Research Article

Water channels are important for osmotic adjustments of yeast cells at low temperature

Microbiology 2006; 152(5):1515 · https://doi.org/10.1099/mic.0.28679-0

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Abstract

The importance of aquaporin expression in water permeability in Saccharomyces cerevisiae was assessed by measuring the osmotic water permeability coefficient (Pf) and the activation energies (Ea) from both hypo- and hypertonic experiments performed with whole protoplasts from four strains differing in aquaporin level of expression: parental, double-deleted and overexpressing AQY1 or AQY2. Double-deleted (lower Pf) and AQY1-overexpressing strains (higher Pf) presented linear Arrhenius plots with Ea consistent with fluxes mainly through the lipids [16·3 kcal mol1 (68·2 kJ mol1)] and with a strong contribution of channels [9·6 kcal mol1 (40·2 kJ mol1)], respectively. The Arrhenius plots for the parental (swelling experiments) and overexpressing AQY2 strains (swelling and shrinking experiments) were not linear, presenting a break point with a change in slope around 23 °C. The Ea values for these strains, calculated for temperatures ranging from 7 to 23 °C, were lower [9·5 kcal mol1 (39·7 kJ mol1)] than the values obtained from 23 to 38 °C [17 kcal mol1 (71·1 kJ mol1)]. This behaviour indicates that only in the lower temperature range did the water fluxes occur predominantly via the water channels. The permeabilities for each strain relative to the deletion strain show that an increase in permeability due to the presence of aquaporins was more relevant at low temperatures. Following our results, we propose that water channels play an important role for osmotic adjustment of yeast cells at low temperature.
Abbreviations: CFDA, carboxyfluorescein diacetate
The first experimental evidence for the existence of water channels in cell membranes was obtained for red blood cells (Farmer & Macey, 1970; Macey et al., 1972; Paganelli & Solomon, 1957; Vieira et al., 1970) and renal epithelia (Verkman, 1992), and was based mainly on measures of high osmotic water permeability (inhibited by mercurial reagents) and of low activation energy for water transport. In 1992 Agre and co-workers revealed that a 28 kDa integral membrane protein was the erythrocyte water channel and that the same protein was also present in renal epithelia (Preston et al., 1992). This protein is now known as aquaporin 1 (Aqp1) and it belongs to a large family of proteins that are widely distributed in nature. In mammals and plants they have important functions in water homeostasis and osmoregulation of individual cells and whole organisms. In micro-organisms, aquaporins were also recognized but their physiological role is yet being explored.

Analysis of the Saccharomyces cerevisiae genome revealed four ORFs encoding members of the major intrinsic protein (MIP) family (Bonhivers et al., 1998): FPS1 and YFL054c related to glycerol facilitator homologues (genetically close to the aquaglyceroporins), and AQY1 and AQY2, more closely related to aquaporin water channels. The functionality of aquaporins in S. cerevisiae has been debated in the literature. To study the polymorphism of aquaporins in yeast, a survey on 52 strains was performed, revealing that all strains carry an allele encoding a functional Aqy1p, but in none of these strains did the Aqy2p seem to be functional, with the exception of strain Σ1278 (Laizé et al., 2000). The authors considered the hypothesis that selective pressure kept an active Aqy1p, but not Aqy2p, in yeast.

Expression of AQY1 in Xenopus oocytes showed an active Aqy1p, mediating water transport (Bonhivers et al., 1998), while the expression of AQY2 from strain Σ1278 was not detectable. Nevertheless, evidence that Aqy2p was expressed and functional in vesicles derived from strain Σ1278 cells has been presented, while the expression of Aqy1p was not detectable (Meyrial et al., 2001). By immunocytochemistry and biochemical subcellular fractionation it was found that Aqy2p was located in the endoplasmic reticulum and in the plasma membrane. Under the experimental conditions tested, AQY2 was expressed only in rich medium, during exponential growth, when glucose was the energy source. The expression of AQY2 was repressed by ethanol or galactose in rich medium, by minimal medium, hyperosmolar medium and by sporulating conditions.

Recently, it was shown that Aqy1p was involved in sporulation (Sidoux-Walter et al., 2004) and that this could be its only function. The authors claimed that Aqy1p was detectable exclusively in spore membranes under ambient conditions and that the lack of Aqy1p reduced spore fitness.

