- Research article
- Open Access
Can differences in phosphorus uptake kinetics explain the distribution of cattail and sawgrass in the Florida Everglades?
© Brix et al; licensee BioMed Central Ltd. 2010
- Received: 24 June 2009
- Accepted: 8 February 2010
- Published: 8 February 2010
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.
- Arbuscular Mycorrhizal Fungus
- Uptake Kinetic
- Growth Unit
- Root Chamber
- Nutrient Uptake Kinetic
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 . 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 . 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 [3–6]. Numerous studies have been conducted to assess the causes and the consequences of this change in vegetation and community structure [7–20], and the driving force for the change appears to be nutrient enrichment, particularly phosphorus (P), from agricultural runoff and Lake Okeechobee outflow .
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 [26–29]. Furthermore, Cladium has lower root porosity and generally higher alcoholic fermentation rates, indicating lower capacity for root aeration than Typha . 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 . Typha is much less abundant than Cladium and has slow growth rates in these areas , and although nutrient enrichment and disturbance around alligator holes have been suggested to favour the proliferation of Typha locally , 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 . 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 [35–37].
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 [38–41].
1.01 ± 0.05
0.30 ± 0.03
5.6 ± 0.7
17.4 ± 1.9
0.98 ± 0.09
0.50 ± 0.10
7.0 ± 1.9
16.1 ± 1.6
1.00 ± 0.12
0.32 ± 0.04
7.0 ± 1.9
18.3 ± 2.2
0.95 ± 0.08
0.30 ± 0.06
12.8 ± 2.9
14.1 ± 2.2
0.69 ± 0.12
0.48 ± 0.05
5.8 ± 0.5
22.3 ± 1.9
0.96 ± 0.05
0.42 ± 0.06
11.6 ± 1.4
8.7 ± 1.6
0.96 ± 0.06
0.39 ± 0.03
9.1 ± 1.3
15.1 ± 2.0
1.08 ± 0.09
0.29 ± 0.04
23.6 ± 4.3
7.7 ± 0.6
Phosphorus uptake kinetics
P uptake capacity
Results of ANOVA for uptake kinetics
Source of variation
B (P level)
C (O2 level)
A × B
A × C
B × C
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
Affinity for P uptake
(l g-1DW h-1)
(l g-1DW h-1)
2.43 ± 0.40
0.75 ± 0.17
0.40 ± 0.22
0.28 ± 0.20
3.40 ± 0.27
1.44 ± 0.15
0.86 ± 0.20
0.32 ± 0.07
2.51 ± 0.35
0.84 ± 0.14
1.63 ± 0.29
0.90 ± 0.25
7.25 ± 1.77
4.08 ± 0.50
1.17 ± 0.13
1.05 ± 0.34
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 [42–44]. 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 . 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.
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 [, 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 . 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 . 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 , 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 . 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 . Another means of P acquisition from P-deficient soils is symbiosis with arbuscular mycorrhizal fungi . Inoculation of Cladium with arbuscular mycorrhizal fungi in a greenhouse pot experiment increased growth and P uptake of Cladium significantly . 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.
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 .
Seeds and germination
Hydroponic nutrient solutions
Basic nutrient solution
P addition solution
1 mS cm-1
<0.5 or 8 mg l-1
5 or 500 μg l-1
50 mg l-1
2.4 mg l-1
3.4 mg l-1
802 mg l-1
130 mg l-1
291 mg l-1
98 mg l-1
690 mg l-1
(NH4)2SO4, CaSO4, MgSO4
41 mg l-1
114 mg l-1
50 mg l-1
12 mg l-1
216 mg l-1
18 mg l-1
351 mg l-1
27 μg l-1
5.4 mg l-1
11 μg l-1
2.2 mg l-1
13 μg l-1
2.6 mg l-1
13 μg l-1
2.6 mg l-1
4.8 μg l-1
1.0 mg l-1
112 μg l-1
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.
The uptake experiments were carried out in the PNT, which is a computer controlled hydroponic growth facility for experiments with whole plants . 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
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 . 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 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, 64–67]. 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.
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.
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