et al. 2004, Liao and Inglett 2012); however, we were only able to observe increased fixation rates in the restored site after one year (Figure 5). This result was similar to that of Zackrisson et al. (2004) that showed, in northern boreal forests in Sweden, the N2 fixation rates increased linearly with time since fire. They attributed the increase to the degree of colonization by cyanobacteria and site factors such as presence of available N. In this study, it is likely that ash deposition from the fire elevated P levels in the restored site (Hogue and Inglett 2012). This pulse of new P may have enhanced the N limitation already present in these sites, thus resulting in stimulated periphyton N2 fixation.

In contrast, at the reference site, the nitrogenase activities only slightly increase one month after the fire and reduced below their control levels one year after the fire. DeLuca et al. (2002) pointed out that since fire increased the availability of N and reduces the presence of P leurozium schreberi and associated N-fixing symbionts, it is likely that the N2 fixation rates by P. schreberi would decrease following the fire. Another study related to nitrogenase response to the fire was done in mountain shrub and grassland communities during two years following fire (Hobbs and Schimel 1984). They found that nitrogenase activity was depressed by fire one year after the burn in the mountain shrub community, and they considered that the elevation of the soil inorganic N levels in burn plots may contribute to the depression in nitrogenase activity. This explanation is plausible in the reference site in which we did see increases of extractable NOX one year after the fire.

Implications for Restoration Management

In this study, we found that fire exerted different influences on the N cycle in sites of different P status. In P-limited ecosystems like the reference site in this study, a small amount of P addition through ash can stimulate N mineralization and nitrification, while for the restored site with high P, the P deposition from ash does not greatly affect the N cycle. Another fire residue, charcoal, has also been reported to elevate the nitrification and N availability (DeLuca et al. 2002, 2006). Since fire intensity decides the proportion of charcoal and ash (Qian et al. 2009, Hogue and Inglett 2012), it would be helpful for land managers to know which form contributes more to the increase of N availability when deciding on a high- or low-intensity fire plan.

Fire volatilizes N but can simultaneously increase the short-term availability of residual soil N (Vitousek and Howarth 1991). The increase of inorganic N is likely a significant influence on the regrowth of native plant species, the invasion of exotic plant species, and ultimately, the site recovery potential (Dalrymple et al. 2003, Rau et al. 2007). For the HID restoration, the young restored sites are more N-limited, while the native reference site is limited more by P. The long-term goal for the restoration is to shift from N limitation in the recently restored sites to a more P-limited condition similar to the reference site (Inglett and Inglett 2013). Frequent fire causes addition of P and losses of N in excess of replacement by N2 fixation, and is probably a significant cause of N limitation in terrestrial ecosystems (Vitousek 1982). Therefore, it is important to decide whether a high- or low-frequency burning cycle should be applied in the restored site to speed up the restoration process.

Overall, this type of research is important to help identify the impacts of fire on the N cycle as it relates to the availability of P. Future research should focus on the relationships between fire intensity and severity, abundance and form of fire residues, as well as the long-term effect of particular fire regimes (low or high frequency). This information is crucial to better understand the function of fire in the natural ecosystem and the balance between N and P leading to the reestablishment of native wetlands with low nutrients, such as the Everglades.

Literature Cited

  1. Ajwa, H., C.J. Dell, and C.W. Rice. 1999. Changes in enzyme activities and microbial biomass of tallgrass prairie soil as related to burning and nitrogen fertilization. Soil Biology and Biochemistry 31: 769–777. doi: 10.1016/S0038-0717(98)00177-1

    Article  CAS  Google Scholar 

  2. Aranibar, J.N., I.C. Anderson, S. Ringrose, and S.A. Macko. 2003. Importance of nitrogen fixation in soil crusts of southern African arid ecosystems: acetylene reduction and stable isotope studies. Journal of Arid Environments 54: 345–358. doi: 10.1006/jare.2002.1094

    Article  Google Scholar 

  3. Battle, J., and S.W. Golladay. 2003. Prescribed fire’s impact on water quality of depressional wetlands in southwestern Georgia. American Midland Naturalist 150: 15–25. doi: 10.1674/0003-0031(2003)150[0015:PFIOWQ]2.0.CO;2

    Article  Google Scholar 

  4. Beckage, B., W.J. Platt, and B. Panko. 2005. A climate-based approach to the restoration of fire-dependent ecosystems. Restoration Ecology 13: 429–431. doi: 10.1111/j.1526-100X.2005.00070.x

