Plasma membrane aquaporin AtPIP2;5 is permeable to CO2 and contributes to mesophyll conductance of CO2 in leaves.
Keywords: Aquaporin, Arabidopsis, CO2, mesophyll conductance, photosynthesis, PIP, stomatal conductance, whole-plant transpiration
Abstract
The roles of different plasma membrane aquaporins (PIPs) in leaf-level gas exchange of Arabidopsis thaliana were examined using knockout mutants. Since multiple Arabidopsis PIPs are implicated in CO2 transport across cell membranes, we focused on identifying the effects of the knockout mutations on photosynthesis, and whether they are mediated through the control of stomatal conductance of water vapour (gs), mesophyll conductance of CO2 (gm), or both. We grew Arabidopsis plants in low and high humidity environments and found that the contribution of PIPs to gs was larger under low air humidity when the evaporative demand was high, whereas any effect of a lack of PIP function was minimal under higher humidity. The pip2;4 knockout mutant had 44% higher gs than wild-type plants under low humidity, which in turn resulted in an increased net photosynthetic rate (Anet). We also observed a 23% increase in whole-plant transpiration (E) for this knockout mutant. The lack of functional plasma membrane aquaporin AtPIP2;5 did not affect gs or E, but resulted in homeostasis of gm despite changes in humidity, indicating a possible role in regulating CO2 membrane permeability. CO2 transport measurements in yeast expressing AtPIP2;5 confirmed that this aquaporin is indeed permeable to CO2.
Introduction
Water flow across membranes, and thus through the plant, is regulated by aquaporins, which in addition to water may also conduct small neutral molecules and gases including carbon dioxide (CO2) and oxygen (O2) (Agre et al., 1993; Heckwolf et al., 2011; Zwiazek et al., 2017). Arabidopsis thaliana possesses 35 different aquaporin isoforms that are divided into four subfamilies (Johanson et al., 2001): plasma membrane intrinsic proteins (PIPs) located in the plasma membrane (Daniels et al., 1994; Kammerloher et al., 1994, 1995; Hachez et al., 2014), tonoplast intrinsic proteins (TIPs) localized to the tonoplast (Maurel et al., 1993; Beebo et al., 2009), Nodulin26-like intrinsic proteins (NIPs) with various membrane locations (Mizutani et al., 2006; Choi and Roberts, 2007), and small basic intrinsic proteins (SIPs) that are found in the membranes of the endoplasmic reticulum (Ishikawa et al., 2005). PIPs are involved in a variety of processes regulating plant water flow starting from the root through the stem, as well as into and out of the leaves (Javot et al., 2003; Fraysse et al., 2005; Da Ines et al., 2010; Ben Baaziz et al., 2012; Gambetta et al., 2013). Based on their phylogeny, PIPs are further divided into two subgroups, the PIP1s and PIP2s, with five and eight isoforms, respectively (Johanson et al., 2001). Water permeability varies between the isoforms (Kammerloher et al., 1994; Kaldenhoff et al., 1995, 1998; Chaumont et al., 2000; Li et al., 2015) and, in fact, PIP1s are believed to transport water only when part of a heterotetramer structure also including PIP2s (Fetter et al., 2004; Zelazny et al., 2007; Otto et al., 2010).
When a plant is provided with optimal light, water, nutrients, and temperature conditions, its rates of photosynthesis (Anet) are largely determined by the rate of CO2 delivery to mesophyll cells, which is limited by two resistances in series: first by the rate of diffusion of CO2 from the leaf exterior into the intercellular airspaces through the stomata, and second by the rate of diffusion from intercellular airspaces into the chloroplast, as described by mesophyll conductance (gm). In A. thaliana, AtPIP1;2 was the first aquaporin identified to be a significant contributor to gm due to its CO2 permeability (Heckwolf et al., 2011), but AtPIP1;4 has now also been recognized to facilitate CO2 diffusion across plasma membranes (Li et al., 2015). Isoforms of the PIP2 subgroup were believed to be specific to water until they were discovered to also conduct hydrogen peroxide (H2O2) (Dynowski et al., 2008). However, recently, AtPIP2;1 was also reported to conduct CO2 in addition to H2O and H2O2 (Wang et al., 2016). Since all PIPs have identical selectivity filters (Wallace and Roberts, 2004), which are major determinants of substrate permeability, it is reasonable to assume that other isoforms of the PIP1 and PIP2 subgroups may also contribute to CO2 diffusion across the plasma membrane and affect gm in leaves.
On the molecular scale, the structures and functions of PIPs have been reasonably well described in many plants, but this knowledge is largely limited to the cellular level, and scaling it up to the whole plant is more challenging, especially since aquaporin mutants lack an obvious phenotype under low evaporative demand conditions commonly used in Arabidopsis research. Our main aim was to determine the respective roles of three Arabidopsis PIP isoforms (AtPIP2;2, AtPIP2;4, and AtPIP2;5) in the regulation of stomatal conductance (gs) and gm, both of which can substantially limit rates of photosynthesis. At saturating light, the CO2 concentration drops to about half that of atmospheric (ca) at the sites of carboxylation (cc). The drawdown from ca to ci (intercellular CO2 concentration) is restricted by gs, accounting for ~60% of the limitation in CO2 diffusion, while gm accounts for the remaining 40%. Therefore, gm is a large, but still poorly understood, limitation to photosynthesis. Soil water deficit has similar effects on gs and gm (Warren, 2008a, b), indicating that they are interconnected and, at least in part, controlled by the same mechanisms. Furthermore, since most of the resistance to the diffusion of CO2 within the leaf comes from the liquid phase (Warren, 2008b), it is conceivable that gm could be regulated through the activity of aquaporins. Thus, PIPs may be instrumental in modulating the link between gs and gm. Ultimately, modulating PIP function to increase gm without altering gs would enhance Anet without an accompanying increase in transpiration, and improve plant water use efficiency.