An important role for aquaporins was found in the increase of freeze tolerance in baker's yeast (Tanghe et al., 2002, 2004). Deletion of the genes AQY1 and AQY2 rendered a laboratory strain more sensitive to freezing, while overexpression of these genes improved freeze tolerance. In these transformants growth and fermentation characteristics were not affected as compared with the parental strains, but the improvement of freezethaw resistance was so notorious that a transformant was selected based on this characteristic (Tanghe et al., 2002). This phenotype was observed only when freezing occurred rapidly (Tanghe et al., 2004).

Surprisingly, it was found that when spores are rapidly frozen, those that lack Aqy1p survive better, providing for a functional test of active spore water channels (Sidoux-Walter et al., 2004). Comparing all these recent works (Sidoux-Walter et al., 2004; Tanghe et al., 2002, 2004), the amazing conclusion is that water channels improve freeze tolerance in vegetative cells and reduce freeze tolerance in spores.

The purpose of our work was to evaluate the role of aquaporins in plasma membrane water permeability of yeast strains for which the effect of aquaporins on freeze tolerance has been documented. We approached this problem by measuring activation energies of osmotic water transport in protoplasts prepared from S. cerevisiae Σ1278b-derived parental strain 10560-6B, and from three derivatives of this strain, one where AQY1 and AQY2 were deleted and two others where either AQY1 or AQY2 was overexpressed. These protoplast populations were submitted to hypo- and hyperosmotic shocks with an impermeant solute at different temperatures; the time dependence for volume equilibration was followed and water permeability coefficients evaluated.

Yeast strains and plasmids used in this study.
Strains used in this work were 10560-6B MATα leu2 : : hisG trp1 : : hisG his3 : : hisG ura3-52; 10560-6B/pYX012 KanMX (=strain ANT29, indicated as parental); 10560-6B/pYX012 KanMX AQY1-1 (=strain ANT27, indicated as overexpressing AQY1); 10560-6B/pYX012 KanMX AQY2-1 (=strain ANT26, indicated as overexpressing AQY2); 10560-6B aqy1 : : KanMX4 aqy2 : : HIS3 (=strain YSH 1172, indicated as double deleted).

Integrative plasmid pYX012 (Novagen) was modified with a dominant marker gene by cloning the EcoRVPvuII fragment containing the loxP-KanMX4-loxP cassette from pUG6 (Güldener et al., 1996) in the URA3 marker (StuI restriction site), resulting in plasmid pYX012 KanMX. The aquaporin ORF AQY1-1 was PCR-amplified using primers AQY1-FP (5'-GCGAATTCTTAACTATAACATGTCTTCGAACG-3'; EcoRI site underlined) and AQY1-RP (5'-CACCCGGGAAAAACACTAATTACCTCAGTAG-3'; XmaI site underlined) on genomic DNA of strain 10560-6B. The resulting fragments were cloned into pYX012 KanMX downstream of the constitutive TPI1 promoter using EcoRI and XmaI restriction sites. The aquaporin ORF AQY2-1 was subcloned from pYX242/AQY2-1 (Meyrial et al., 2001) in pYX012 KanMX using EcoRI and BamHI restriction sites. Integration of SphI-linearized pYX012 KanMX/AQY1-1 or AQY2-1 at the TPI1 locus resulted in geneticin-resistant strains of 10560-6B, overexpressing AQY1-1 and AQY2-1 respectively.

Preparation of yeast protoplasts.
Cells were grown in YPD medium [1 % (w/v) peptone, 0·5 % (w/v) yeast extract, 2 % (w/v) glucose], with orbital shaking, at 28 °C. Protoplasts were prepared essentially as described by Faye et al. (1974). Cells were harvested in the exponential phase (OD6401) by centrifugation (18 000 g) for 5 min at 4 °C, and washed once with 1·2 M sorbitol, after which 10 g (wet wt) was resuspended in 30 ml digestion buffer and incubated in an orbital shaking water bath at 30 °C. To prepare the digestion buffer, 30 ml 2 M sorbitol was mixed with 3 ml 1 M potassium phosphate buffer, pH 7·5; 0·1 ml 0·5 M EDTA; 1·25 ml 0·25 mM dithiothreitol; 15·25 ml water; and 2 units zymolase 100T ml1. When the digestion was complete, 150 ml of a 1·2 M sorbitol solution was added to the suspension, which was centrifuged at 3000 g for 10 min (4 °C). The pellet was then washed twice with 150 ml 1·2 M sorbitol. The protoplasts were resuspended in 1·2 M sorbitol. The concentration of 1·2 M sorbitol was chosen throughout the preparation of protoplasts, because disruption of the protoplasts was observed when they were suspended in lower concentrations of sorbitol. In 0·8 M sorbitol many disrupted membranes were observed under the microscope and only at 1 M did most protoplasts remain intact. The concentration of 1·2 M guarantees that protoplasts will not burst during swelling experiments.

