Skip to main content
  • Research article
  • Open access
  • Published:

Can differences in phosphorus uptake kinetics explain the distribution of cattail and sawgrass in the Florida Everglades?



Cattail (Typha domingensis) has been spreading in phosphorus (P) enriched areas of the oligotrophic Florida Everglades at the expense of sawgrass (Cladium mariscus spp. jamaicense). Abundant evidence in the literature explains how the opportunistic features of Typha might lead to a complete dominance in P-enriched areas. Less clear is how Typha can grow and acquire P at extremely low P levels, which prevail in the unimpacted areas of the Everglades.


Apparent P uptake kinetics were measured for intact plants of Cladium and Typha acclimated to low and high P at two levels of oxygen in hydroponic culture. The saturated rate of P uptake was higher in Typha than in Cladium and higher in low-P acclimated plants than in high-P acclimated plants. The affinity for P uptake was two-fold higher in Typha than in Cladium, and two- to three-fold higher for low-P acclimated plants compared to high-P acclimated plants. As Cladium had a greater proportion of its biomass allocated to roots, the overall uptake capacity of the two species at high P did not differ. At low P availability, Typha increased biomass allocation to roots more than Cladium. Both species also adjusted their P uptake kinetics, but Typha more so than Cladium. The adjustment of the P uptake system and increased biomass allocation to roots resulted in a five-fold higher uptake per plant for Cladium and a ten-fold higher uptake for Typha.


Both Cladium and Typha adjust P uptake kinetics in relation to plant demand when P availability is high. When P concentrations are low, however, Typha adjusts P uptake kinetics and also increases allocation to roots more so than Cladium, thereby improving both efficiency and capacity of P uptake. Cladium has less need to adjust P uptake kinetics because it is already efficient at acquiring P from peat soils (e.g., through secretion of phosphatases, symbiosis with arbuscular mycorrhizal fungi, nutrient conservation growth traits). Thus, although Cladium and Typha have qualitatively similar strategies to improve P-uptake efficiency and capacity under low P-conditions, Typha shows a quantitatively greater response, possibly due to a lesser expression of these mechanisms than Cladium. This difference between the two species helps to explain why an opportunistic species such as Typha is able to grow side by side with Cladium in the P-deficient Everglades.


The wetland species, Cladium mariscus ssp. jamaicense (L.) Pohl (Crantz) K. Kenth (sawgrass; hereafter Cladium) and Typha domingensis Pers. (cattail; hereafter Typha) are both native to the Florida Everglades and occupy similar habitats [1]. Cladium was the dominant plant species in the historical freshwater Everglades, whereas Typha was a minor species occurring in small and scattered patches throughout the Everglades [2]. However, during the past decades Typha has expanded rapidly and replaced thousands of hectares of Cladium marshes and aquatic slough areas in the northern part of the Everglades [36]. Numerous studies have been conducted to assess the causes and the consequences of this change in vegetation and community structure [720], and the driving force for the change appears to be nutrient enrichment, particularly phosphorus (P), from agricultural runoff and Lake Okeechobee outflow [21].

Cladium and Typha are both large, clonal species that can form monospecific communities in freshwater habitats. The two species differ, however, in morphology, growth, and life history characteristics [10, 15, 22]. Cladium exhibits many characteristics of adaptation to infertile environments, such as slow growth rate, long leaf longevity, low capacity for nutrient uptake, low leaf nutrient concentrations and a relatively inflexible partitioning of biomass in response to increased nutrient availability [23, 24]. Typha, on the other hand, has traits of an opportunistic species from nutrient-rich habitats with high growth rates, short leaf longevity, high capacity for nutrient uptake, high leaf nutrient concentrations and flexible biomass partitioning [8, 25]. Both species are adapted to grow in waterlogged soils by virtue of a well-developed aerenchyma system, but convective gas flow has been documented only in Typha and not in Cladium [2629]. Furthermore, Cladium has lower root porosity and generally higher alcoholic fermentation rates, indicating lower capacity for root aeration than Typha [30]. These inherently different traits are considered the main explanation for the rapid spread and competitive success of Typha in the P-enriched areas of the Florida Everglades.

Cladium and Typha also co-exist in the oligotrophic areas of the Florida Everglades where P availability is extremely low. In the interior of Water Conservation Area 2A, an impounded area in the northern Everglades, Cladium and Typha grow together despite soluble P concentrations of less than 4 μg l-1 in the porewaters throughout the soil profile [31]. Typha is much less abundant than Cladium and has slow growth rates in these areas [32], and although nutrient enrichment and disturbance around alligator holes have been suggested to favour the proliferation of Typha locally [33], the traits that allow the growth of a high resource-adapted plant like Typha in this low P environment are not understood.

Studies at high P availability have demonstrated that Typha has a greater relative growth rate, a greater allocation of biomass to leaves, and a lower P-use efficiency than Cladium [10, 15, 16]. In fertile habitats, a high nutrient uptake capacity per unit of root biomass and a high growth rate and biomass allocation to leaves increase the capability to compete for light and reduce the need for a high root biomass. However, these traits are not advantageous for growth in a nutrient deficient environment where plants must acquire nutrients at low availability and minimize nutrient losses [34]. In such conditions, optimal features would include an extensive root system for soil exploration, a high root surface area (long, thin roots and/or root hairs) for acquisition of nutrients, and efficient mechanisms to capture nutrient ions at low external concentrations [3537].

The main research question we address here is: Which characteristics of Cladium and Typha allow the species to grow in the oligotrophic P-deficient interior of the Florida Everglades, and at the same time explain why Typha out-competes Cladium under P-enriched conditions? As to the second part of the question, abundant evidence in the literature explains how the opportunistic features of Typha can lead to complete dominance in P-enriched areas [e.g. [7, 8, 13, 15]]. Less clear is how Typha can grow and acquire P at the extreme low P-levels prevailing in the unimpacted areas of the Everglades.

We hypothesized that Typha has a more plastic P uptake system than Cladium in relation to P availability, and this strategy will allow adequate uptake of P and better competitive ability over a wide range of external P concentrations. Furthermore, we hypothesized that oxygen-deficient conditions will affect the uptake kinetics of Cladium more than that of Typha, as the latter species has a more efficient system for root aeration (via aerenchyma and internal convective gas flow). These hypotheses were tested in a series of P uptake experiments designed to distinguish differences in P uptake kinetics between the two species.

Apparent P uptake kinetics were measured for whole plants of Cladium and Typha grown from seeds and acclimated to identical, steady state conditions, in a factorial treatment arrangement with two levels of P (5 and 500 μg P l-1) and two levels of oxygen (8.0 and <0.5 mg O2 l-1) in hydroponic culture solutions (n = 4-8). The P uptake kinetic parameters were estimated using a modified Michaelis-Menten model [3841].