Past studies of the functions of aquaporins have generated a wealth of information concerning single isoforms in Arabidopsis, maize, and various other herbaceous and woody plant species (Fetter et al., 2004; Zelazny et al., 2007; Ben Baaziz et al., 2012; Gambetta et al., 2013; Li et al., 2015). However, the multitude of different species and methods employed also makes it difficult to develop a cohesive picture of the roles of aquaporins in plants. In this study, we compared three different single knockout mutants of A. thaliana and their wild type (WT) to clarify their putative roles in whole-plant function. Assigning more clearly defined and specific roles to the different isoforms will aid in determining whether there is redundancy among plant aquaporins. An indication that different aquaporins are not redundant is given by their differing expression patterns. In adult plants, AtPIP2;2 is highly expressed throughout the plant (Javot et al., 2003), while AtPIP2;5 reaches moderate to high levels of expression in mature leaves and guard cells, respectively (Alexandersson et al., 2010). However, its expression levels are lower in roots (Alexandersson et al., 2005), while AtPIP2;4 is only moderately expressed in leaves but highly expressed in roots (Javot et al., 2003). Since the function of PIPs also depends on their mutual interactions in the tetramer structure (Fetter et al., 2004; Zelazny et al., 2007; Otto et al., 2010), we furthermore examined two double mutants (pip2;2x2;4 and pip2;4x2;5) as well as a triple mutant (pip2;2x2;4x2;5).
In the present study, we grew plants in two environments differing in their ambient relative humidity, to compare plant responses to different vapour pressure deficits (Vpds). A high Vpd promotes high rates of transpiration and thus triggers plant responses aimed at conserving water such as stomatal closure. Earlier studies failed to find a visible phenotype for aquaporin knockout mutants growing under ideal (low Vpd) conditions (Javot et al., 2003; Da Ines et al., 2010; Heckwolf et al., 2011; Wang et al., 2016), so this high Vpd treatment was applied to increase the relative contribution of aquaporins to plant water flow and the likelihood of producing a distinct phenotypic response. We therefore hypothesize that PIP2 knockout mutants would produce a phenotypic response under conditions of high Vpd, which, under low Vpd, would go unnoticed or show as statistically non-significant trends only.
Materials and methods
Plant material
T-DNA single knockout mutants of A. thaliana were obtained from the Nottingham Arabidopsis Stock Centre (NASC; www.arabidopsis.org) for the following aquaporin grnes: PIP2;2 (N871747), PIP2;4 (N105980), and PIP2;5 (N117303) in the Columbia background (Alonso et al., 2003). All genotypes were checked by PCR to confirm the correct T-DNA insertion and homozygosity. Only homozygous plants were used to grow a seed stock and in the subsequent experiments. Multiple knockout plants were created by crossing, which resulted in a total of two different double mutant lines—pip2;2x2;4, pip2;4x2;5—and one triple mutant—pip2;2x2;4x2;5. It was not possible for us to create the pip2;2x2;5 mutant for this study.
Since gm acclimates to the environmental conditions (Warren, 2008b), we grew the plants under different humidities in situ in the two environments differing in Vpd instead of raising them in the same conditions and subjecting them to short-term treatments, which would probably affect both gm and gs and thus prevent us from separating the role of aquaporins in these two processes. The environmental parameters for the high humidity and low humidity conditions are summarized in Supplementary Table S1.
Low humidity growing conditions
The experiment was carried out in a greenhouse at the University of Sydney, Sydney, Australia. Seeds of the A. thaliana genotypes were sown in pots containing a pre-fertilized potting mix (Scotts Osmocote, plus trace elements) and germinated in the light under the conditions described in Supplementary Table S1. Seedlings were transplanted 4 d after germination into 700 ml pots. Pots were overfilled with the same potting mix, as described in Flexas et al. (2007b). Young seedlings were kept under a transparent plastic cover for several days after transplanting to keep them moist. The pots were arranged randomly and rearranged every second day to ensure even light interception and to minimize any effects of air movement caused by the air conditioning. All measurements were carried out between 09.30 h and 16.30 h on 25- to 39-day-old plants using only fully expanded leaves at least 4 cm long. Anet is reported to be stable over this time period (Flexas et al., 2007b). The experiment was conducted during the Australian spring from mid-October to mid-December 2015. During this time, new seeds were planted at weekly intervals to continuously provide plants of equivalent ages for measurements.
Plants were provided with ample water in order to prevent soil water stress signalling from the roots, since our aim was to expose plants to low air humidity without imposing other accompanying stresses. Water was provided from below as soon as the soil surface had dried (every 2–3 d), but after the day’s measurements.
High humidity growing conditions
This part of the experiment was carried out in a growth room at the University of Helsinki, Helsinki, Finland. Seeds of the A. thaliana genotypes were sown and grown in a pre-fertilized peat–vermiculite mixture (1:1) in 350 ml pots. Seedlings were transplanted 4 d after germination into overfilled pots as described above. Plants were grown in a growth chamber under conditions described in Supplementary Table S1. Measurements were carried out between 09.00 h and 16.00 h from October 2016 until January 2017 on 27- to 33-day-old plants using only fully expanded leaves at least 4 cm long. The plants were watered as in the low humidity treatment described above; however, due to the higher air humidity in these growing conditions, watering was required only once a week.
Gas exchange measurements
All gas exchange measurements were carried out with the portable photosynthesis system LI6400XT infrared gas analyser equipped with a fluorescence chamber (LI-COR Biosciences, Lincoln, NE, USA) during the same 7 h time window every day. The leaf chamber (leaf chamber fluorometer), a 2 cm2 circular cuvette, allowed single leaves to be measured.