    Article  Google Scholar 

  5. Bell, R.L., and D. Binkley. 1989. Soil nitrogen mineralization and immobilization in response to periodic prescribed fire in loblolly pine plantation. Canadian Journal of Forest Research 19: 816–820. doi: 10.1139/x89-125

    Article  Google Scholar 

  6. Bissett, J., and D. Parkinson. 1980. Long-term effects of fire on the composition and activity of the soil microflora of a subalpine, coniferous forest. Canadian Journal of Botany 58: 1704–1721. doi: 10.1139/b80-199

    Article  Google Scholar 

  7. Blair, J.M. 1997. Fire, N availability, and plant response in grasslands: a test of the transient maxima hypothesis. Ecology 78: 2359–2368. doi: 10.1890/0012-9658(1997)078[2359:FNAAPR]2.0.CO;2

    Article  Google Scholar 

  8. Blank, R.R., and D.C. Zamudio. 1998. The influence of wildfire on aqueous-extractable soil solutes in forested and wet meadow ecosystems along the eastern Sierra-Nevada range, California. International Journal of Wildland Fire 8: 79–85. doi: 10.1071/WF9980079

    Article  Google Scholar 

  9. Boerner, R.E.J., and J.A. Brinkman. 2003. Fire frequency and soil enzyme activity in southern Ohio oak-hickory forests. Applied Soil Ecology 23: 137–146. doi: 10.1016/S0929-1393(03)00022-2

    Article  Google Scholar 

  10. Boerner, R.E.J., C. Giai, J.J. Huang, and J.R. Miesel. 2008. Initial effects of fire and mechanical thinning on soil enzyme activity and nitrogen transformations in eight North American forest ecosystems. Soil Biology and Biochemistry 40: 3076–3085. doi: 10.1016/j.soilbio.2008.09.008

    Article  CAS  Google Scholar 

  11. Boerner, R.E.J., S.J. Morris, E.K. Sutherland, and T.F. Hutchinson. 2000. Spatial variability in soil nitrogen dynamics after prescribed burning in Ohio mixed-oak forests. Landscape Ecology 15: 425–439. doi: 10.1023/A:1008179702536

    Article  Google Scholar 

  12. Brookes, P.C., A. Landman, G. Pruden, and D.S. Jenkinson. 1985. Chloroform fumigation and the release of soil nitrogen: a rapid direct extraction method to measure microbial biomass nitrogen in soils. Soil Biology and Biochemistry 17: 83–84. doi: 10.1016/0038-0717(85)90144-0

    Google Scholar 

  13. Brown, R.T., J.K. Agee, and J.F. Franklin. 2004. Forest restoration and fire: principles in the context of place. Conservation Biology 18: 903–912. doi: 10.1111/j.1523-1739.2004.521_1.x

    Article  Google Scholar 

  14. Castaldi, S., and D. Aragosa. 2002. Factors influencing nitrification and denitrification variability in a natural and fire-disturbed Mediterranean shrubland. Biology and Fertility of Soils 36: 418–425. doi: 10.1007/s00374-002-0549-2

    Article  CAS  Google Scholar 

  15. Certini, G. 2005. Effects of fire on properties of forest soils: a review. Oecologia 143: 1–10. doi: 10.1007/s00442-004-1788-8

    Article  Google Scholar 

  16. Covington, W.W., L.F. DeBano, and T.G. Huntsberger. 1991. Soil nitrogen changes associated with slash pile burning in pinyon-juniper woodlands. Forest Science 37: 347–355.

    Google Scholar 

  17. Dalrymple, G.H., R.F. Doren, N.K. O’Hare, M.R. Norland, and T.V. Armentano. 2003. Plant colonization after complete and partial removal of disturbed soils for wetland restoration of former agricultural fields in Everglades National Park. Wetlands 23: 1015–1029. doi: 10.1672/0277-5212(2003)023[1015:PCACAP]2.0.CO;2

    Article  Google Scholar 

  18. DeBano, L.F., and J.M. Klopatek. 1988. Phosphorus dynamics of pinyon-juniper soils following simulated burning. Soil Science Society of America Journal 52: 271–277. doi: 10.2136/sssaj1988.03615995005200010048x

    Article  CAS  Google Scholar 

  19. DeLuca, T.H., M.C. Nilsson, and O. Zackrisson. 2002. Nitrogen mineralization and phenol accumulation along a fire chronosequence in northern Sweden. Oecologia 133: 206–214. doi: 10.1007/s00442-002-1025-2