Plant characteristics

The plants used in the uptake studies all appeared healthy, with no visual signs of nutrient deficiencies. However, long acclimation periods in the various culture combinations (up to 4 months in the low P treatments) inevitably created plants with different biomass, allocation patterns, and tissue nutrient concentrations. Overall the shoot height (average 0.95 m) and root length (average 0.37 m) of the two species varied little across the treatments, but the plant weights and biomass allocation differed significantly (table 1). Low-P acclimated plants had less biomass than high-P acclimated plants, and significantly (P < 0.001) more biomass allocated to roots. Typha in particular allocated less biomass to roots in the high P treatment (table 1). Plants in the low oxygen cultures had 25% shorter root systems than those in aerated cultures (P < 0.001), but the oxygen treatment did not affect the proportion of biomass allocated to roots (P > 0.05).

Table 1 Plant size

The tissue N concentrations in Cladium were similar (average 10.4 mg g-1 dry weight) in all treatments, and lower overall than in Typha (approximately 17 mg g-1 dry weight), except in the aerated, low-P treatment where plants were smaller (figure 1). The tissue P concentrations were, as expected, more variable across treatments, and were generally higher (P < 0.001) in the high P treatment (average 3.1 mg g-1 dry weight) than in the low P treatment (average 1.1 mg g-1 dry weight). Moreover, the tissue P concentrations were consistently higher in the low oxygen treatments than in the corresponding aerated treatments (figure 1). However, tissue P analyses were carried out on tissues harvested after the uptake kinetic studies, in which plants were exposed to high P concentrations (up to 500 μg l-1) for several hours. Uptake during the uptake studies may have contributed to enhance the tissue concentration by 0.4-0.7 mg P g-1 dry weight. Hence, the tissue P concentrations in the low-P acclimated plants presented here are likely higher than they would have been if plants were collected for analysis before the uptake kinetic studies.

Figure 1
figure 1

Plant tissue N and P concentrations. Average (± SE) concentrations of nitrogen (N) and phosphorus (P) (mg g-1 dry weight) in whole plants of Cladium mariscus spp. jamaicense and Typha domingensis acclimated to low (5 μg l-1) and high (500 μg l-1) P concentrations and high (+O2: 8 mg l-1) and low (-O2: <0.5 mg l-1) oxygen concentration in the culture solutions.

Phosphorus uptake kinetics

The relationships between solution P concentrations and the net rate of P uptake of selected Cladium and Typha plants acclimated to low P and to high P levels are shown in figure 2. Generally, the modified Michaelis-Menten model fitted the relationships and estimated the kinetic uptake parameters with high statistical confidence. Vmax was entered as a fixed parameter in the model and was estimated as the average uptake rate at solution P concentrations where uptake appeared to be saturated. At the low concentration range, where P uptake increases nearly linearly with solution P concentration, the model fitted the data very well, but the uncertainty associated with estimating Cmin for high-P acclimated plants was relatively large. The Cmin values presented for these conditions are therefore uncertain and should be interpreted accordingly.

Figure 2
figure 2

P uptake kinetic curves. Examples of relationships between the concentration of inorganic phosphorus (P) in the root chambers and the rate of P uptake of single specimens of (A) Cladium mariscus spp. jamaicense and (B) Typha domingensis acclimated to low (5 μg l-1) P concentrations (solid lines and closed symbols) and to high (500 μg l-1) P concentrations (dashed lines and open symbols). Plants were grown at low (<0.5 mg l-1) oxygen concentration in culture solutions. Uptake was measured by P depletions of root solutions followed by stepwise increments of the P concentrations. The relationship was fitted to a modified Michaelis-Menten model (curves).

P uptake capacity

The saturated rate of P uptake (Vmax) differed significantly between species and was also affected by both P treatment and oxygen level, but the effects of oxygen differed between P treatments as shown by a significant interaction in the ANOVA (table 2). Across treatments the average Vmax was 38% higher in Typha than in Cladium and the Vmax of low-P acclimated plants was overall more than three-fold higher than the Vmax of high-P acclimated plants (figure 3a and table 2). Vmax was generally more than two-fold higher in the low oxygen treatment compared to the high oxygen treatment, except for Typha from the high P treatment, where rates were equal.

Table 2 Results of ANOVA for uptake kinetics
Figure 3
figure 3

P uptake kinetic parameters. Average (± SE) phosphorus (P) uptake kinetic parameters for Cladium mariscus spp. jamaicense and Typha domingensis acclimated to low (5 μg l-1) and high (500 μg l-1) P concentrations and high (+O2: 8 mg l-1) and low (-O2: <0.5 mg l-1) oxygen concentration in the culture solutions. Uptake was measured by P depletions of root solutions followed by stepwise increments of the P concentrations. The kinetic parameters: (A) Vmax (maximum uptake at saturating P concentration), (B) K0.5 (half saturation constant), and (C) Cmin (P concentration where there is no net uptake) were estimated by fitting to a modified Michaelis-Menten model.

Half saturation constant

The half saturation constant (K0.5) differed significantly between the two species and was also affected by the P treatment, but the effects of P treatment differed between species as shown by the significant interactions in the ANOVA (table 2). Across treatments the half saturation constants were approximately 70% higher in Cladium than in Typha, indicating that Cladium overall has a lower affinity for P uptake than Typha (figure 3b). In Typha the half saturation constants did not differ much across treatments, but in Cladium the half saturation constants were 1.5-2.5 times higher in the high-P acclimated plants than in low P plants. Oxygen did not significantly affect K0.5.

Minimum P concentration

The solution P concentration at which there was no net uptake, Cmin, was significantly affected by the treatments as shown by the significant interactions in the ANOVA (table 2). On average, low-P acclimated Cladium and Typha plants had a Cmin of 3.5 and 9.9 μg P l-1, whereas high-P acclimated plants had a Cmin of 43 and 25 μg P l-1, respectively (figure 3c). However, in the low P-aerated treatments both species had a low Cmin (1.2 μg P l-1). For high-P acclimated plants Cmin was significantly higher (18-64 μg l-1) and the effects of oxygen differed between the species (figure 3c).

Affinity for P-uptake

The slope of the initial linear part of the uptake curve at low P solution concentrations, α, as well as the ratio between Vmax and K0.5, are measures of the uptake affinity. Both affinity measures were significantly affected by plant species, P acclimation and oxygen level, and effects of oxygen level differed between the P treatments (table 2). Overall the affinity for P uptake by Typha was two-fold higher than that of Cladium, and affinities were 2 to 3 times higher for low-P acclimated plants compared to high-P acclimated plants (table 3). Both species had higher P uptake affinities in low oxygen treatments, and the effects of oxygen were greatest for low-P acclimated plants. The highest affinity was found for low P and low oxygen acclimated Typha plants. Numerically, the affinities derived from the initial slope of the curves (α) were higher than the affinity measures derived from the Michaelis-Menten model (Vmax/K0.5), but the overall treatment effects were alike.