Photosynthetic light responses were measured under non-photorespiratory conditions in the low air humidity (LH) treatment (1% O2, 400 µmol mol–1 CO2) to determine the relationship between photosynthetic rate and light intensity as well as the rate of electron transport (J). High purity N2 gas (BOC Gas, Australia) was mixed with air to create a 1% O2 mixture, directly attached to the air inlet of the LICOR-6400. Under non-photorespiratory conditions, J is entirely dependent on gross photosynthesis A (Warren and Dreyer, 2006):
(1) |
where Rd is the respiration in the light. The curves were measured using an automated program with the following fixed settings: temperature 25 °C; leaf fan, fast; reference CO2 concentration (CO2R), 400 µmol mol–1; flow, 300 µmol s–1; and 10% blue light. Light adaptation lasted for 30 min at maximum irradiance [photosynthetically active radiation (PAR) 2000 µmol m–2 s–1]. The light curves began at the highest irradiance and decreased at ~4 min intervals of acclimation time between each step: 2000, 1500, 1000, 500, 200, 100, 50, 20, and 0 µmol m–2 s–1. Light curves measured under high air humidity (HH) were measured using the same automated program, but under ambient O2 concentrations.
Full A–ci curves were measured in the high humidity growth chamber experiment to determine whether the standard CO2 concentration used in our gas exchange measurements falls within the CO2-limiting range for all plant lines. An automated program was used throughout the curve with the same settings as for the light curves except a constant PAR of 1500 µmol m–2 s–1. Plants acclimated for 10 min in the leaf chamber before the first measurement at 400 µmol mol–1 CO2. After the first measurement, the following steps with 3 min acclimation time between each step were used to obtain a complete A–ci curve: 450, 550, 650, 750, 850, 1000, 1500, 2000, 400, 350, 300, 250, 200, 150, 100, and 50 µmol mol–1 (Warren and Dreyer, 2006).
The Laisk method (Laisk, 1977; Brooks and Farquhar, 1985) was used to estimate ci* (photorespiratory compensation point) and Rd. In both experiments, LH and HH conditions, an automated program with the same settings was used for the Laisk method: temperature, 25 °C; leaf fan, fast; CO2R, 400 µmol mol–1; flow, 200 µmol s–1; PAR, 1500 µmol m–2 s–1; and 10% blue light. The A–ci curves were measured at PAR 300, 150, 100, and 50 µmol m–2 s–1 and, after each curve, CO2 was returned to 400 µmol mol–1 for 5 min to maintain Rubisco activation. The CO2 steps used for the curve were 150, 125, 100, 75, and 50 µmol mol–1 with ~3 min acclimation time between each step.
g min describes the minimum conductance; that is, the rate of water loss from leaves due to direct diffusion through the cuticle and leaky stomata. This pathway for gas exchange is often neglected as it represents only values in the range of 5–10 mmol m–2 s–1 H2O (Fig. 3B; Supplementary Table S2; Duursma et al., 2019) as compared with a gs of 100–400 mmol m–2 s–1 for actively transpiring Arabidopsis leaves (Fig. 1C). Nevertheless, all gas exchange data were adjusted to account for gmin as well as any CO2 leaks into or out of the LICOR measuring chamber. We estimated gmin for fully expanded leaves using the protocol described by Sack and Scoffoni (2010) with some modifications to accommodate fragile and small Arabidopsis leaves: for each data point, three leaves that were suitably large for gas exchange measurements were excised from 21 plants per line close to the centre of the rosette. The leaves were weighed for initial FW, placed flat on millimetre graph paper, and photographed to calculate their initial leaf area using ImageJ as described by Wang (2016). After photographing, they were placed on labelled Petri dishes and allowed to dry at room temperature (20 °C) for 1 h until complete stomatal closure. From this point on, leaves were weighed every 25–30 min. The first time point after the 1 h drying period was taken to be time 0. After 6–10 time points had been obtained over the course of 3–4 h, the leaves were again photographed to calculate their final leaf area. The collected data were input into the ‘gmin Analysis Spreadsheet Tool’ (Sack and Scoffoni, 2010) in order to calculate gmin.
The same leaves that had been used for estimating gmin were floated on water overnight to obtain their saturated weight (SW). Finally, the leaves were dried in a drying oven overnight at 60 °C to obtain their DW. The relative water content (RWC) was then calculated using the following formula:
(2) |
The leak flow was calculated using the manufacturer’s instructions; however, we placed an intact leaf in the chamber instead of carrying out the estimation for an empty chamber. In the dark, the leaf’s respiration rates should not be affected by changing CO2 concentrations or flow rates and thus can be considered constant. Therefore, we were able to obtain a diffusion coefficient of 0.40 mol s–1 for the actual measuring conditions, which is similar to the 0.44 mol s–1 obtained by Flexas et al. (2007a).
The mesophyll conductance of CO2 was estimated using the variable J method as described by Harley et al. (1992):
(3) |
The variables A, ci, and J were obtained from the combined gas exchange and chlorophyll fluorescence measurements. Rd as well as ci* were estimated from the Laisk method using slope–intercept regression (Walker and Ort, 2015). One of the largest sources of error when using the variable J method to estimate gm can be the mismatch between the measurement of electron transport rates and photosynthesis (Flexas et al., 2013), however, for thin Arabidopsis leaves, this discrepancy is relatively small. For each estimate of gm, we also calculated the δCc/δA as described in Harley et al. (1992) and excluded measurements that fell outside the recommended range of 10 <δCc/δA <50.
(4) |
As we did not find any statistically significant differences in either Rd or ci* between the different genotypes, we calculated a global average for both variables (Rd=0.914±0.031 µmol m–2 s–1, n=69; ci*=38.95±0.70 µmol mol–1, n=65) in order to obtain a more robust estimate of gm. In comparison, Walker and Ort (2015) reported values of Rd=1.04±0.33 µmol m–2 s–1, ci*=40.0±0.7 µmol mol–1 for Nicotiana tabacum and Rd=1.02±0.22 µmol m–2 s–1, ci*=40.8±2.4 µmol mol–1 for Glycine max.