    Article  CAS  Google Scholar 

  20. DeLuca, T.H., D.M. MacKenzie, M.J. Gundale, and W.E. Holben. 2006. Wildfire produced charcoal directly influences nitrogen cycling in forest ecosystems. Soil Science Society of American Journal 70: 448–453. doi: 10.2136/sssaj2005.0096

    Article  CAS  Google Scholar 

  21. DeLuca, T.H., and A. Sala. 2006. Frequent fire alters nitrogen transformations in ponderosa pine stands of the inland northwest. Ecology 87: 2511–2522. doi:[2511:FFANTI]2.0.CO;2

    Article  Google Scholar 

  22. Dumontet, S., H. Dinel, A. Scopa, A. Mazzatura, and A. Saracino. 1996. Post-fire soil microbial biomass and nutrient content of a pine forest soil from a dunal Mediterraneal environment. Soil Biology and Biochemistry 28: 1467–1475. doi: 10.1016/S0038-0717(96)00160-5

    Article  CAS  Google Scholar 

  23. Eisele, K.A., D.S. Schimel, L.A. Kapustka, and W.J. Parton. 1990. Effects of available P and N: P ratios on non-symbiotic dinitrogen fixation in tall grass prairie soils. Oecologia 79: 471–474. doi: 10.1007/BF00378663

    Article  Google Scholar 

  24. Glaser, B., J. Lehmann, and W. Zech. 2002. Ameliorating physical and chemical properties of highly weathered soils in the tropics with charcoal—a review. Biology and Fertility of Soils 35: 219–230. doi: 10.1007/s00374-002-0466-4

    Article  CAS  Google Scholar 

  25. Grogan, P., T.D. Bruns, and F.S. Chapin III. 2000. Fire effects on ecosystem nitrogen cycling in a Californian Bishop pine forest. Oecologia 122: 537–544. doi: 10.1007/s004420050977

    Article  CAS  Google Scholar 

  26. Hobbs, N.T., and D.S. Schimel. 1984. Fire effects on nitrogen mineralization and fixation in mountain shrub and grassland communities. Journal of Range Management 37: 402–404. doi: 10.2307/3899624

    Article  CAS  Google Scholar 

  27. Hogue, B.A., and P.W. Inglett. 2012. Nutrient release from combustion residues of two contrasting herbaceous vegetation types. Science of the Total Environment 431: 9–19. doi: 10.1016/j.scitotenv.2012.04.074

    Article  CAS  Google Scholar 

  28. Hoppe, H.G. 1983. Significance of exoenzymatic activities in the ecology of brackish water-measurements by means of Methylumbelliferyl-substrates. Marine Ecology-Progress Series 11: 299–308. doi: 10.3354/meps011299

    Article  CAS  Google Scholar 

  29. Inglett, P.W., and K.S. Inglett. 2013. Biogeochemical changes during early development of restored calcareous wetland soils. Geoderma 192: 132–141. doi: 10.1016/j.geoderma.2012.07.009

    Article  CAS  Google Scholar 

  30. Inglett, P.W., K.R. Reddy, and P.V. McCormick. 2004. Periphyton chemistry and nitrogenase activity in a northern Everglades ecosystem. Biogeochemistry 67: 213–233. doi: 10.1023/B:BIOG.0000015280.44760.9a

    Article  CAS  Google Scholar 

  31. Inglett, P.W., K.R. Reddy, B. Lorenzen, and S. Newman. 2007. Increased soil δ15N following phosphorus enrichment: historical patterns and tests of two hypotheses in a P-limited wetland. Oecologia 153: 99–109. doi: 10.1007/s00442-007-0711-5

    Article  CAS  Google Scholar 

  32. Inglett, P.W., V.H. Rivera-Monroy, and J.R. Wozniak. 2011. Biogeochemistry of nitrogen across the Everglades landscape. Critical Reviews in Environmental Science and Technology 41: 187–216. doi: 10.1080/10643389.2010.530933

    Article  CAS  Google Scholar 

  33. Kirby, R.E., S.J. Lewis, and T.N. Sexson. 1988. Fire in North American wetland ecosystems and fire-wildlife relations: an annotated bibliography. Biological Report 88(1), USDI Fish and Wildlife Service, Washington, DC, USA.

    Google Scholar 

  34. Liao, X., and P.W. Inglett. 2012. Biological nitrogen fixation in periphyton of native and restored Everglades marl prairies. Wetlands 32: 137–148. doi: 10.1007/s13157-011-0258-4

    Article  Google Scholar 

  35. Lockwood, J.L., M.S. Ross, and J.P. Sah. 2003. Smoke on the water: the interplay of fire and water flow on Everglades restoration. Frontiers in Ecology and the Environment 1: 462–468. doi: 10.1890/1540-9295(2003)001[0462:SOTWTI]2.0.CO;2

    Article  Google Scholar 

  36. Miao, S.L., and S. Carstenn. 2006. Assessing long-term ecological effects of fire and natural recovery in a phosphorus enriched Everglades wetland: cattail expansion, phosphorus biogeochemistry, and native vegetation recovery. Pages 3-1 to 3-42 in: South Florida Water Management District, editor. Options for accelerating recovery of phosphorus impacted areas of the Florida Everglades, research plan. South Florida Water Management District, West Palm Beach, Florida, USA.

    Google Scholar 

  37. Miao, S.L., and F.H. Sklar. 1998. Biomass and nutrient allocation of sawgrass and cattail along a nutrient gradient in the Florida Everglades. Wetlands Ecology and Management 5: 245–263. doi: 10.1023/A:1008217426392

    Article  Google Scholar 

  38. Mulvaney, R.L. 1996. Nitrogen-inorganic forms. Pages 1123–1184 in: D.L. Sparks, A.L. Page, P.A. Helmke, R.H. Loepper, P.N. Soltanpour, M.A. Tabatabai, C.T. Johnston, and M.E. Sumner, editors. Methods of soil analysis part 3: chemical methods. Soil Science Society of America, Madison, Wisconsin, USA.

    Google Scholar 

  39. Neary, D.G., C.C. Klopate, L.F. Debano, and P.F. Ffolliott. 1999. Fire effects on belowground sustainability: a view and synthesis. Forest Ecology and Management 122: 51–71.

    Article  Google Scholar 

  40. Ojima, D.S., D.S. Schimel, W.J. Parton, and C.E. Owens. 1994. Long- and short-term effects of fire on nitrogen cycling in tallgrass prairie. Biogeochemistry 24: 67–84. doi: 10.1007/BF02390180

    Article  Google Scholar 

  41. Qian, Y., S.L. Miao, B. Gu, and Y.C. Li. 2009. Estimation of postfire nutrient loss in the Florida Everglades. Journal of Environmental Quality 38: 1812–1820. doi: 10.2134/jeq2008.0391

    Article  CAS  Google Scholar 

  42. Raison, R.J. 1979. Modification of the soil environment by vegetation fires, with particular reference to nitrogen transformations: a review. Plant and Soil 51: 73–108. doi: 10.1007/BF02205929

    Article  CAS  Google Scholar 

  43. Rau, B.M., R.R. Blank, J.C. Chambers, and D.W. Johnson. 2007. Prescribed fire in a Great Basin sagebrush ecosystem: dynamics of soil extractable nitrogen and phosphorus. Journal of Arid Environments 71: 362–375. doi: 10.1016/j.jaridenv.2007.05.006

    Article  Google Scholar 

  44. Saa, M.A., C. Trasar-Cepeda, F. Gil-Sotres, and T. Carballas. 1993. Changes in soil phosphorus and acid phosphatase activity immediately following forest fires. Soil Biology and Biochemistry 25: 1223–1230. doi: 10.1016/0038-0717(93)90218-Z

    Article  CAS  Google Scholar 

  45. Sinsabaugh, R.L., S. Findlay, P. Franchini, and D. Fisher. 1997. Enzymatic analysis of riverine bacterioplankton production. Limnology and Oceanography 42: 29–38. doi: 10.4319/lo.1997.42.1.0029

    Article  CAS  Google Scholar 

  46. Smith, M.S., and J.M. Tiedje. 1979. Phases of denitrification following oxygen depletion in soil. Soil Biology and Biochemistry 11: 261–267. doi: 10.1016/0038-0717(79)90071-3

    Article  CAS  Google Scholar 

  47. Spier, L.P., and J.R. Snyder. 1998. Effects of wet- and dry-season fires on Jaquemontia curtisii, a South Florida pine forest endemic. Natural Areas Journal 18: 350–357.

    Google Scholar 

  48. Stock, W.D., and O.A.M. Lewis. 1986. Soil nitrogen and the role of fire as a mineralizing agent in a south African coastal fynbos ecosystem. Journal of Ecology 74: 317–328. doi: 10.2307/2260257

    Article  Google Scholar 

  49. Turner, C.L., J.M. Blair, R.J. Schartz, and J.C. Neel. 1997. Soil N and plant responses to fire, topography, and supplemental N in tallgrass prairie. Ecology 78: 1832–1843. doi: 10.1890/0012-9658(1997)078[1832:SNAPRT]2.0.CO;2

    Article  Google Scholar 

  50. Turner, M.G., E.A.H. Smithwick, K.L. Metzger, D.B. Tinker, and W.H. Romme. 2007. Inorganic nitrogen availability after severe stand-replacing fire in the greater Yellowstone ecosystem. Proceedings of the National Academy of Sciences 104: 4782–4789. doi: 10.1073/pnas.0700180104

    Article  CAS  Google Scholar 

  51. USEPA [US. Environmental Protection Agency]. 2012. Clean Water Act methods: approved general purpose methods. <>. Last accessed 12 December 2012.

  52. Vance, E.D., and G.S. Henderson. 1984. Soil nitrogen availability following long-term burning in an oak-hickory forest. Soil Science Society of America Journal 48: 184–190. doi: 10.2136/sssaj1984.03615995004800010034x

    Article  CAS  Google Scholar 

  53. Vazquez, F.J., M.J. Acea, and T. Carballas. 1993. Soil microbial populations after wildfire. FEMS Microbiology Ecology 13: 93–103.

    Article  Google Scholar 

  54. Vitousek, P. 1982. Nutrient cycling and nutrient use efficiency. American Naturalist 119: 553–572. doi: 10.1086/283931

    Article  Google Scholar 

  55. Vitousek, P.M., and R.W. Howarth. 1991 Nitrogen limitation on land and in the sea: how can it occur? Biogeochemistry 13: 87–115 doi: 10.1007/BF00002772

    Article  Google Scholar 

  56. Wan, D.H., and Y. Luo. 2001. Fire effects on nitrogen pools and dynamics in terrestrial ecosystems: a meta-analysis. Ecological Applications 11: 1349–1365. doi: 10.1890/1051-0761(2001)011[1349:FEONPA]2.0.CO;2

    Article  Google Scholar 

  57. Wardle, D.A., O. Zackrisson, and M.C. Nilsson. 1998. The charcoal effect in boreal forest: mechanisms and ecological consequences. Oecologia 115: 419–426. doi: 10.1007/s004420050536

    Article  CAS  Google Scholar 

  58. White, J.R., and K.R. Reddy. 1999. The influence of nitrate and phosphorus loading on denitrifying enzyme activity in Everglades wetland soils. Soil Science Society of America Journal 63: 1945–1954. doi: 10.2136/sssaj1999.6361945x

    Article  CAS  Google Scholar 

  59. White, J.R., and K.R. Reddy. 2000. The effects of phosphorus loading on organic nitrogen mineralization of soils and detritus along a nutrient gradient in the northern Everglades, Florida. Soil Science Society of America Journal 64: 1525–1534. doi: 10.2136/sssaj2000.6441525x

    Article  CAS  Google Scholar 

  60. Zackrisson, O., M.C. Nilsson, and D.A. Wardle. 1996. Key ecological function of charcoal from wildfire in the boreal forest. Oikos 77: 10–19. doi: 10.2307/3545580

    Article  Google Scholar 

  61. Zackrisson, O., T.H. DeLuca, M.C. Nillsson, A. Sellstedt, and L.M. Berglund. 2004. Nitrogen fixation increases with successional age in boreal forests. Ecology 85: 3327–3334. doi: 10.1890/04-0461

    Article  Google Scholar 

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We thank the following for their help in this work. Field support was provided by L. Serra, C. Fisher, and A.S. McKinley (US National Park Service); and D. Irick, B. Hogue, A. Baker, and A. Brestel (University of Florida). Prescribed fire was conducted by the members of the Everglades Fire Operations Program, and the authors would like to thank T.Z Osborne (University of Florida) for his assistance with the burn. Laboratory assistance was provided by Y. Wang and F.G. Wilson of the Wetland Biogeochemistry Laboratory (University of Florida). This research was funded by grant J5297-07-0276 from the US National Park Service and the Everglades National Park, Hole-in-the-Donut Wetland Restoration Project.

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Liao, X., Inglett, P.W. & Inglett, K.S. Fire Effects on Nitrogen Cycling in Native and Restored Calcareous Wetlands. fire ecol 9, 6–20 (2013).

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  • aminopeptidase
  • denitrification
  • marl
  • nitrogen fixation
  • periphyton
  • restoration