Table 3 Affinity for P uptake


Ecophysiological studies on nutrient uptake kinetics must be conducted using hydroponically grown plants rather than in soil. Although it is possible to mimic the porewater composition of wetland soils in terms of major nutrient ions and pH, the growth conditions in hydroponic cultures differ significantly from those of wetland soils, particularly oxygen and redox conditions [4244]. In wetland soils, porewaters are nearly always oxygen-free and may contain variable concentrations of reduced ions and organic compounds resulting in low redox potentials depending on soil organic content, nutrient status and other factors. In hydroponic plant culture, the solution is usually aerated to ensure a good oxygen supply for roots. However, in wetland soils, the root oxygen is delivered from the atmosphere via internal transport through the aerenchyma, and so oxygen supply to support aerobic metabolism within root cells potentially differs considerably [27]. Our experimental conditions mimicked the low oxygen conditions in wetland soils by flushing culture solutions with gaseous N2. This treatment maintained oxygen in culture solutions at levels less than 0.5 mg l-1 and so provided a largely anoxic, but not highly reducing, root environment. The growth of the plants was little affected by the oxygen treatments, except for Typha root length, which was shorter in the low oxygen treatments.

Except for Typha at high P, tissue P concentrations were higher in the low oxygen treatment (figure 1), and uptake kinetics were also significantly affected by oxygen (figure 4). In waterlogged, anoxic soils, plants have been reported to produce less root biomass with a greater P uptake per unit of root mass than in drained soils [45]. This response has been ascribed to a combination of increased P availability in waterlogged soils and a higher physiological capacity of roots to absorb P, although the mechanisms are not known [4547]. In the present study, oxygen treatment likely did not affect P availability in the solution cultures. Also, root morphology did not change in response to the oxygen treatments. We, therefore, suggest that the observed differences in uptake characteristics were related to the effects of oxygen on the function and/or expression of the high affinity ion transporters in the root plasma membranes. Plants acquire P in the form of phosphate anions, mostly H2PO4 -, from the soil solution, and uptake occurs against a steep concentration gradient (three orders of magnitude or greater) across the plasmamembrane [34, 48]. Many uptake models have been proposed to explain the ability of plants to acquire P both under deficiency and sufficiency conditions [34, 35, 48, 49]. A dual uptake model involving both a high affinity uptake system (HATS) operating at low (<200 μM) concentrations, and a low affinity uptake system (LATS) operating at high (>1 mM) concentrations is widely used to explain the concentration-dependent uptake of nutrient ions [48]. In P-deficient soils only the HATS is operating, apparently with multiple phosphate transporters located in the plasmamembrane through which the energy-mediated uptake occurs [49]. In general, plants respond to nutrient deprivation by increasing uptake affinity as well as uptake capacity [50]. The lack of response to oxygen of high-P acclimated plants, however, indicates that the high affinity transporters are regulated more by P demand than oxygen.

Figure 4
figure 4

P uptake curves. Average estimated uptake of phosphorus (μg P g-1 root dry weight h-1) as a function of solution inorganic P concentration for Cladium mariscus spp. jamaicense and Typha domingensis acclimated to low P (5 μg l-1) and high P (500 μg l-1) concentrations and high oxygen (8 mg l-1; dashed lines) and low oxygen (<0.5 mg l-1; solid lines) concentration in the culture solutions. The curves were generated by the modified Michaelis-Menten model using the average kinetic parameters for the two species in the different treatments.

We hypothesized that oxygen-deficient conditions would affect the uptake kinetics of Cladium more than that of Typha because of differences in their inherent ability to transport oxygen to the roots. This hypothesis could not be verified, because of the confounding effects of P availability. At low P, oxygen affected uptake kinetics more for Typha than for Cladium whereas at high P the effects were small and mostly on Cladium. In earlier studies [[14], and unpublished], low oxygen and particularly reducing (Eh-150 mV) soil conditions significantly reduced growth and performance of both Cladium and Typha when P availability was low, but the effects could be largely ameliorated by high P availability. A similar tendency was observed in the present study: effects of oxygen were most pronounced at low P, and nearly disappeared at high P.

Our primary aim was to assess whether differences in P uptake kinetics could explain the observed growth characteristics of the two species in the Everglades. To achieve this goal, we have focused this discussion on plant responses under low oxygen, as this resembles the environmental conditions in the Everglades soils better than the aerated culture solutions. Under low oxygen and high P availability, Vmax did not differ much between the species, but the affinity for P (Vmax/K0.5 and α) was significantly lower for Cladium than Typha. However, Cladium had a greater proportion of the biomass allocated to roots, so overall uptake capacity of the two species at high P did not differ much. Root P uptake was largely controlled by the plant P demand. Although we did not investigate ion transport regulation, uptake kinetics may have adjusted via regulation of the membrane-bound high affinity ion transporters [51, 52]. These results imply that under P-sufficient conditions, uptake kinetics does not influence competition between the two species. With sufficient P, the plants only need to adjust their uptake system to meet their respective P demands.

At an external concentration of inorganic P of only 5 μg l-1, P is certainly growth limiting for both species, as has been shown in many previous studies [14, 15]. Plants may respond to such P-deficient conditions in several ways, including allocation of greater mass to roots relative to shoots, and the production of thinner and longer roots enhancing total surface area for nutrient acquisition [53]. In this study, the proportion of biomass allocation to roots increased for both Cladium (from 14 to 18%) and Typha (from 8 to 15%), but there were no changes in root morphology to increase absorptive area. Both species also adjusted their P uptake system in an attempt to obtain adequate P, but Typha more so than Cladium. The maximum uptake velocity, Vmax, increased by a factor of 5.3 and 3.1; the half saturation constant, K0.5, decreased by a factor 0.14 and 0.54; and the P uptake affinity, Vmax/K0.5 and α, increased by a factor 3.9-6.2 and 4.0-4.5 for Typha and Cladium, respectively. The estimated levels of Cmin (about 6 and 19 μg l-1 in the low-P treatment for Cladium and Typha, respectively) are obviously too high, as plants were growing and taking up P at 5 μg l-1. The depletion methodology used in this study, which included spiking with P to relatively high levels, may have resulted in the build-up of internal pools of P that interfered with the estimation of the true Cmin values. When Cladium and Typha plants were grown for 30 days in solution cultures with a low supply of P, both species maintained concentrations of 2-3 μg P l-1 in the solutions (unpublished results). We therefore suggest that the true Cmin level for the two species is in this range.

The adjustment of the P uptake system under low P conditions for Cladium and Typha increased the uptake velocity per unit of root mass 4 to 5-fold compared to the velocities for high-P acclimated plants. Adding the simultaneous increased biomass allocation to roots, the adjustment would result in a 5-fold higher P uptake per plant for Cladium and a 10-fold higher uptake for Typha. The combined effect of these adjustments is that the P uptake per plant would be alike for low-P acclimated plants at a solution concentration of ~35 μg P l-1 and for high-P acclimated plants at a solution concentration of ~500 μg P l-1 for both species. Actual plant uptake at 5 μg l-1 was of course much lower, as plants grew slower and had lower tissue P concentrations.