The average gm obtained for each mutant line was used to calculate A–cc curves from the previously measured A–ci curves. Parameters Jmax (maximum rate of electron transport), Vcmax (maximum rate of carboxylation), and the inflection point shown in Supplementary Table S2 were estimated from fitted A–cc curves utilizing the ‘Plantecophys’ R package version 1.4.4 (Duursma, 2015) using the chloroplastic Michaelis–Menten constants for CO2 (Kc) and O2 (Ko) at cc as described by Bernacchi et al. (2002), which allowed us to calculate Km=620.3322 to be used in the curve fit. The fitted A–cc curves were not normalized to 25 °C as the measurements were done at this temperature and the Rd as well as ci* estimates presented above were provided to obtain a more accurate fit. Using an orthogonal non-linear least-squares regression (‘onls’ package in R), the following parameters were extracted from the light curves: saturating photosynthesis (Asat), quantum efficiency (φ), Rd, degree of curvature between the light-limited and CO2-limited part of the curve (θ), light compensation point (LCP), and irradiance at 75% Asat (Supplementary Table S2).
Whole-plant transpiration measurements
We estimated the water transpired by entire plants under the LH and HH growing conditions over a 30 d period. This experiment at the University of Helsinki used a Fitoclima 1200 growth chamber (Aralab, Rio de Mouro, Portugal) to create the LH and HH growing conditions (day length, temperature, humidity, etc.). The air circulation inside the chambers was set to maximum to ensure adequate ventilation and a high boundary layer conductance. A total of 10–16 plants of each genotype were planted in 350 ml pots which had their soil surface sealed with a plastic membrane preventing evaporative water loss from the pot. A small hole was cut into the membrane through which the plants grew. Prior to transplanting, the pots were saturated with water to their water-holding capacity (52% gravimetric soil moisture content in this case). Immediately after transplanting, the pots were weighed with the plastic cover and the plant in order to obtain the initial weight (Wi). Thereafter, pots were weighed roughly every 2 d and, if necessary, a known volume of water was added to the soil surface using a syringe. Soil moisture was maintained at a minimum of 25% (gravimetric), ensuring the soil surface never dried up completely. Total leaf area was measured weekly for each plant using ImageJ as described by Wang (2016) and, at the end of the experiment, plant FW was measured. The total amount of water transpired by each plant was calculated with respect to cumulative leaf area using the following formula:
(5) |
where V denotes the volume of water added to one pot over the course of experiment, Wi is the initial weight of the pot including the plant, Wf the final weight of the pot including the plant at the end of the experiment, FW is the fresh weight of the plant at the end of the experiment, and At is the total cumulative leaf area of the plant over the course of 30 d.
RNA extraction and cloning
Tissue from 6-day-old seedlings of A. thaliana ecotype Columbia-0 were used for RNA extraction. Total RNA was extracted using the QIAGEN RNeasy Plant Mini Kit (Qiagen, Valencia, CA, USA). RNA concentration and purity were assessed using the Thermo Scientific™ NanoDrop™ One Microvolume UV-Vis Spectrophotometer (Thermo Scientific, Waltham, MA, USA). The first-strand cDNAs were synthesized from 1 μg of total RNA using Superscript II reverse transcriptase (Invitrogen, Carlsbad, CA, USA) and an oligo(dT) primer. Coding sequences of Arabidopsis PIP2;5 (AT3G54820) and carbonic anhydrase 1 (CA1; AT3G01500) were amplified with Phusion DNA Polymerase using the primers listed in Supplementary Table S4. The PCR products of the expected size were eluted from the gel and purified using the Wizard® SV Gel and PCR Clean-Up System (Promega, Madison, WI, USA). The PCR products were then cloned into a pCR2.1-TOPO vector using the Topo TA Cloning kit (Invitrogen) and transformed into DH5α chemically competent cells (Invitrogen). About 3–6 white colonies were sequenced for each PCR product using M13 sequencing primers.
Plasmid construction and yeast transformation
The ORF of AtPIP2;5 and carbonic anhydrase 1 (AtCA1) were cloned as Gateway entry clones in plasmid pDONR221 (Invitrogen). ORFs of AtPIP2;5 and CA1 from the entry clones were shuttled into the galactose-inducible yeast expression plasmid pAG426GAL-ccdB (Addgene: Plasmid #1415) and pAG425GAL-ccdB (Addgene: Plasmid #14153), respectively, by Gateway LR cloning reaction. The S.c. EasyComp™ Transformation Kit (ThermoFisher Scientific) was used to transform the Saccharomyces cerevisiae yeast strain (INVSc1 from ThermoFisher Scientific) with each plasmid DNA. Double transformants used for CO2 permeability measurements containing AtCA1 and AtPIP2;5 (AtCA1::AtPIP2;5) constructs were selected by ura3 and leu2 complementation. Expression of the constructs was verified by quantitative real-time PCR (qRT-PCR) using SYBR Green I dye in an Applied Biosystems 7500 Fast system.
Subsequently, the subcellular localization of AtPIP2;5 in yeast cells was investigated using fluorescence microscopy (Supplementary Fig. S2). The attB-PCR fragment of AtPIP2;5 was transferred into pDONR221 with BP clonase and shuttled from the entry clones into the yeast expression plasmid pAG426Gal-ccdB-eGFP by Gateway LR cloning reaction to generate C-terminally tagged protein–enhanced green fluorescent protein (eGFP) fusions. Yeast transformation was carried out as described above. Single colony isolates of the yeast strains were grown to midlog phase in 2% Glu/−Ura medium at 30 °C. Cultures were spun down and re-suspended in the same volume of 2% Gal/−Ura to induce expression of the constructs.