For fluorescence experiments, protoplasts were pre-loaded for 10 min at 30 °C with the non-fluorescent precursor 5-(and 6)-carboxyfluorescein diacetate (CFDA, 1 mM in iso-osmotic solution) prior to the osmotic challenges in the stopped-flow apparatus. To avoid pH interference in fluorescence, cell suspensions and osmotic solutions were prepared in 50 mM K+-citrate buffer, pH 5.

Protoplast size determination.
Protoplast size (initial equilibrium volume) of all the preparations tested was determined by quasi-elastic light scatter (QELS) using a particle sizer (BI-90 Brookhaven Instruments). An application of this technique in the determination of vesicular sizes has been published (Perevucnik et al., 1985).

The protoplast preparations were homogeneous and protoplasts were spherical in shape, as observed under light microscopy. The QELS technique for measuring the initial diameter has shown unimodal populations for all the preparations with a mean value of 1·9±0·2 µm.

Stopped-flow experiments
Experiments were performed on a HI-TECH Scientific PQ/SF-53 stopped-flow apparatus, which has a 2 ms dead time and is temperature controlled, interfaced with an IBM PC/AT compatible 80386 microcomputer. Experiments were performed at temperatures ranging from 7 to 38 °C. Three runs were usually stored and analysed in each experimental condition. In each run 0·1 ml protoplast suspension [1 : 20 dilution in preparation buffer, initial osmolarity (osmout)0=1·2 M] was mixed with an equal amount of iso-, hypo- or hyperosmotic sorbitol solutions to reach different out or inwardly directed gradients of solute. The time-course of volume change was followed by light scatter and/or fluorescence of a trapped fluorophore.

Light-scatter experiments.
The time-course of 90° scattered light intensity at 400 nm was followed until a stable light-scattered signal was obtained (1024 data points were acquired for periods ranging from 15 to 90 s).

Fluorescence experiments.
A concentration-dependent self-quenching fluorophore was used to monitor cell volume changes. Carboxyfluorescein (CF) was excited using a 470 nm interference filter and detected using a >530 nm cut-on filter. Cells were subjected to hyper- and hypo-osmotic shocks following the same protocol applied for the light-scatter experiments, and changes in CF fluorescence due to fluorescence quenching were followed until a stable signal was obtained.

Signals were recorded on a computer interfaced directly with the Hi-Tech SF-53 using dedicated software (Hi-Tech Scientific) and were fitted to a single exponential from where the total signal amplitude and the rate constant K were evaluated.

Pf evaluation from the rate constant of volume equilibration.
The osmotic water permeability coefficient Pf can be estimated from the linear relationship between Pf and K (van Heeswijk & van Os, 1986), Pf=K(V0/A)(1/Vw(osmout)), where Vw is the molar volume of water, V0/A is the initial volume to area ratio of the protoplast population, and (osmout) is the final medium osmolarity after the osmotic shock.

The activation energy (Ea) of water transport was evaluated from the slope of the Arrhenius plot (lnPf as a function of 1/T).

To determine the importance of aquaporins in water permeability, we measured the osmotic water coefficient (Pf) in four S. cerevisiae strains: parental, double-deleted and overexpressing AQY1 or AQY2. The experiments were performed under hypo- or hypertonic conditions at different temperatures using the stopped-flow technique.