Adjustment of the uptake system, particularly Vmax, when plants are exposed to nutrient deficiency is a common response observed by many species and many nutrient ions. The affinity for nutrient uptake as expressed by K0.5 is commonly assumed to be less plastic and less affected by plant growth conditions than Vmax [34, 45, 52]. However, the slope of the uptake curve at low P concentrations, α, and the ratio between Vmax and K0.5 (Vmax/K0.5) are better measures of affinity than K0.5. In the present study, these affinity measures were clearly affected by P availability in a manner similar to Vmax.

A high uptake affinity becomes increasingly important in P-deficient soils, where P uptake is controlled largely by the rate of diffusion to the depleted zones around the roots [54]. The fact that Typha adjusts the affinity for P uptake and root biomass more than Cladium and that Typha has thinner root laterals than Cladium [15], increases this species' capacity to extract P from low P solutions relative to Cladium. However, despite an apparently less efficient uptake system, Cladium outperforms Typha during prolonged growth under P-deficient conditions (unpublished). Increased allocation of biomass by Typha to roots may reduce its capacity to maintain a balanced acquisition of C and other resources and result in poor growth at P-deficient conditions. Hence, an efficient P uptake system alone does not ensure good performance at persistent low P availability.

Besides optimising the physiology of root P uptake, plants may also increase the availability of P in the rhizosphere by releasing specialized enzymes, known as phosphatases, which hydrolyse soluble organic P derived from soil organic matter to ortho-P for plant uptake [55]. Both Cladium and Typha secrete phosphatases at low P availability, but the rate of secretion is higher in Cladium, enhancing hydrolysis of organic P compounds [56]. Another means of P acquisition from P-deficient soils is symbiosis with arbuscular mycorrhizal fungi [57]. Inoculation of Cladium with arbuscular mycorrhizal fungi in a greenhouse pot experiment increased growth and P uptake of Cladium significantly [58]. These additional capabilities are clearly important for acquiring sufficient P from the peat-based, low-P soils of the Everglades, where P is stored primarily as organic P with an additional component of Ca-bound P [59, 60]. The ability of Cladium to access organic P fractions, in concert with its slow growth rate, long tissue life time and high P-use efficiency, likely explains why this species is prolific in the P-deficient Everglades soils.


A main finding of our study was that Typha has a more plastic P uptake system than Cladium that allows uptake of P over a wide range of external P concentrations and promotes high growth rates with a relatively low investment in root mass at high P levels. Both species adjust P uptake kinetics in relation to plant demand when P availability is high, but because of its opportunistic traits, Typha is more likely to outcompete Cladium in P-enriched areas. Under P-deficient conditions Typha adjusts P uptake kinetics and biomass allocation to roots more than Cladium, and thereby achieves very efficient acquisition of P at low P levels. In contrast, Cladium has less need to adjust its P uptake kinetics in response to low P conditions probably because it is already efficient at acquiring P from peat-based soils (e.g., through secretion of phosphatases, symbiosis with arbuscular mycorrhizal fungi, and efficient nutrient conservation growth traits). These findings suggest that differential expression of a similar strategy by Cladium and Typha under low-P conditions explains why an opportunistic species like Typha is able to grow side by side with Cladium in the persistently P-deficient Everglades.


Experimental setup

Phosphorus uptake kinetics were measured for whole plants of Cladium and Typha acclimated in a factorial setup with two levels of P (5 and 500 μg P l-1) and two levels of oxygen (8.0 and <0.5 mg O2 l-1) in hydroponic culture solutions. Since P availability and internal pools of P in the plant tissues are known to affect plant development and physiology, and hence P uptake characteristics, special care was taken to ensure that plants were germinated and propagated at the desired P treatment concentrations. This was achieved by propagating plants from seeds hydroponically in growth cabinets with efficient control of the nutrient composition of the culture solutions. The P uptake kinetic parameters were estimated for whole individual plants of the two species in a controlled environment, the "PhytoNutriTron" (PNT), which is a computer controlled growth facility with four independent steady state hydroponic rhizotrons built into growth cabinets [61].

Seeds and germination

Seeds of Typha and Cladium were collected from populations of the two species in the oligotrophic interior of Water Conservation Area 2A in the northern Everglades and germinated on vermiculite at a 14:10 h day:night photoperiod and a 25:10°C thermoperiod, a climatic regime shown to be optimal for germination of the two species [62]. The seedlings were watered with a basic nutrient solution (table 4) at pH 6.5 with additional phosphorus added as K2HPO4 to obtain the two P levels (5 and 500 μg l-1). The composition of the nutrient solution was developed to resemble the porewater concentrations of the major nutrient ions in the interior oligotrophic area of Water Conservation Area 2A of the Everglades. When plants had developed a root system that was large enough to allow the mounting of plants in hydroponic culture (after 3 to 5 months), the seedlings were transferred to a hydroponic nursery culture system.

Table 4 Hydroponic nutrient solutions

Plant acclimation in nursery system

The plants were acclimated to hydroponic growth at low and high P levels (5 and 500 μg l-1) in a nursery system that was set up in a growth chamber operated at a 15 h light/9 h dark cycle, a 30:25°C thermocycle and a 85:90% relative air humidity day:night cycle. Light was provided by a combination of inflorescent light tubes and metal halide bulbs at a photon flux density of 350 μmol m-2 s-1 (PAR) at the base of the plants. Between day and night, the climatic parameters were changed gradually over a one hour transition period. The nursery contained four independent hydroponic growth units, each consisting of one or two 30 litre aerated growth tanks with up to 22 plants. The tanks of each growth unit were connected to a 360 litre external nutrient solution reservoir. The culture solution was recirculated between the reservoir and the growth tanks by pumps delivering 6 litre min-1 of solution to each growth tank. The culture solution consisted of the basic nutrient solution, and phosphorus was adjusted to the experimental levels using the P addition stock solution (table 4). The NH4 + level was adjusted with a solution of (NH4)2SO4. Changes in nutrient concentrations in the culture solutions were minimized through daily monitoring and adjustment of concentration levels. On weekdays, pH was adjusted to pH 6.5, and 112 μg Fe l-1 (FeSO4) was added to each unit. Temperature and conductivity were registered and the concentrations of NH4 + and PO4 3- were analysed using standard colorimetric methods (Lachat Instruments, Milwaukee, WI, USA). Orthophosphate detection was based on the ascorbic acid method (Method EPA-600/4-79-020, 1983, U.S. Environmental Protection Agency) and NH4 + was analysed using the salicylate method (Ammonia in waters 1981, London, Her Majesty's Stationary Office). Changes in conductivity during operation of the nursery were minimized by intermediate renewal of approximately 75% of the culture solutions when conductivity reached 2 mS cm-1. After 2 to 4 months, depending on species and treatment, when the plants started to produce rhizomes and ramets, individual plants were transferred to the controlled environment of the PNT.