The yeast strains expressing pAG426Gal::At2;5, pAG425Gal::AtCA, and PAG426Gal::At2;5XpAG425Gal::AtCA were induced by changing the carbon source of the medium from glucose to galactose for 24 h (1.2 g, 30 °C). RT-PCR was performed to determine the relative abundance of mRNA in the yeast strains. An RNeasy Mini Kit (QIAGEN, Venlo, Limburg, The Netherlands) was used to extract total RNA from the yeast cells according to the manufacturer’s instructions. The QuantiTect Reverse Transcription Kit (Qiagen) was used to synthesize first-strand cDNAs with 500 µg of total RNA, according to the manufacturer’s instructions, and the qRT-PCR was performed as above. The relative expression of all genes was calculated using the ΔΔCt method with actin as a reference gene (Supplementary Fig. S3).
CO2 transport measurements
The entry of CO2 through the plasma membrane was followed by intracellular acidification and decreased fluorescence in whole yeast cells loaded with fluorescein diacetate. Loading of the yeast cells was carried out according to the protocol described by Bertl and Kaldenhoff (2007). In brief, cells were harvested by centrifugation and then resuspended in loading buffer (50 mM HEPES-NaOH pH 7.0, 5 mM 2-deoxy-d-glucose) with 50 μM fluorescein diacetate, incubated for 14 min at 30 °C, shaken at ~225 rpm, and centrifuged again at 1700 g for 3 min at 4 °C. The cells were then resuspended in incubation buffer (25 mM HEPES. 75 mM NaCl) and kept on ice until use. Before use, the cells were resuspended in incubation buffer to a final OD600 of 60, after which 50 μl were dissolved in the incubation buffer and mixed rapidly in a 1:1 (v/v) ratio with CO2-Mixing Buffer (25 mM HEPES, 75 mM NaHCO3, pH 6) at a rate of 100 μl s–1 in a stopped flow spectrophotometer (Applied Photophysics, DX.17 MV). Entry of CO2 into yeast cells expressing AtCA1 resulted in H2CO3– formation (and subsequent dissociation into H+ and CO3–) and thus intracellular acidification, as indicated by a decrease in fluorescence intensity. The spectrophotometer emitted at a λ of 490 nm (maximum excitation wavelength of the fluorescein). The receiver had a filter attached that did not allow the passage of wavelengths below 515 nm, because fluorescein emits at a λ of no longer than 514 nm. The fluorescence was recorded over time and the conductivity quantification (K-relative) was calculated by fitting the experimental data to a decreasing exponential function during the first 8.0 ms using SigmaPlot 11.0 (Systat Software Inc., Chicago, IL, USA).
Gene expression analysis
Transcript abundance was measured by qRT-PCR for each plant line and growing condition. Under LH, 4–6 rosettes/genotype, and under HH 12 rosettes/genotype were harvested and immediately frozen in liquid nitrogen. Due to the larger sample number under HH, we combined three samples and treated them together, resulting in n=4 for HH. RNA was extracted using the GeneJET Plant RNA Purification Mini Kit (ThermoFisher Scientific) according to the manufacturer’s instructions, with the exception that the Plant RNA Lysis Solution was supplemented with β-mercaptoethanol instead of DTT. The quality and concentration of the extracted RNA were determined with an ND-1000 Spectrophotometer (ThermoFisher Scientific), and 1 µg of RNA was used for cDNA synthesis following DNase I treatment. Maxima H Minus Reverse Transcriptase, oligo(dT)19, and dNTP (ThermoFisher Scientific) were used in a 30 µl reaction volume for cDNA synthesis, which was then diluted to a final volume of 70 µl. A 1 μl aliquot of cDNA was used for PCR in triplicate with 5× HOT FIREPol EvaGreen qPCR Mix Plus (Solis BioDyne, Tartu, Estonia) with a CFX 384 Real-Time PCR detection system (Bio-Rad, Hercules, CA, USA) in triplicate. PIP-specific primers were taken from Alexandersson et al. (2010) and information on reference gene primers can be found in Supplementary Table S4. Ct values were converted using the ΔΔCt method employing all three reference genes listed in Supplementary Table S4 and ln-transformed for statistical analysis.
Data processing and statistical analysis
ANOVAs were conducted separately for the LH and HH experiment in R (package Deducer) using a linear model with plant genotype and the measured variable as the factors, and for each graph/panel we calculated the pooled standard error except for gene expression data. For estimations of gmin and RWC, n = 21; for all gas exchange measurements, n=3–9; for whole-plant transpiration, n=10–16; while for gene expression, n=4–12. Tukey’s multiple comparison was used to compare the means of all measured variables for the mutant lines with the WT as well as with each other.
Generalized additive mixed modelling (GAMM, package=‘mgcv’) (Wood, 2017) was used to evaluate the photosynthetic response curves, with the mutant line as a parametric term and a smoothing term for PAR and ci. Due to heterogeneous variation, we employed the weighting function ‘weights=varExp’. The fluorescence decay rates from the stopped-flow measurements were compared using Duncan’s multiple range test.
Results
Effects of PIP2 aquaporins on gas exchange under high and low humidity
The difference in evaporative demand between the HH and LH growing conditions had a clear effect on gas exchange and was most strikingly visible in the values of gs and its consequences for Anet (Fig. 1A–D).
In the LH environment, all plant genotypes displayed 41–61% lower gs than in the HH environment (Fig. 1C, D). However, single and double mutant plants lacking AtPIP2;4 decreased their stomatal conductance less than the WT in response to LH. The stomatal conductance of the pip2;4, pip2;2x2;4, and pip2;2x2;4x2;5 mutants was significantly higher than that of the WT under LH, but nevertheless reduced compared with the HH treatment (41, 53, and 57% for pip2;4, pip2;2x2;4, and pip2;2x2;4x2;5, respectively). The WT gs under LH was reduced by 57% compared with HH.