Water permeability measurements
Fig. 1 shows records of a typical stopped-flow experiment (obtained with AQY2 overexpressing strain) where the light-scatter intensity from a protoplast suspension suddenly exposed to three different solutions (iso-, hyper- and hypo-osmotic) was followed for 20 s. The three curves are identified by the tonicity of the shock (Λ), defined as the ratio of the final to initial osmolarity of the outside medium, i.e. Λ=(osmout)/(osmout)0. Fig. 1 insert shows the linear dependence of the signal amplitude on 1/Λ, obtained from these stopped-flow traces. For all protoplast preparations, similar traces were obtained and linear relations between the total amplitude and 1/Λ were also obtained for all the temperatures tested. The time-dependent volume changes at 23 °C for the different strains subjected to the same osmotic shocks (Λ=0·75, or Λ=1 for the baseline) are shown in Fig. 2. These traces show similar time constants for the deletion and parental strains, while strains harbouring overexpression constructs for AQY1 or AQY2 show higher rate constants. Equivalent symmetrical traces were obtained for hypertonic shocks of Λ=1·25 (data not shown). Each strain presented equivalent Pf values for both hypo- and hypertonic shocks at all temperatures tested. The mean Pf (x104 cm s1) values (±SD) at 23 °C were 7·28±1·07 and 5·13±0·59 for the strains overexpressing AQY1 and AQY2, respectively, and 1·88±0·25 and 2·02±0·20 for the parental and deletion strain, respectively.



(12K):

Fig. 1. Record of a typical stopped-flow experiment where the light scatter intensity from a protoplast suspension (AQY2-overexpressing strain) equilibrated in 1·2 M sorbitol solution was suddenly exposed to different osmotic shocks (Λ=0·75, 1 and 1·25). Data acquisition was followed for 20 s at 23 °C. Insert: signal amplitudes as a function of the 1/Λ, obtained from the previous traces.


(33K):

Fig. 2. Light-scatter signals obtained for the four yeast strains subjected to the same osmotic shock at 23 °C. Λ=1 (baseline) and Λ=0·75.

To assure that other light-scattering artefacts not related to volume changes did not contribute to the light-scattering signal, we validated this methodology on yeast protoplasts with fluorescence measurements applied to the AQY1 strain. The fluorophore used is an ester form of CFDA, which is membrane permeable but of low fluorescence until cleaved intracellularly by non-specific esterases to give the impermeable fluorescent form. As the cells shrink or swell in response to osmotic changes, the concentration of the entrapped fluorophore will rise or fall with a consequent change in fluorescence output (Chen & Knutson, 1988); the concentration-dependent self-quenching properties of the fluorophore enable cell volume changes to be recorded as changes in fluorescence.

Applying in these fluorescence experiments the same osmotic shocks used in the light-scatter experiments (Λ=0·75, 1 and 1·25), it was observed that, at all the temperatures tested, the rate constants for volume equilibration obtained by this approach were similar to the rate constants obtained by light scatter, giving similar Pf values. Table 1 compares the Pf values obtained at 23 °C by the two different methods and for the lower and higher temperature tested. These results demonstrate that for small perturbations, the light scatter is an adequate methodology to follow protoplast volume changes and perform measurements of osmotic water permeability in yeasts.


Table 1. Pf values (cm s1) obtained by light scattering and fluorescence for the AQY1-overexpressing strain


Activation energies
The activation energy (Ea) for water transport was estimated from Arrhenius plots for the four populations tested. Fig. 3 shows the plots obtained for the four strains for swelling and shrinking respectively when Pf was evaluated using the light-scatter technique. The deletion strain and the strain with overexpression of AQY1 show a linear plot with a lower Ea value for the overexpressing AQY1 strain (confirmed in fluorescence experiments, data not shown). The shrinking and swelling experiments for the parental strain showed different behaviours. A single straight line could only be fitted to the shrinking data points with Ea value equivalent to the deletion strain (Fig. 3).



(9K):

Fig. 3. Arrhenius plots for the four strains tested: , AQY1; •, AQY2; , parental; , deletion. (a) Hypotonic conditions, swelling experiments; (b) hypertonic conditions, shrinking experiments. All the experimental points are presented as mean values±SD of triplicates.

The protoplasts derived from the parental (swelling experiments) and AQY2 overexpression strain (swelling and shrinking experiments) showed a different behaviour for different temperature spans. The Ea values calculated for temperatures ranging from 7 to 23 °C were lower than the values obtained from 23 to 38 °C. The Ea values obtained for the lower temperature range were similar to the values obtained for the AQY1 strain, while the values obtained for the higher temperature range were equivalent to those for the deletion strain (Table 2).