Controlled environment

The uptake experiments were carried out in the PNT, which is a computer controlled hydroponic growth facility for experiments with whole plants [61]. The hydroponic rhizotron system of the PNT consisted of four independent growth units each containing eight root vessels built into a controlled growth chamber in a block design. The growth chamber regulated air temperature, humidity and light intensity (maximum 1200 μmol m-2 s-1 PAR at the base of the plants) in day:night cycles similar to those of the nursery. Each of the four growth units was connected to a separate steady state, temperature (27°C), pH (6.5) and oxygen controlled reservoir (180 l) through which the culture solution was recirculated. The reservoirs were equipped with UV-sterilization units, and the concentrations of NH4 + and PO4 3- were monitored continuously by an auto-analyzer using standard colorimetric methods (Lachat Instruments, Milwaukee, WI, USA). The nutrient concentrations were maintained at constant levels through computer-mediated feedback regulation of peristaltic pumps that delivered the P nutrient stock solution and a (NH4)2SO4 stock solution to the reservoirs. The nutrients were supplied continuously at rates equivalent to their depletion in the culture solutions. The reservoirs and the root vessels were sealed from the atmosphere and flushed with either N2 gas or atmospheric air to control solution oxygen at the desired levels (<0.5 and 8 mg l-1, respectively). Each root vessel (height 700 mm, diameter 80 mm) had a lid with two openings for plants. The culture solution was circulated through each vessel at a rate of 4 litre min-1. The use of the P nutrient stock solution and partial replacement of the culture solutions (approximately 60% of the volume) ensured that concentrations of the major nutrients were maintained within ± 10% of desired set point level during the acclimation periods in PNT.

The four growth units of the PNT were used in sequence to create the 8 different treatment combinations (2 P levels × 2 species × 2 O2 levels). In order to optimize the control system for P detection, experiments with low and high-P acclimated plants were carried out separately. Between four and eight plants of each species for each treatment were selected at random from the stock of plants in the nursery unit. New ramets, rhizomes and senescent plant parts were removed from the plants before they were mounted in the root vessels of the PNT. The plants were acclimated to the steady state nutrient and oxygen levels in the controlled rhizotrons for at least one month prior to measurement of nutrient uptake.

Nutrient uptake kinetics

Plant P uptake was measured by the rate of depletion from nutrient solutions using an automated flow injection analyzer with four PO4 3- channels (Lachat Instruments, Milwaukee, WI, USA). Orthophosphate detection was based on the ascorbic acid method (Quickchem method no. 10-115-01-1-A (low sensitivity) and 10-115-01-1-B (high sensitivity), Lachat Instruments). At least 16 h before uptake kinetic studies were initiated, four plants were selected at random from the plants in the PNT. The roots were carefully rinsed in nutrient solution, and depending on plant size, transferred to root chambers with a volume between 0.7 and 12 litre (figure 5). The solution levels in the root chambers were marked and the chambers were placed in one of the growth cabinets of the PNT. Each root chamber was placed in a 10 litre tank containing 7 litre of nutrient solution. Centrifugal pumps recirculated water between the tanks and the root chambers at a rate of 1 litre min-1. Magnetic stirrers ensured mixing of the nutrient solutions in the root chambers, and depending on treatment, the chambers were flushed with atmospheric air or N2 gas at a rate 0.5 litre min-1.

Figure 5
figure 5

Experimental chamber used for uptake studies. Schematic diagram of the experimental system used to estimate the plant P uptake showing the connection between the plant chamber and the flow injection analyzer (FIA) used for PO4 3- detection. 1: Acrylic root chamber with diffuser for flushing with air or N2; 2: Collar and seal for plant mounting; 3: Magnetic stirring bar protected by a net; 4: High speed peristaltic pump for recirculation of solution in the root chamber; 5: Tee pieces; 6: Three-way valves for calibration of FIA; 7: Peristaltic pump of the FIA; 8: Six port valve of a FIA analyzer channel.

One hour before the initiation of the uptake kinetics studies, the circulation between the root chambers and the solution in the external tank was stopped, and the root chambers were flushed five times with a nutrient solution containing 5 μg P l-1. Thereafter, uptake studies were initiated by measuring a series of P depletion rates at stepwise increasing levels of P. The concentration of P was increased from 5 to 500 μg P l-1 in steps of 5 to 50 μg P l-1 followed by periods where the rates of depletion were measured. The root chamber was connected to the flow injection analyzer (FIA) through tubing (figure 5). A high-speed peristaltic pump (figure 5, item 4) recirculated solution through two tee-pieces connected to the FIA. The peristaltic pump of the FIA pumped the solution through a three-way valve connected to the recycling flow and to calibration solutions and back into the recycling flow line through the six-port valve of the analyzer. A three-way valve connected the return flow line from the FIA to the drain in order to collect sample water during instrument calibration. The setup ensured that no solution was lost during sampling, except for the volume extracted by the FIA for P analysis. During measurement of P depletion the sample rate was 20 per hour with a sample volume of 780 μl. The extracted volume was replaced with a complete nutrient solution but without P. Calibration of the analyzer channels was performed at regular intervals during the depletion series. The loss of test volume during the measurements due to evapotranspiration, was replaced with distilled water. pH was maintained at 6.5 ± 0.5 by addition of NaOH when necessary.

Plant tissue measurements

At the end of the depletion experiments, the length of the root and shoot system was measured and plants were separated into roots, leaves, rhizomes and ramets, rinsed in deionised water, and the fresh weights (FW) were recorded before drying in a forced ventilated oven for 48 hours at 80°C for dry weight (DW) determination. The dried plant material was then finely ground and analyzed for N using a N-protein analyzer (Na2000, Carlo Erba, Milan, Italy). The concentrations of P in the plant fractions were analyzed using an ICP-AES (Plasma II, Perkin-Elmer, CT, USA) after HNO3 and H2O2 digestion [63]. The concentration of N and P in the plant fractions and the weight proportions of the fraction were used to calculate the nutrient concentration on a plant basis.

Estimation of uptake kinetics parameters

The P uptake rates were estimated by linear regression analysis of 3 to 5 consecutive samples of P concentrations measured during depletion. The slopes of the regression lines were corrected for the loss due to sampling by the flow injection analyzer, and divided by root dry weight to obtain the P uptake rate (μg P g-1 root DW h-1). Data collected during the initial 8 to 12 minutes after a shift in P concentration in the root chambers were omitted from the analyses in order to ensure that equilibrium between apoplastic and the external P concentrations was achieved.