In the HH environment, there was a tendency for the genotypes lacking AtPIP2;2 to have higher values of gs compared with the WT (pip2;2, P=0.089; pip2;2x2;4, P=0.055; and pip2;2x2;4x2;5, P=0.091). Although for the individual mutants alone this was not a statistically significant effect at P<0.05, when all mutant plants lacking AtPIP2;2 were considered together as a group, the increase of 28% compared with the WT was statistically significant.
Those genotypes in which Vpd had a large effect on gs also displayed large differences in Anet (Fig. 1A–D; Supplementary Table S2). In the WT, Anet was reduced by 34% in the LH environment compared with the HH environment, whereas the reduction was only 11% for pip2;4. Rates of photosynthesis were very uniform among all genotypes under the HH condition (Fig. 1A, B). Under LH, however, Anet declined less in pip2;4 and pip2;4x2;5 than in the WT, as would be expected given their smaller decrease in gs from HH to LH compared with the WT. In addition, the pip2;5 single mutant had lower values of Anet than the pip2;4x2;5 double mutant under both growing conditions.
The gm of the mutant plants did not significantly differ from that of the WT under either LH or HH conditions (Fig. 1E). However, unlike Anet or gs, gm increased under LH in all genotypes except pip2;5. Pairwise comparisons revealed that pip2;5 tended to have a lower gm than pip2;4x2;5 and pip2;2x2;4x2;5 under HH (Fig. 1E, F). Similarly, under LH, pip2;5 had marginally lower gm compared with pip2;4, pip2;2x2;4, and pip2;2x2;4x2;5 (Fig. 1E, F). There was a similar pattern of typically lower Anet in pip2;5 versus pip2;4x2;5 or pip2;2x2;4x2;5 (Fig. 1A).
The Vpd in the cuvette during measurements differed ~2-fold in LH versus HH, affecting both Anet and gs, with individual plants, as well as means for each genotype, forming two distinct clusters (Fig. 1B, D, F). Values of gm differed less, but nevertheless also formed two distinct clusters. Variation in cuvette Vpd was larger under LH (2.0–2.5 kPa) than under HH (1.0–1.25 kPa), but none of the genotypes differed significantly from the WT under either growing condition (Supplementary Table S2), and thus Vpd does not account for statistically significant differences in Anet, gs, or gm among genotypes.
Whole-plant transpiration
Whole-plant transpiration (E) was measured over the course of 30 d beginning from germination to determine whether genotypic variation in instantaneous leaf-level gas exchange measurements scaled to long-term whole-plant differences in water use. Despite the higher gs (Fig. 1C) under HH growing conditions, E was low and did not differ among genotypes (Fig. 2). Under LH conditions, E was 3–4 times higher, with E of pip2;2 and pip2;4 significantly higher than that of the WT, which is in line with their increased gs under the same LH growing conditions. Despite similar values of gs (Fig. 1C), pip2;2x2;4 and pip2;4x2;5 did not differ significantly from the WT in their whole-plant transpiration.
Effects of PIP2 aquaporins on mesophyll conductance under high and low humidity measured through A–response curves
Using the mean gm for each mutant line, we calculated A–cc curves (Supplementary Fig. S1) from the measured A–ci curves to detect effects of the PIP2 mutations on the limits of CO2 fixation. There were no significant differences among the genotypes for either the Jmax or Vcmax (Supplementary Table S2). Furthermore, there were no differences in ci/ca at low CO2 (<400 µmol CO2 mol–1 air), but at high CO2 (>400 µmol CO2 mol–1 air), ci/ca was significantly lower in all mutants lacking AtPIP2;5 than in the WT (Fig. 3A).
In line with the steady-state measurements of gas exchange, pip2;5 produced light–response curves with lower values of Anet, as well as gs, than the other genotypes (13% and 5% lower, respectively, compared with the WT; Fig. 4). At the points on the curve at saturating PAR (500–2000 µmol m–2 s–1 for these plants), Anet was similar in the WT plants and the examined genotypes (Fig. 4). However, for measurement points at subsaturating PAR (<500 µmol m–2 s–1), Anet of pip2;5 was lower than that of all other genotypes including the WT (21–50% lower), which resulted in a significantly lower quantum efficiency, φ. At low light intensities, gs did not differ among genotypes, whereas at higher light intensities (1000–2000 µmol m–2 s–1), pip2;5 displayed significantly lower gs compared with all other genotypes including the WT. In addition to the traditional parameters extracted from photosynthetic light–response curves, we also used GAMM which enabled us to also analyse the mutants’ stomatal response to changing light intensities. These analyses confirmed the differences in the shape of light–response curves, which were significant for Anet, corroborating the significant difference we report in φ, as well as gs in pip2;5 compared with the WT. Furthermore, the curves for pip2;2 and pip2;2x2;4x2;5 also differed significantly from the WT in the response of gs to increasing PAR.
The light–response curves measured under HH (Fig. 4 top) were also in line with the steady-state gas exchange measurements and did not produce significant differences between the mutants and the WT, with the exception of Asat, which was lower for pip2;2, pip2;2x2;4, and pip2;4x2;5.
Values of the minimum conductance of water (gmin) (Fig. 3B) were within the expected range of 5–10 mmol m–2 s–1. No significant differences in gmin were found between the WT and any of the mutants. Only gmin of pip2;2x2;4x2;5 tended to be higher than the WT, and higher than pip2;4 and pip2;2x2;4.