Table 2. Activation energies for swelling experiments The strains used were 10560-6B/pYX012 KanMX (parental); 10560-6B/pYX012 KanMX AQY1-1 (AQY1); 10560-6B/pYX012 KanMX AQY2-1 (AQY2); 10560-6B aqy1 : : KanMX4 aqy2 : : HIS3 (deletion).


Table 3 presents the Pf values for all the strains obtained for the lowest and highest temperatures tested (7 and 38 °C). For both temperatures the lowest value was obtained for the deletion strain. The table also shows the permeabilities for each strain relative to the deletion strain, calculated as the ratio . This ratio shows that the increase in permeability due to the presence of aquaporins becomes more relevant at low temperatures.


Table 3. Osmotic permeability coefficients for the lower (7 °C) and higher (38 °C) temperature limits For each strain the Pf value is compared with the value obtained for the deletion strain at the same temperature ().

Water may cross cell membranes by two different parallel pathways with distinct mechanisms for permeation: partition/diffusion of water molecules across the hydrophobic bilayer (high activation energy for transport) and single file diffusion of water molecules through the channels (low activation energy). The flux of water across the membrane is the sum of the fluxes through these two pathways and the resulting activation energy depends on the relative contribution of each pathway to the total flux. In order to establish which pathway is dominant in a particular cellular system, measures of the activation energy for osmotic water transport are usually performed. High values suggest that the lipid pathway predominates while lower values indicate the presence of functional aquaporins in these cells.

All our experiments were performed in protoplasts derived from strains with different levels of expression of aquaporins and they responded osmotically to the different tonicity shocks (hypo- and hypertonic, Fig. 1 and Fig. 2), rendering these protoplasts a useful model to study water transport in yeast. For small volume perturbations, the light-scatter technique has proved to be an adequate method to evaluate the osmotic permeability coefficient as the use of an independent technique (concentration-dependent quenching fluorescence) applied to the same AQY1 strain gave equivalent values of Pf for all the temperatures tested and, consequently, an equivalent Ea value.

A similar methodology was previously used (Laizé et al., 1999) when working with strain Σ1278b presenting Pf values much higher that those we measured. We speculate that the differences observed may be explained by different initial concentrations of sorbitol used. In the work by Laizé et al. (1999), the initial concentration was 0·5 M, but in our experiments we observed that an important fraction of the protoplasts was disrupted when suspended in 0·8 M sorbitol and only at 1 M did most protoplasts remain intact. We chose 1·2 M to guarantee that disruption would not occur during swelling experiments.

Our results from both hypo- and hypertonic experiments (protoplast swelling and shrinking) show that, in general, the Pf values for all the temperatures tested were higher for the AQY1 followed by the AQY2 overexpressing strains. Since both genes are expressed behind the same promoter, this result suggests that Aqy1p may be slightly more active than Aqy2p, although the hypothesis that this difference is due to different levels of expression cannot be discarded.

For the lower temperature range (723 °C) the parental strain showed higher Pf values than the deletion strain, representing clear evidence that at least one of the aquaporins was expressed in the parental strain under the growth conditions used for the experiments (Table 3). Nevertheless, the values for both these strains were similar for the higher temperature range tested (2338 °C). This may indicate that the presence of aquaporins is of major importance at lower temperatures and is in agreement with the aquaporin-mediated improvement of freeze tolerance as suggested (Tanghe et al., 2002). Although the concept of cold-induced improvement of freeze tolerance is highly controversial, the most recent studies on this topic are all indicative of an adaptation of yeast cells to cold stress (Alves-Araujo et al., 2004; Rodriguez-Vargas et al., 2002; Sahara et al., 2002).

The activation energy values obtained for the deletion strain were high and compatible with water flowing mainly through the lipid bilayers as expected from the genotype of this strain. For the strain overexpressing AQY1, much lower values were found for the Ea, indicating the presence of active water channels, under all the temperatures tested (Table 2).

Interestingly, however, the Arrhenius plots for the parental (swelling experiments) and overexpressing AQY2 strains (swelling and shrinking experiments) were not linear, presenting a break point with a change in slope around 23 °C. The calculated Ea for the higher temperature range (2338 °C) was high and only for temperatures below 23 °C was the value low (Table 2, Fig. 3). This behaviour indicates that below this temperature the water fluxes through the water channels become important.