The relationship between solution P concentration (C) and uptake rates (V) was plotted and fitted by a modified Michaelis-Menten model [3841]:

The kinetic constants in this model are: Vmax, the maximum uptake velocity at saturating ion concentration; K0.5 (= K + Cmin), the half-saturation constant where uptake is 50% of Vmax; and Cmin, the ion concentration at which there is no net inflow. Vmax is a measure of the uptake capacity, and K0.5 as well as the ratio between Vmax and K0.5 are measures of the affinity of the uptake system. Also the slope, α, of the initial linear part of the uptake curve is a measure of affinity. This model has been successfully used in many studies to assess the underlying mechanisms responsible for up-regulating and down-regulating influx of different nutrient ions into whole plants, as well as the acclimations of the uptake system to different environmental conditions [39, 40, 61, 6467]. Vmax was entered into the model as a fixed parameter, and was estimated prior to the fitting as the average of the maximum uptake rates registered in a run. The modified Michaelis-Menten equation was fitted to the experimental data by means of a non-linear regression analysis using the Marquardt method (Statgraphics ver. 3, Manugistics, Inc., Maryland, USA). Two measures for P uptake affinity was calculated: (1) the ratio between Vmax and K0.5 (Vmax/K0.5); and (2) the slope, α, of the initial linear part of the uptake curve as estimated by linear regression analysis.


All statistics were carried out using the software Statgraphics ver. 3 (Manugistics, Inc., Maryland, USA). The difference in uptake kinetic parameters between the two species and the effects of growth P level and oxygen treatment were assessed by a factorial ANOVA model using type III sum of squares. Three-way interactions were ignored in the model. The data were tested for normality and variance homogeneity using Cochran's C-test, and data were log-transformed when necessary. Multiple levels of main effects were compared by multiple range tests using the Tukeys HSD procedure at the 5% significance level.


  1. Davis SM, Ogden JC: Everglades: the ecosystem and its restoration Boca Raton, FL: St. Luci Press 1994.

    Google Scholar 

  2. Loveless CM: A study of the vegetation in the Florida Everglades. Ecology. 1959, 40: 1-9. 10.2307/1929916.

    Article  Google Scholar 

  3. McCormick PV, Newman S, Vilchek LW: Landscape responses to wetland eutrophication: Loss of slough habitat in the Florida Everglades, USA. Hydrobiologia. 2009, 621: 105-114. 10.1007/s10750-008-9635-2.

    Article  CAS  Google Scholar 

  4. Vaithiyanathan P, Richardson CJ: Macrophyte species changes in the Everglades: Examination along a eutrophication gradient. J Environ Qual. 1999, 28: 1347-1358.

    Article  CAS  Google Scholar 

  5. Rutchey K, Vilcheck L: Development of an Everglades vegetation map using a spot image and the global positioning system. Photogramm Eng Remote Sens. 1994, 60: 767-775.

    Google Scholar 

  6. Rutchey K, Schall T, Sklar F: Development of vegetation maps for assessing Everglades restoration progress. Wetlands. 2008, 28: 806-816. 10.1672/07-212.1.

    Article  Google Scholar 

  7. Miao S, Sindhøj E, Edelstein C: Allometric relationships of field populations of two clonal species with contrasting life histories, Cladium jamaicense and Typha domingensis. Aquat Bot. 2008, 88: 1-9. 10.1016/j.aquabot.2007.08.001.

    Article  Google Scholar 

  8. Miao S: Rhizome growth and nutrient resorption: Mechanisms underlying the replacement of two clonal species in Florida Everglades. Aquat Bot. 2004, 78: 55-66. 10.1016/j.aquabot.2003.09.001.

    Article  CAS  Google Scholar 

  9. Miao SL, DeBusk WF: Effects of phosphorus enrichment on structure and function of sawgrass and cattail communities in the Everglades. Phosphorus Biochemistry in Subtropical Ecosystems New York, WashingtonDC.: Lewis PublishingReddy KR, O’Conner GA, Schelske CL 1999, 275-299.

    Google Scholar 

  10. Miao SL, Sklar FH: Biomass and nutrient allocation of sawgrass and cattail along a nutrient gradient in the Florida Everglades. Wetlands Ecol Manage. 1998, 5: 245-263. 10.1023/A:1008217426392.

    Article  Google Scholar 

  11. Smith SM, Leeds JA, McCormick PV, Garrett PB, Darwish M: Sawgrass (Cladium jamaicense) responses as early indicators of low-level phosphorus enrichment in the Florida Everglades. Wetlands Ecol Manage.

  12. Ponzio KJ, Miller SJ, Lee MA: Long-term effects of prescribed fire on Cladium jamaicense crantz and Typha domingensis pers. densities. Wetlands Ecol Manage. 2004, 12: 123-133. 10.1023/B:WETL.0000021671.65897.0c.

    Article  Google Scholar 

  13. Weisner SEB, Miao SL: Use of morphological variability in Cladium jamaicense and Typha domingensis to understand vegetation changes in an Everglades marsh. Aquat Bot. 2004, 78: 319-335. 10.1016/j.aquabot.2003.11.007.

    Article  Google Scholar 

  14. Lissner J, Mendelssohn IA, Lorenzen B, Brix H, McKee KL, Miao SL: Interactive effects of redox intensity and phosphate availability on growth and nutrient relations of Cladium jamaicense (Cyperaceae). Am J Bot. 2003, 90: 736-748. 10.3732/ajb.90.5.736.

    Article  PubMed  CAS  Google Scholar 

  15. Lorenzen B, Brix H, Mendelssohn IA, McKee KL, Miao SL: Growth, biomass allocation and nutrient use efficiency in Cladium jamaicense and Typha domingensis as affected by phosphorus and oxygen availability. Aquat Bot. 2001, 70: 117-133. 10.1016/S0304-3770(01)00155-3.

    Article  CAS  Google Scholar 

  16. Newman S, Grace JB, Koebel JW: Effects of nutrients and hydroperiod on Typha, Cladium, and Eleocharis: implications for Everglades restoration. Ecol Appl. 1996, 6: 774-783. 10.2307/2269482.

    Article  Google Scholar 

  17. Newman S, Schuette J, Grace JB, Rutchey K, Fontaine T, Reddy KR, Pietrucha M: Factors influencing cattail abundance in the northern Everglades. Aquat Bot. 1998, 60: 265-280. 10.1016/S0304-3770(97)00089-2.

    Article  Google Scholar 

  18. Reddy KR, DeLaune RD, DeBusk WF, Koch MS: Long-term nutrient accumulation rates in the Everglades. Soil Sci Soc Am J. 1993, 57: 1147-1155.

    Article  CAS  Google Scholar 

  19. Craft CB, Vymazal J, Richardson CJ: Response of Everglades plant communities to nitrogen and phosphorus additions. Wetlands. 1995, 15: 258-271.

    Article  Google Scholar 

  20. Craft CB, Richardson CJ: Relationships between soil nutrients and plant species composition in Everglades peatlands. J Environ Qual. 1997, 26: 224-232.

    Article  CAS  Google Scholar 

  21. Richardson CJ, King RS, Qian SS, Vaithiyanathan P, Qualls RG, Stow CA: Estimating ecological thresholds for phosphorus in the Everglades. Environ Sci Technol. 2007, 41: 8084-8091. 10.1021/es062624w.