CO2 conductance of AtPIP2;5 expressed in yeast
Yeast cells expressing either AtPIP2;5, AtCA1, or both, and loaded with fluorescein diacetate, displayed significantly different fluorescence intensities after the application of the CO2 mixing buffer (Fig. 5A). Fluorescence intensity did not decrease in yeast cells expressing only AtPIP2;5, because AtCA1 was not present and thus no significant acidification occurred (Fig. 5B). This assay was used as the first control. Yeast cells expressing only AtCA1 were used as a second control in order to quantify the CO2 permeability of the yeast membrane in the absence of AtPIP2;5. These cells displayed a slight decrease in fluorescence intensity due to CA1-facilitated formation of H2CO3– and subsequent intracellular acidification (Fig. 5B). When both AtPIP2;5 and AtCA1 were expressed together, the fluorescence intensity decreased markedly (Fig. 5B).
Gene expression
The expression levels of PIP genes (Fig. 6) were generally higher under LH as compared with HH, and this effect was statistically significant for PIP1;2, PIP1;3, PIP2;1, PIP2;2, and PIP2;4. Under both growing conditions, the knockout mutations generally had no significant effect on the expression of other PIP genes, though there are a few notable exceptions. For example, compared with the WT, in pip2;2 there was significant up-regulation of PIP2;1 and PIP2;4 under HH, whereas under LH, PIP1;5 and PIP2;8 were up-regulated and PIP2;3 down-regulated. In pip2;4, compared with the WT, the effect on other PIP genes was small under HH, with only PIP2;1 significantly up-regulated, but under LH, PIP1;3, PIP1;5, and PIP2;2 were up-regulated while the expression of PIP2;5 was strongly reduced (Fig. 6).
Discussion
Similarly to earlier reports (Javot et al., 2003; Da Ines et al., 2010; Heckwolf et al., 2011; Wang et al., 2016), the leaf gas exchange of the Arabidopsis plants grown under HH conditions did not appear to be affected by PIP knockout mutations as is apparent from the very uniform values of Anet, gs, and E. Increasing the evaporative demand (higher Vpd) by lowering ambient air humidity increased water flow through the plant (Fig. 2), and hence the contribution of aquaporins to the regulation of water flow through the plant also probably increased, which in part can be seen in the increased PIP expression under LH (Fig. 6). By allowing plants to grow from germination under LH conditions, we aimed to amplify any differences in water relations between the WT and knockout mutants (Fig. 1).
AtPIP2;5 responds to various stresses such as H2O2 (Hooijmaijers et al., 2012) and salt (Lee and Zwiazek, 2015), as well as being up-regulated by drought (Alexandersson et al., 2010), but is only expressed at intermediate levels under standard growing conditions, especially in the roots (Jang et al., 2004; Lee et al., 2012). Thus the WT and the pip2;5 mutant had a similar Anet and gs in our HH environment. However, while gm increased in every other genotype grown under LH, pip2;5 showed no change (Fig. 1E). Furthermore, light–response curves from plants grown under LH (Fig. 4 bottom) showed Anet and gs of this mutant to be significantly less than those of the WT. Soil water deficit commonly decreases gm (Warren et al., 2004; Warren, 2008a, b) but, since our plants were not experiencing such stress, the inability of pip2;5 to maintain high Anet and gm led us to conclude that AtPIP2;5 is involved in the regulation of gmin planta. Our stopped-flow measurements on yeast cells expressing AtPIP2;5 support this. When AtPIP2;5 and AtCA1 were co-expressed, CO2 entry into the cells was >100-fold more rapid than in the controls, indicating that the CO2 permeability of the membrane was drastically increased by the insertion of AtPIP2;5. Thus, AtPIP2;5 is clearly permeable to CO2, when expressed in yeast, and its ability to regulate gm is likely to be due to it directly facilitating CO2 diffusion across the cell membrane. AtPIP2;5 has not previously been shown to alter CO2 fluxes across cell membranes to affect gm nor has it, to our knowledge, been tested for CO2 permeability.
Up-regulation of AtPIP2;5 during drought differentiates it from most other PIPs, and the lack of functional AtPIP2;5 in combination with LH may thus have triggered the drop in gm. Furthermore, it is only weakly co-expressed with one other PIP isoform, AtPIP1;4 (Alexandersson et al., 2010), the expression of which was not significantly affected in pip2;5 (Fig. 6). However, in the very same mutants, the missing interaction of AtPIP1;4 with AtPIP2;5 may compromise the proper insertion of AtPIP1;4 into the plasma membrane. AtPIP2;5 may thus also be involved in maintaining gm across a greater range of watering and humidity regimes by affecting the function of AtPIP1;4 (Fetter et al., 2004; Zelazny et al., 2007; Otto et al., 2010), which is not only up-regulated by drought (Alexandersson et al., 2010), but has been shown to also contribute to CO2 membrane permeability (Li et al., 2015). Further evidence to support this theory is provided by the results of our light–response curves where gs was similar for all genotypes, whereas Anet was clearly lower in pip2;5 than in the other genotypes. Therefore, contrary to our expectations, gs did not behave like Anet in pip2;5 in response to a changing light environment, particularly at subsaturating PAR. It would therefore appear that AtPIP2;5, despite its relatively low abundance (Lee et al., 2012), does reduce resistance to CO2 diffusion through the mesophyll under light- and CO2-limiting conditions.
Further evidence in support of AtPIP2;5 regulating gm is provided by our A–ci curves. Its knockout mutation did not appear to significantly affect Jmax or Vcmax, which was not unexpected since none of the PIPs has previously been shown to impact chlorophyll fluorescence or CO2 fixation by Rubisco. However, at high [CO2], the ci/ca was significantly lower for all mutants lacking AtPIP2;5 than for the WT (Fig. 3A). Since ca was constant, the lower ci/ca was due to lower ci, probably the result of an incremental effect on a combination of Anet and gs during the A–ci curve or to an increase in gm.