The question is, why were the water fluxes across the channels not visible at higher temperatures? Were the water channels less active at higher temperatures or was their activity masked by the flux across the bilayer at higher temperatures? If this latter explanation is true then at the very low temperatures the contribution of the lipid pathway may even become insignificant and the activation energy could become much lower. On the other hand, and according to this hypothesis, if we could increase the temperature range to much higher values (above 40 °C), we should probably also detect a break in the AQY1 plot.

A numerical simulation of this hypothesis is shown in the Arrhenius plot of Fig. 4. The two dashed straight lines represent the typical behaviour for the lipid pathway with an activation energy of 18 kcal mol1 (75·3 kJ mol1; line with greater slope) and the channel pathway with an Ea of 4 kcal mol1 (16·7 kJ mol1; line with lesser slope). These lines will cross at a certain point corresponding to the temperature below which the channel pathway overcomes the lipid pathway (right side of the graph). This temperature can vary depending on the number of active channels present. The sum of these two contributions for the total permeability will give rise to a non-linear Arrhenius plot (solid curve). In this example, if the temperature is sufficiently high (left side of the graph) the total permeability will equal the lipid permeability with an Ea of 18 kcal mol1 (75·3 kJ mol1) while, if the temperature is sufficiently low (right side of the graph), the total permeability will be equivalent to the channel permeability with an Ea of 4 kcal mol1 (16·7 kJ mol1). In the middle temperature range, the slope varies from 18 to 4 kcal mol1 (75·3 to 16·7 kJ mol1). Within our experimental temperatures the four strains behaved differently, showing a diverse contribution of both pathways. The deletion strain had no contribution of the channel pathway, as expected. The overexpressing AQY1 was the strain with the highest contribution of the channel pathway at all temperatures tested. The overexpressing AQY2 and parental strains showed a mixed behaviour, since at high temperatures they behaved like lipid membranes but as the temperature decreased the channel pathway became visible and the activation energy decreased accordingly.



(8K):

Fig. 4. Numerical simulation of an Arrhenius plot. The two dashed straight lines represent the typical behaviour for the lipid pathway with an Ea of 18 kcal mol1 (75·3 kJ mol1; line with greater slope) and for the channel pathway with an Ea of 4 kcal mol1 (16·7 kJ mol1; line with lesser slope) respectively. The solid line represents the sum of both pathways for the total permeability and simulates the behaviour of all the four strains shown in Fig. 3. The experimental temperature range for each particular strain is differently positioned in the x-axis.

We would point out that the results were obtained with protoplasts and this delicate balance in water transport through the lipid bilayer and channels may be disturbed as compared with intact cells. Nevertheless, it is very probable that, in any case, aquaporins become more relevant for yeast behaviour at low temperatures. We should not forget that the only visible phenotypes for genotypes associated with aquaporins were found in freeze tolerance (Sidoux-Walter et al., 2004; Tanghe et al., 2002, 2004). If the lipid membrane is more rigid and less permeable it makes sense that water channels become important during water volume increase and crystal formation at low temperature, preventing cell bursting (Tanghe et al., 2003).

Cold stress responsiveness in plants has also been associated with aquaporins. It was shown that cold promotes the expression of the water channel γTIP in Tulipa gesneriana associated with the stalk elongation (Balk & de Boer, 1999). In maize, a contribution of aquaporins to the recovery of root hydraulic conductance after chill injury was reported (Aroca et al., 2005). The hypothesis that aquaporins may be involved in the cryopreservation of animal cells was also considered. Data indicate that the regulation of aquaporins can attenuate cold-induced osmotic damage in rat kidney cells (Wang & Ben, 2004).

In summary, and following our experimental results, we propose that yeast aquaporins may have a relevant function restricted to low temperature.

Strains 10560-6B and YSH1172 were kindly provided by Gerald Fink, Whitehead Institute, Cambridge, USA and Stefan Hohmann, Göteborg University, Sweden, respectively. Plasmid pYX242/AQY2-1 was kindly provided by Vincent Laizé, Göteborg University, Sweden. This work was supported by Fundação para a Ciência e a Tecnologia, POCTI/AGR/57403/2004. A. V. received a fellowship (SFRH/BPD/8548/2002) from Fundação para a Ciência e a Tecnologia. A. T. received a fellowship from the Institute for Scientific and Technological research (IWT) and the Katholieke Universiteit Leuven (PDM/02/114). We thank V. Neves and A. Madeira for technical support.

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Received 9 November 2005; revised 20 January 2006; accepted 3 February 2006.