    Article  PubMed  CAS  Google Scholar 

  22. Davis SM: Sawgrass and cattail production in relation to nutrient supply in the Everglades. Edited by: Sharitz RR, Gibbons JW. 61. U.S. Department of Energy, 1989:325-341.

    Google Scholar 

  23. Steward KK, Ornes WH: Mineral-nutrition of Sawgrass (Cladium jamaicense Crantz) in relation to nutrient supply. Aquat Bot. 1983, 16: 349-359. 10.1016/0304-3770(83)90080-3.

    Article  Google Scholar 

  24. Richardson CJ, Ferrell GM, Vaithiyanathan P: Nutrient effects on stand structure, resorption efficiency, and secondary compounds in Everglades sawgrass. Ecology. 1999, 80: 2182-2192. 10.1890/0012-9658(1999)080[2182:NEOSSR]2.0.CO;2.

    Article  Google Scholar 

  25. Li SW, Lissner J, Mendelssohn IA, Brix H, Lorenzen B, McKee KL, Miao S: Nutrient and growth responses of cattail (Typha domingensis) to redox intensity and phosphate availability. Ann Bot. 2010, 105: 175-184. 10.1093/aob/mcp213.

    Article  PubMed  CAS  PubMed Central  Google Scholar 

  26. Brix H, Sorrell BK, Orr PT: Internal pressurization and convective gas flow in some emergent freshwater macrophytes. Limnol Oceanogr. 1992, 37: 1420-1433.

    Article  Google Scholar 

  27. Sorrell BK, Mendelssohn IA, McKee KL, Woods RA: Ecophysiology of wetland plant roots: A modelling comparison of aeration in relation to species distribution. Ann Bot. 2000, 86: 675-685. 10.1006/anbo.2000.1173.

    Article  Google Scholar 

  28. Bendix M, Tornbjerg T, Brix H: Internal gas transport in Typha latifolia L and Typha angustifolia L .1. Humidity-induced pressurization and convective throughflow. Aquat Bot. 1994, 49: 75-89. 10.1016/0304-3770(94)90030-2.

    Article  Google Scholar 

  29. Tornbjerg T, Bendix M, Brix H: Internal gas transport in Typha latifolia L and Typha angustifolia L .2. Convective throughflow pathways and ecological significance. Aquat Bot. 1994, 49: 91-105. 10.1016/0304-3770(94)90031-0.

    Article  Google Scholar 

  30. Chabbi A, McKee KL, Mendelssohn IA: Fate of oxygen losses from Typha domingensis (Typhaceae) and Cladium jamaicense (Cyperaceae) and consequences for root metabolism. Am J Bot. 2000, 87: 1081-1090. 10.2307/2656644.

    Article  PubMed  CAS  Google Scholar 

  31. Koch MS, Reddy KR: Distribution of soil and plant nutrients along a trophic gradient in the Florida Everglades. Soil Sci Soc Am J. 1992, 56: 1492-1499.

    Article  Google Scholar 

  32. Davis SM: Phosphorus inputs and vegetation sensitivity in the Everglades. Everglades. The ecosystem and its restoration. Edited by: Davis SM, Ogden JC. 1994, Boca Raton, Florida: St. Lucie Press, 357-378.

    Google Scholar 

  33. Palmer ML, Mazzotti FJ: Structure of everglades alligator holes. Wetlands. 2004, 24: 115-122. 10.1672/0277-5212(2004)024[0115:SOEAH]2.0.CO;2.

    Article  Google Scholar 

  34. Raghothama KG: Phosphate acquisition. Annu Rev Plant Phys. 1999, 50: 665-693. 10.1146/annurev.arplant.50.1.665.

    Article  CAS  Google Scholar 

  35. Clarkson DT: Factors affecting mineral nutrient acquisition by plants. Ann Rev Plant Physiol. 1985, 36: 77-115.

    Article  CAS  Google Scholar 

  36. Loneraga JF, Asher CJ: Response of plants to phosphate concentration in solution culture .2. Rate of phosphate absorption and Its relation to growth. Soil Sci. 1967, 103: 311.

    Article  Google Scholar 

  37. Keerthisinghe G, Hocking PJ, Ryan PR, Delhaize E: Effect of phosphorus supply on the formation and function of proteoid roots of white lupin (Lupinus albus L.). Plant Cell Environ. 1998, 21: 467-478. 10.1046/j.1365-3040.1998.00300.x.

    Article  CAS  Google Scholar 

  38. Barber SA: Growth requirements for nutrients in relation to demand at the root surface. The Soil-Root InterfaceLondon, New York, San Francisco: Academic PressHarley JL, Russell RS. 1979, 5-20.

    Chapter  Google Scholar 

  39. Brix H, Dyhr-Jensen K, Lorenzen B: Root-zone acidity and nitrogen source affects Typha latifolia L. growth and uptake kinetics of ammonium and nitrate. J Exp Bot. 2002, 53: 2441-2450. 10.1093/jxb/erf106.

    Article  PubMed  CAS  Google Scholar 

  40. Brix H, Lorenzen B, Morris JT, Schierup H-H, Sorrell BK: Effects of oxygen and nitrate on ammonium uptake kinetics and adenylate pools in Phalaris arundinacea L and Glyceria maxima (Hartm) Holmb. P Roy Soc Edinb B. 1994, 102: 333-342.

    Google Scholar 

  41. Jampeetong A, Brix H: Effects of NH4 + concentration on growth, morphology and NH4+ uptake kinetics of Salvinia natans. Ecol Eng. 2009, 35: 695-702. 10.1016/j.ecoleng.2008.11.006.

    Article  Google Scholar 

  42. Lissner J, Mendelssohn IA, Anastasiou CJ: A method for cultivating plants under controlled redox intensities in hydroponics. Aquat Bot. 2003, 76: 93-108. 10.1016/S0304-3770(03)00017-2.

    Article  Google Scholar 

  43. Sorrell BK: Effect of external oxygen demand on radial oxygen loss by Juncus roots titanium citrate solutions. Plant Cell Environ. 1999, 22: 1587-1593. 10.1046/j.1365-3040.1999.00517.x.

    Article  CAS  Google Scholar 

  44. Brix H, Sorrell BK: Oxygen stress in wetland plants: comparison of de-oxygenated and reducing root environments. Funct Ecol. 1996, 10: 521-526. 10.2307/2389945.

    Article  Google Scholar 

  45. Rubio G, Oesterheld M, Alvarez CR, Lavado RS: Mechanisms for the increase in phosphorus uptake of waterlogged plants: soil phosphorus availability, root morphology and uptake kinetics. Oecologia. 1997, 112: 150-155. 10.1007/s004420050294.

    Article  Google Scholar 

  46. Atwell BJ, Veerkamp MT, Stuiver BCEE, Kuiper PJC: The uptake of phosphate by Carex species from oligotrophic to eutrophic swamp habitats. Physiol Plant. 1980, 49: 487-494. 10.1111/j.1399-3054.1980.tb03339.x.