AtPIP2;2 is amongst the most abundantly expressed PIPs in the plant (Javot et al., 2003; Da Ines et al., 2010), but, despite these high levels of expression, its knockout mutation induced no visible phenotype in our study or elsewhere (Javot et al., 2003). However, unlike past reports, we found compensatory up-regulation of other PIP genes (Fig. 6) in mutants lacking functional AtPIP2;2 grown under both LH and standard HH conditions. Javot et al. (2003) found a 14% reduction in the osmotic water conductivity of the root and hypothesized that AtPIP2;2 plays a crucial role in root water uptake under conditions of low evaporative demand, as in our HH treatment. In our study, two highly expressed genes, AtPIP2;1 and AtPIP2;4, were up-regulated in pip2;2 rosettes. It is reasonable to assume that these two genes would also have been up-regulated in the roots, potentially explaining why water uptake by the roots as well as flow through the plant was not significantly altered in this mutant. Further support for this assumption is provided by the finding that the root anatomy of pip2;2 did not differ from that of the WT (Javot et al., 2003).
Interestingly, under LH, gs of mutants lacking AtPIP2;2 did not significantly differ from that of the WT. Although AtPIP2;2 has previously been shown to be drought sensitive (Alexandersson et al., 2010), our plants were only subjected to LH and in fact we observed quite the opposite. AtPIP2;2 was significantly, though moderately, up-regulated under LH compared with HH. Furthermore, whole-plant transpiration in pip2;2 was significantly higher than that of the WT under LH, indicating that water uptake and flow are not impaired by the lack of functional AtPIP2;2 at the whole-plant level, but may even be overcompensated. Together with the fact that gs increased under HH in mutants lacking AtPIP2;2, this suggests that AtPIP2;2 may be involved in regulating plant water balance in response to changes in Vpd.
In the LH environment, pip2;4 had higher gs and E than the WT. Lack of functional AtPIP2;4 clearly increases the amount of water lost by the plant (Fig. 2), reducing the plants’ overall water use efficiency. However, this lack of function enabled pip2;4 plants to maintain higher values of Anet and gm than the WT. Similar effects were found in the double mutants, both of which also lacked functional AtPIP2;4. This aquaporin is thus a likely candidate for manipulating plant water relations to improve plant carbon gain, though at the expense of water use efficiency.
Since all mutant plants had similar or higher gs and E than the WT under both growing conditions, this clearly indicates that none of the knockout mutations sufficiently disrupts root water uptake to a degree that could not be compensated for. Thus these mutants did not have a visible phenotype. Furthermore, the lack of significant differences in gmin (Fig. 3B) or RWC (Supplementary Table S2) suggests that the observed effects on gs and gm are unlikely to be due to an effect of the knockout mutation on leaf water status. Another factor potentially affecting leaf water status is boundary layer resistance. However, high air circulation decreases this resistance to a negligible minimum under both LH and HH conditions, as well as within the leaf chamber during gas exchange measurements. Therefore, the reported differences between the mutants and the WT are more likely to directly result from the knockout mutation and lack of aquaporin function, rather than being an indirect effect caused by altered plant water status.
We report that AtPIP2;5 is permeable to CO2 when expressed in yeast and that it contributes to the regulation of mesophyll conductance of CO2 in leaves of A. thaliana under conditions of high evaporative demand. AtPIP2;4 may play a role in maintaining plant water status, so may also be a suitable target for crop improvement, since the lack of functional AtPIP2;4 led to a 29% increase in Anet when VPD was high, though at the expense of water use efficiency. Identification of the mechanisms underpinning these results may represent the means of teasing apart the factors regulating gs and gm.
Supplementary data
The following supplementary data are available at JXB online.
Table S1. Summary of the main environmental variables under high and low humidity.
Table S2. Gas exchange data and variables calculated from the A–response curves under high and low humidity.
Table S3. Two-way ANOVA for whole-plant transpiration.
Table S4. Primers used in this study.
Fig. S1. A–cc curves for all plant lines.
Fig. S2. Fluorescence images of transformed S. cerevisiae cells.
Fig. S3. Expression levels of AtPIP2;5 in S. cerevisiae.
Acknowledgements
We thank Mikael Brosché for providing the seeds of the knockout mutants, and Mohsina Siddique and Baiba Matule for support with experimental work in Helsinki.
This work was funded by the Finnish Cultural Foundation (grants #00180402 and #00160334) to DI. TMR was funded by the Academy of Finland decision #324555.
Glossary
Abbreviations
- A net
net photosynthetic rate
- A sat
saturating photosynthesis
- c a
atmospheric CO2 concentration
- CA1
carbonic anhydrase 1
- c c
CO2 concentration at the site of carboxylation
- c i
intercellular CO2 concentration
- c i*
photorespiratory compensation point
- E
whole-plant transpiration
- GAMM
generalized additive mixed modelling
- g m
mesophyll conductance of CO2
- g min
minimum conductance
- g s
stomatal conductance
- HH
high humidity
- J
rate of electron transport
- J max
maximum rate of electron transport
- LH
low humidity
- PAR
photosynthetically active radiation
- PIP
plasma membrane intrinsic protein
- R d
respiration in the light
- RWC
relative water content
- V cmax
maximum rate of carboxylation
- Vpd
vapour pressure deficit
- WT
wild type
- φ
quantum efficiency
Author contributions
DI, CRW, and TMR: designing the experiments; CRW, TMR, and JJZ: supervision; DI and SK: performing the experiments; CRW and TMR: technical assistance; DI: data analysis; DI: writing with contributions from all authors.
Data availability
The data supporting the findings of this study are available from the corresponding author, David Israel, upon request.
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Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Supplementary Materials
Data Availability Statement
The data supporting the findings of this study are available from the corresponding author, David Israel, upon request.