    Article  CAS  Google Scholar 

  47. Veerkamp MT, Corre WJ, Atwell BJ, Kuiper PJC: Growth-rate and phosphate utilization of some Carex species from a range of oligotrophic to eutrophic swamp habitats. Physiol Plant. 1980, 50: 237-240. 10.1111/j.1399-3054.1980.tb04456.x.

    Article  CAS  Google Scholar 

  48. Raghothama KG, Karthikeyan AS: Phosphate acquisition. Plant Soil. 2005, 274: 37-49. 10.1007/s11104-004-2005-6.

    Article  CAS  Google Scholar 

  49. Raghothama KG: Phosphate transport and signaling. Curr Opin Plant Biol. 2000, 3: 182-187.

    Article  PubMed  CAS  Google Scholar 

  50. Lee RB: Selectivity and kinetics of ion uptake by barley plants following nutrient deficiency. Ann Bot. 1982, 50: 429-449.

    CAS  Google Scholar 

  51. Jungk A, Asher CJ, Edwards DG, Meyer D: Influence of phosphate status on phosphate-uptake kinetics of Maize (Zea mays) and Soybean (Glycine max). Plant Soil. 1990, 124: 175-182. 10.1007/BF00009256.

    Article  CAS  Google Scholar 

  52. Drew MC, Saker LR, Barber SA, Jenkins W: Changes in the kinetics of phosphate and potassium absorption in nutrient-deficient barley roots measured by a solution-depletion technique. Planta. 1984, 160: 490-499. 10.1007/BF00411136.

    Article  PubMed  CAS  Google Scholar 

  53. Fohse D, Claassen N, Jungk A: Phosphorus efficiency of plants .2. Significance of root radius, root hairs and cation-anion balance for phosphorus influx in 7 plant-species. Plant Soil. 1991, 132: 261-272.

    Google Scholar 

  54. Jungk A, Claassen N: Ion diffusion in the soil-root system. Adv Agron. 1997, 61: 53-110. full_text.

    Article  CAS  Google Scholar 

  55. Jungk A, Seeling B, Gerke J: Mobilization of different phosphate fractions in the rhizosphere. Plant Soil. 1993, 156: 91-94. 10.1007/BF00024991.

    Article  Google Scholar 

  56. Kuhn NL, Mendelssohn IA, McKee KL, Lorenzen B, Brix H, Miao SL: Root phosphatase activity in Cladium jamaicense and Typha domingensis grown in everglades soil at ambient and elevated phosphorus levels. Wetlands. 2002, 22: 794-800. 10.1672/0277-5212(2002)022[0794:RPAICJ]2.0.CO;2.

    Article  Google Scholar 

  57. Rengel Z: Mechanistic simulation models of nutrient uptake - a review. Plant Soil. 1993, 152: 161-173. 10.1007/BF00029086.

    Article  CAS  Google Scholar 

  58. Jayachandran K, Shetty KG: Growth response and phosphorus uptake by arbuscular mycorrhizae of wet prairie sawgrass. Aquat Bot. 2003, 76: 281-290. 10.1016/S0304-3770(03)00075-5.

    Article  CAS  Google Scholar 

  59. Reddy KR, Wang Y, DeBusk WF, Fisher MM, Newman S: Forms of soil phosphorus in selected hydrologic units of the Florida Everglades. Soil Sci Soc Am J. 1998, 62: 1134-1147.

    Article  CAS  Google Scholar 

  60. Qualls RG, Richardson CJ: Forms of soil-phosphorus along a nutrient enrichment gradient in the Northern Everglades. Soil Sci. 1995, 160: 183-198. 10.1097/00010694-199509000-00004.

    Article  CAS  Google Scholar 

  61. Lorenzen B, Brix H, Schierup H-H, Madsen TV: Design and performance of the Phyto-Nutri-Tron: a system for controlling the root and shoot environment for whole-plant ecophysiological studies. Environ Exp Bot. 1998, 39: 141-157. 10.1016/S0098-8472(97)00041-5.

    Article  PubMed  CAS  Google Scholar 

  62. Lorenzen B, Brix H, McKee KL, Mendelssohn IA, Miao S: Seed germination of two Everglades species, Cladium jamaiscense and Typha domingensis. Aquat Bot. 2000, 66: 169-180. 10.1016/S0304-3770(99)00076-5.

    Article  Google Scholar 

  63. Brix H, Lyngby JE, Schierup H-H: Eelgrass (Zostera marina L.) as an indicator organism of trace metals in the Limfjord, Denmark. Mar Environ Res. 1983, 8: 165-181. 10.1016/0141-1136(83)90049-1.

    Article  CAS  Google Scholar 

  64. Jampeetong A, Brix H: Nitrogen nutrition of Salvinia natans: Effects of inorganic nitrogen form on growth, morphology, nitrate reductase activity and uptake kinetics of ammonium and nitrate. Aquat Bot. 2009, 90: 67-73. 10.1016/j.aquabot.2008.06.005.

    Article  CAS  Google Scholar 

  65. Dyhr-Jensen K, Brix H: Effects of pH on ammonium uptake by Typha latifolia L. Plant Cell Environ. 1996, 19: 1431-1436. 10.1111/j.1365-3040.1996.tb00022.x.

    Article  CAS  Google Scholar 

  66. Tylova-Munzarova E, Lorenzen B, Brix H, Votrubova O: The effects of NH4+ and NO3- on growth, resource allocation and nitrogen uptake kinetics of Phragmites australis and Glyceria maxima. Aquat Bot. 2005, 81: 326-342. 10.1016/j.aquabot.2005.01.006.

    Article  CAS  Google Scholar 

  67. Romero JA, Brix H, Comín FA: Interactive effects of N and P on growth, nutrient allocation and NH4 uptake kinetics by Phragmites australis. Aquat Bot. 1999, 64: 369-380. 10.1016/S0304-3770(99)00064-9.

    Article  CAS  Google Scholar 

Download references


The project was supported by a grant from the South Florida Water Management District, West Palm Beach, Florida (Macrophyte Nutrient Kinetics, Contract C-6642). Additional travel and salary support was provided by the John P. Laborde Endowed Chair for Sea Grant Research and Technology Transfer Program. We thank Ken Krauss, Rebecca Howard, Sue Newman and Fred Sklar for comments on the manuscript. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the US Government.

Author information

Authors and Affiliations


Corresponding author

Correspondence to Hans Brix.

Additional information

Authors' contributions

BL carried out the controlled growth experiments and uptake studies and performed most of the statistical analyses. HB and BL drafted the manuscript. IAM, KLM and SLM participated in the design of the study and helped to draft the manuscript. All authors read and approved the final manuscript.

Authors’ original submitted files for images

Rights and permissions

This article is published under license to BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Reprints and permissions

About this article

Cite this article

Brix, H., Lorenzen, B., Mendelssohn, I.A. et al. Can differences in phosphorus uptake kinetics explain the distribution of cattail and sawgrass in the Florida Everglades?. BMC Plant Biol 10, 23 (2010).

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: