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1 Laboratory of Epithelial Cell
Biology, Aquaporins 1 (AQP1) and 2 (AQP2) were expressed in the yeast
secretory mutant sec6-4. The mutant
accumulates post-Golgi, plasma membrane-targeted vesicles and may be
used to produce large quantities of membrane proteins. AQP1 or AQP2
were inducibly expressed in yeast and were localized within isolated
sec6-4 vesicles by immunoblot analysis. Secretory vesicles containing AQP1 and AQP2 exhibited high
water permeabilities and low activation energies for water flow,
indicating expression of functional AQP1 and AQP2. AQP1 solubilized
from secretory vesicles was successfully reconstituted into
proteoliposomes, demonstrating the ability to use the yeast system to
express aquaporins for reconstitution studies. The AQP2-containing secretory vesicles showed no increased permeability toward formamide, urea, glycerol, or protons compared with control vesicles,
demonstrating that AQP2 is highly selective for water over these other
substances. We conclude that the expression of aquaporins in yeast
sec6 vesicles is a valid system to
further study mammalian water channel function.
activation energy; heterologous protein expression; proton
permeability; water and solute permeability
WATER CROSSES MEMBRANES by diffusion through either the
lipid bilayer or through specific water channels (aquaporins; reviewed in Refs. 3 and 52). Water permeability is ~20-fold greater when water
channels are expressed in oocytes or reconstituted (3, 52), and water
permeation occurs with an activation energy of 2-5 kcal/mol (25)
instead of the activation energy of 10-15 kcal/mol observed for
diffusion across a lipid bilayer. Six aquaporins (AQP0-AQP5) have been
cloned from mammals. AQP0 [major intrinsic protein (MIP)]
is located in lens fiber cells (40, 48). AQP1 is found in the renal
proximal tubule (9), red blood cells, and a variety of endothelia (30,
52). AQP2 mediates vasopressin-stimulated water flow across the apical
membrane of kidney collecting duct cells, whereas both AQP3 and AQP4
are constitutively expressed and allow water flow across the
basolateral membrane of these cells (18, 52). AQP5 is localized in
salivary and lacrimal glands, cornea, and lung (38). Although the
physiological significance of these proteins is not completely defined,
loss of function mutations in AQP2 result in severe nephrogenic
diabetes insipidus (7, 8), and mutations in AQP0 in mice lead to
cataract formation (42). However, extremely rare individuals with AQP1
mutations have been identified and lack a significant clinical
phenotype (37).
Aquaporins are members of the larger MIP family of proteins based on
sequence homology (33). Although >80 proteins have been cloned from
the MIP family, few have been biophysically characterized (3, 52), so
it is difficult to define the structure and function of the water pores
formed by the individual aquaporins.
Most studies of aquaporin function have involved expression in
Xenopus oocytes (7, 10, 12, 35, 36).
Reconstitutions of AQP1 protein into proteoliposomes have provided
direct measurements of water permeability (49, 50). Data from
reconstitution studies may be difficult to obtain due to lack of
purified protein, and it is not always clear that the functional
properties of the native protein are maintained during its
solubilization and insertion into the bilayer (48). Only AQP1 from red
blood cells (49, 50) and AQP0 from the bovine eye lens (31, 48) are
easily purified in sufficient quantities from tissues for
reconstitution and biophysical studies. Studies in oocytes are limited
by a lack of biophysical definition because the interior environment
cannot be modified and because endogenous channels may produce spurious activities. Oocytes have at times produced conflicting biophysical results, such as in the case of AQP3 (10, 17, 24), and, in some cases,
results in oocytes (26) have conflicted with those obtained from
reconstitution into planar lipid bilayers (13, 31). Thus an expression
system is needed in which unique aquaporin cDNAs may be expressed.
Vesicles containing the aquaporins from the expression system may then
be studied under conditions in which the composition of the solutions
on both sides of the channel can be controlled.
To this end, we now present the expression of AQP1 and AQP2 in the
well-characterized sec6-4 yeast
expression system to examine their biophysical properties. Aquaporins
were expressed in yeast, and secretory vesicles were isolated. The
temperature-sensitive sec6-4 mutant
accumulates plasma membrane-targeted vesicles upon shift to the
nonpermissive temperature (37°C) and has previously been used to
study other membrane proteins (19, 28, 39). Although a previously
published study showed functional expression of AQP1 in yeast secretory
vesicles, the water permeability increased only two- to fourfold (21),
indicating that the system would not be useful for detailed studies of
the biophysical properties of aquaporins. In the present study,
conditions for aquaporin expression were optimized so that water
permeabilities up to ~60-fold higher than control vesicles were
obtained. From secretory vesicles containing AQP1, successful
reconstitution into proteoliposomes was demonstrated. Moreover, the
selectivity properties of AQP2 were defined.
Materials. All reagents were of the
highest purity available. Common reagents were from Sigma (St. Louis,
MO), C. J. T. Baker (Phillipsburg, NJ), or Bio-Rad (Hercules, CA).
5,6-Carboxyfluorescein (CF) was from Molecular Probes (Eugene, OR).
Affinity-purified antibodies to AQP1 and AQP2 were generated and
characterized as described previously (18, 50).
Yeast strains and plasmid
construction. SY1 (34) was the yeast strain used for
all work. cDNAs encoding the aquaporin proteins were cloned into the
yeast expression vector pYES2 (Invitrogen, San Diego, CA) by standard
techniques (41). The human AQP1 cDNA was cloned into the
Hind III and
BamH I sites of the pYES2 vector, the
human AQP2 cDNA (provided by Peter Deen and Carel van Os, University of
Nijmegen, The Netherlands) was cloned into the
EcoR I site, and the orientation was
verified by digestion with Kpn I. Yeast was transformed by electroporation with a Bio-Rad gene pulser
with the following settings: 1.5 kV, 200 ohms, and 25 µF. Transformed
yeast was grown and maintained in defined media lacking uracil and
containing raffinose as a carbon source. Yeast was transferred to rich
yeast extract/peptone (YEP)-galactose medium [0.5%
yeast extract (wt/vol), 1.0% bactopeptone (wt/vol), and 2.0%
galactose (wt/vol)] at 25°C for 2-4 h to initiate
protein expression and then was switched to 37°C overnight to force
accumulation of the secretory vesicles. Control studies were performed
using vesicles prepared from the background strain or from yeast
transformed with the pYES2 vector lacking any aquaporin insert. Both
sets of control vesicles gave identical results in permeability
studies.
Immunoblotting. Samples were incubated
at 60-80°C for 5 min and then separated by sodium dodecyl
sulfate (SDS)-polyacrylamide gel electrophoresis using 4-20%
continuous-gradient tris(hydroxymethyl)aminomethane (Tris)-Cl-glycine
Ready Gels or 12% SDS-polyacrylamide slabs (20) and transferred to
nitrocellulose (Bio-Rad). The blots were blocked with blot buffer
consisting of 1% powdered milk and 3% Tween 20 in phosphate-buffered
saline (pH 7.25). The blots were incubated with 1:2,000
affinity-purified, anti-AQP1 (43) or anti-AQP2 (29) antibody overnight
at 4°C and then visualized by the enhanced chemiluminescence method
(NEN or Amersham).
Vesicle preparation. Vesicles were
prepared as described previously (6, 28) but modified for stopped-flow
studies. Briefly, growth conditions were modified as described above,
the yeast was treated with 10 mM dithiothreitol (DTT) in 100 mM
Tris-Cl, pH 9.4, and spheroplasts were generated by digesting the cell wall with bacterially expressed recombinant lyticase. The plasma membrane was cross-linked with concanavalin A to increase its density
above that of the secretory vesicles. Spheroplasts were lysed in lysis
buffer (0.8 M sorbitol, 10 mM triethanolamine, 1 mM EDTA, pH 7.2)
containing CF (7.5 mg/ml), and unlysed cells and
concanavalin-cross-linked plasma membranes were pelleted at 11,000 revolutions/min (20,000 g) in a
Sorvall GSA rotor for 10 min at 4°C. Vesicles were pelleted from
the supernatant and washed to remove extravesicular CF by
centrifugation at 29,000 revolutions/min (144,000 g) in a Sorvall TH-641
swinging-bucket rotor for 1 h at 4°C. The surface area-to-volume
ratio was calculated as previously described (51).
Reconstitution. Secretory vesicles
were solubilized in 1.5% (wt/vol) octyl glucoside, 50 mM
3-(N-morpholino)propanesulfonic acid (MOPS), pH 7.5, 20%
glycerol, 1 mM DTT, 0.4% E. coli
phospholipids, and 0.5 mM phenylmethylsulfonyl fluoride (PMSF) for 20 min on ice and centrifuged at 100,000 g for 1 h at 4°C. The supernatant was used for reconstitution into proteoliposomes (4). Octyl glucoside
extract of secretory vesicles (5 mg/ml) was solubilized in 5 mg of
bath-sonicated E. coli phospholipid
containing 1.5% (wt/vol) octyl glucoside. This mixture was incubated
on ice for 20 min. Proteoliposomes were formed by rapid dilution of the
mixture into 25 ml of 150 mM N-methyl
glucamine, 50 mM MOPS, pH 7.5, 15 mM CF, 1 mM DTT, and 0.5 mM PMSF
(buffer A) at room temperature. Proteoliposomes were pelleted by centrifugation for 1 h at 100,000 g at 4°C. The pellet was
resuspended in 300 µl of buffer A
lacking CF as previously described (50). Protein concentrations were measured as described previously (4).
Water, solute, and proton transport.
Water transport was measured by stopped-flow fluorescence quenching as
previously described (22, 49, 50). Briefly, the integrity of the yeast
vesicles that were loaded with CF during lysis was verified by first
measuring their fluorescence intensity on an SLM-AMINCO SPF-500C
spectrofluorimeter connected to an NEC/MultiSync 2A computer.
Extravesicular CF was then quenched by addition of an anti-CF antibody,
and vesicles were shrunk by successive additions of a high-osmolal
solution using sucrose as the osmoticant. Vesicle shrinkage correlated linearly with the osmolality increase over the range of
values tested. Yeast vesicles were loaded onto an Applied Photophysics SF.7mv stopped-flow apparatus with a measured dead time of 0.7 ms. The
vesicles were subjected to an abrupt doubling of the osmolality, causing the vesicles to shrink and the CF to self-quench. Water permeabilities were calculated using MATHCAD software as previously described (22, 49, 50). For solute and proton permeabilities, the
vesicles were rapidly subjected to a solute gradient (700 mM inside,
300 mM outside) or pH gradient (pH 6.8 inside, pH 5.0 outside). All
experiments were designed to force a decrease in fluorescence, either
due to shrinkage and CF self-quenching or due to the pH sensitivity of
CF fluorescence. The decrease in fluorescence was measured and
correlated to the decrease in volume. Fluorescence was measured with
incident light of 490 ± 1 nm and a cut-on filter that measures
light emitted at wavelengths >510 nm.
Whether from control, AQP1-, or AQP2-expressing yeast, isolated
secretory vesicles behaved as a single population with a median diameter of 188 ± 13 nm. This value did not change appreciably for
the different vesicle preparations and was used for all permeability calculations. This is somewhat larger than the 100-nm yeast secretory vesicle size reported from electron microscopy measurements within whole yeast cells (16) and may reflect changes in vesicle size during
preparation.
As shown in Fig. 1, AQP1 and AQP2 vesicles,
but not control vesicles, contained detectable aquaporin proteins by
immunoblotting. Each lane contains total vesicle protein either from an
aquaporin-expressing strain or from a control strain transformed with
the pYES vector lacking aquaporin. To determine if the yeast expression
system produced functional protein, both AQP1-containing and
AQP2-containing sec vesicles were
assayed for osmotic water permeability
(Pf). As shown
in Fig. 2,
Pf increased
dramatically in AQP1-containing vesicles compared with control. Note
the difference in time scale along the abscissa. The
Pf for the
control vesicles was 0.0022 ± 0.0004 (SD) cm/s
(n = 5). The original
Pf value obtained
for AQP1-containing vesicles was 0.030 ± 0.010 cm/s
(n = 3). Expression conditions were
optimized, and water permeability measurements reached values as high
as 0.087 cm/s. Figure 2 shows the rate of vesicle shrinkage after
optimization for expression.
![]()
ABSTRACT
Top
Abstract
Introduction
Materials & Methods
Results
Discussion
References
![]()
INTRODUCTION
Top
Abstract
Introduction
Materials & Methods
Results
Discussion
References
![]()
MATERIALS AND METHODS
Top
Abstract
Introduction
Materials & Methods
Results
Discussion
References
![]()
RESULTS
Top
Abstract
Introduction
Materials & Methods
Results
Discussion
References

View larger version (44K):
[in a new window]
Fig. 1.
Immunoblots showing expression of aquaporin 1 (AQP1;
A) and aquaporin 2 (AQP2;
B) in yeast expressing the aquaporin
or control yeast. Fifty micrograms of protein were applied to each lane
and probed with specific antisera directed against AQP1 or AQP2, and
binding of the antisera was detected by incubation with goat
anti-rabbit horseradish peroxidase-conjugated antibody. Results are
representative of 2-3 individual determinations.

View larger version (15K):
[in a new window]
Fig. 2.
Stopped-flow measurement of water flow in secretory vesicles from yeast
expressing (A) or lacking
(B) AQP1 at 16°C. Averaged
curves and fitted single exponentials are shown.
When AQP1 was solubilized from the yeast secretory vesicles and reconstituted into artificial proteoliposomes (49, 50), the water permeability increased proportionately with the amount of AQP1 protein (Fig. 3). Control proteoliposomes contained protein from yeast secretory vesicles lacking AQP1 at a protein-to-lipid ratio of 1:1, whereas the other graphs show protein additions from AQP1-containing yeast. Protein from AQP1-expressing yeast was reconstituted at total protein-to-lipid ratios of 1:1, 1:2, and 1:5, with increasing amounts of protein leading to increased rates of water flux. Thus the fast shrinkage rate of the AQP1-containing proteoliposomes was due specifically to the AQP1 protein. Further evidence for this is shown in Fig. 4, which shows the differences in activation energy between AQP1-containing and control proteoliposomes. The proteoliposomes had activation energies of 3.7 kcal/mol (AQP1 proteoliposomes, protein/lipid = 1:1) and 12.1 kcal/mol (control proteoliposomes containing protein from SY1 yeast, protein/lipid = 1:1). These results demonstrate that the yeast system can serve as a source of aquaporin protein for reconstitution studies.
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The human AQP2 cDNA was also expressed in yeast sec vesicles. Sec vesicles isolated from this AQP2-containing strain showed a dramatic increase in water permeability (Fig. 5). Vesicle shrinkage was complete in ~4 ms after rapid exposure to hypertonic solution. The rate of water flow in AQP2-containing vesicles may have been faster than that of AQP1-containing vesicles because of a higher protein expression level. The Pf for the AQP2-containing vesicles was 0.14 ± 0.03 cm/s (n = 4; P < 0.001). The activation energy for water transport in the AQP2-containing vesicles was 4.0 ± 0.5 kcal/mol compared with 13.2 ± 1.2 kcal/mol for control secretory vesicles (Fig. 6). The activation energy for AQP2-containing vesicles was measured over a smaller temperature range because the entrapped CF leaked, possibly due to lysis, from the vesicles at higher temperatures.
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AQP1 has been shown to be highly selective for water over other substances, including urea, glycerol, and protons (49, 50). Some aquaporins, such as AQP3 and the glycerol facilitator of yeast, are known to mediate fluxes of small nonelectrolytes, such as glycerol and urea, in addition to water (10, 17). Some evidence has been presented to suggest that AQP1 and AQP2 can also mediate such fluxes when expressed in oocytes (1, 2). To determine the selectivity for water of AQP2, the permeabilities to formamide, urea, and glycerol were measured (Figs. 7-9). In all three cases, water fluxes were measured in the vesicles used for solute flux studies (see Figs. 7-9, insets). Despite the 64-fold increase in water permeability mediated by expression of AQP2, there were no detectable differences in flux rates of formamide, urea, or glycerol in control vesicles or vesicles containing AQP2. Solute permeability values for all preparations are summarized in Table 1 in which means ± SE are reported for three to five separate secretory vesicle preparations; only water permeability was significantly increased (P < 0.001) in vesicles with AQP2.
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The selectivity of AQP2 for water over protons was also determined because evidence from Ussing chamber studies as well as measurements of proton flux across endosomes had indicated that a closely related aquaporin, the aquaporin responsible for vasopressin-mediated water flow in toad bladder, conducts protons (14, 15). Figure 10 shows the rate of change of internal pH when sec vesicles at pH 6.8 were rapidly subjected to an external pH of 5.0. The change in fluorescence and change in pH are linearly related over this range. Despite the 64-fold increase in Pf for AQP2-containing vesicles over control vesicles, the rate of proton flux was unaltered, demonstrating its high degree of selectivity for water over protons.
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DISCUSSION |
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Although numerous animal and plant aquaporins have been cloned and identified, there is still little understanding of how these unique proteins form water channels (3, 52). There are several aspects of aquaporin function which, if correlated with primary structure, would provide insights into how the protein functions. These include the unit conductance, the selectivity for water over other substances, the ratio of osmotic to diffusive water permeability (which defines the length of the single-file water pore), and the ability of different solutes to penetrate partially into the water pore.
The presently known aquaporins have been expressed in Xenopus oocytes, from which some information about their function has been obtained. However, oocytes do not permit detailed biophysical definition of aquaporin function because the solution on the cytoplasmic side of the aquaporin cannot be controlled. In addition, it is possible that oocytes alter aquaporin expression at the membrane or function in a manner distinct from regulation in vivo (7).
Reconstitution of aquaporins into proteoliposomes allows detailed biophysical definition of aquaporin function. However, large quantities of protein must be isolated, thereby reducing the numbers of aquaporins that can be studied. Furthermore, mutant forms of the proteins are difficult to obtain. In addition, solubilization and reconstitution of aquaporins may alter their function. This appears to occur with MIP (AQP0), which, when reconstituted into planar bilayers, creates a high-conductance, low-selectivity ion channel (48). It has been reported that MIP reconstituted into proteoliposomes will permit large molecules, such as glucose, to permeate the vesicles (13, 31). By contrast, when MIP is expressed in oocytes, it forms a high-selectivity, low-conductance water channel (26). Finally, reconstitution results in a random orientation of the aquaporin in the proteoliposome, which makes it more difficult to study the effects of phosphorylation on channel function (23, 47).
The present study seeks to develop a method for studying aquaporin function that combines the advantages of oocytes with those of reconstitution but avoids many of the disadvantages. First, because the starting material is a cDNA, it is theoretically possible to express any native or mutant aquaporin in the yeast system. Second, because the yeast inserts the protein into the secretory vesicle as it is being made (6), in a process similar to the process that occurs in the native tissue, there is little chance that aquaporin function will be altered during expression. Third, the solutions inside and outside of the vesicles can be modified systematically, permitting detailed definition of channel function. Fourth, the channels are likely to be inserted into the vesicles in a cytoplasmic-side out configuration, permitting studies of the effects of phosphorylation on channel function. Finally, as demonstrated here, the yeast system may serve as a starting point for purification and reconstitution experiments.
The present study demonstrates the utility of this approach for AQP1 and AQP2 in that the vesicles containing the channel exhibited markedly increased water permeability with a low activation energy. In this respect, these studies agree with those published by Laize et al. (21), in which successful expression of AQP1 in yeast secretory vesicles was demonstrated. In their studies, expression of AQP1 led to a threefold increase in secretory vesicle water permeability. Although this was sufficient to demonstrate functional AQP1 expression, the modest increase in water permeability obtained would not permit a biophysical definition of aquaporin function. With optimization of induction protocols, we have increased water flow by 14- to 40-fold in the case of AQP1 and by ~64-fold in the case of AQP2. These dramatic increases in water permeability will permit biophysical definition of aquaporin function.
Solubilization of the protein extracted from yeast secretory vesicles followed by its reconstitution into proteoliposomes gave results identical to those published previously, establishing the yeast secretory vesicle system as a viable source of aquaporin protein for reconstitution (49, 50). Because AQP1 has been prepared for two-dimensional crystallization studies in proteoliposomes, the yeast expression system opens the way for structural studies of aquaporins that cannot be isolated in quantity directly from their native tissues (45, 46).
AQP2 expression in secretory vesicles also led to dramatic increases in water permeability, again at low activation energy. The vesicles were then used to define the selectivity of this channel for water over other substances. Several members of the aquaporin family, including AQP3, NOD26, and glpF, exhibit high permeabilities to glycerol and urea and appear to exhibit variable permeabilities to water (10, 17, 24, 27, 32). Studies of the selectivity of AQP2 in oocytes have given conflicting results, with most authors reporting little to no solute permeability and one group reporting appreciable permeability to glycerol and urea (1, 12). In the present studies, we were unable to demonstrate any ability of AQP2 to increase the permeability of secretory vesicles to urea, formamide, or glycerol despite a >60-fold increase in water permeability. Water, formamide, urea, and glycerol represent a range of radii for solutes, with van der Waals volumes of 10.6, 24.8, 32.8, and 51.4 cm3/mol (5, 44), respectively. If the solutes are assumed to have van der Waals volumes that occupy spheres, this suggests that the pore radius is >1.6 Å but <2.1 Å. The results of the present study indicate that AQP2, like AQP1, has a narrow pore that is highly selective for water.
In previous studies, we have shown that AQP1 is highly selective for water over protons (49, 50). However, vasopressin stimulation of toad urinary bladder granular cells causes a concurrent increase in water and proton permeabilities (14). Moreover, gramicidin forms single-file water channels that functionally resemble aquaporins and conduct protons rapidly (11). Because AQP2 is functionally similar to the aquaporin found in toad bladder, proton flux across AQP2 could increase proton permeability of the collecting duct whenever vasopressin-mediated water reabsorption occurs (14, 15). Our results provide the most direct evidence to date that AQP2 does not conduct protons. This is physiologically consistent, since vasopressinstimulated concentration of the urine should not simultaneously require deacidification of the urine via proton leak through collecting duct principal cells. The results also suggest that the water pore through AQP1 and AQP2 has a barrier to the flow of charged species, such as protons (50).
AQP1 and AQP2 appear to function similarly as high-conductance, high-selectivity aquaporins, which likely feature a narrow, water-selective pore (49, 50). By contrast, other aquaporins, such as AQP3 and glpF, which conduct glycerol and urea, exhibit low water permeability in some cases (24, 27) but high water permeability in others (10, 17). Finally, there may be an intermediate class of aquaporins, such as NOD26 and AQP0, which exhibit moderate water conductance and may, under some circumstances, mediate fluxes of solutes (13, 26, 31, 32, 48, and R. Rivers, D. M. Roberts, and M. L. Zeidel; unpublished observations). Further studies of the biophysical properties of these aquaporins using the yeast expression system will permit clarification of the relationship between aquaporin primary structure and function.
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ACKNOWLEDGEMENTS |
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We thank Mark Knepper for the use of anti-aquaporin 1 antibody.
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FOOTNOTES |
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These studies were supported by National Institutes of Health Grants DK-43955 (to M. L. Zeidel), HL-33991, HL-48268, and GY-11239 (to P. Agre). J. L. Brodsky was supported by National Science Foundation Grant MCB9506002 and American Cancer Society Grant JFRA602. L. A. Coury was supported by an National Research Service Award from the National Institutes of Health. J. C. Mathai was supported by a fellowship from the American Heart Association, Maryland affiliate (1996-1997). DNA and protein sequence analysis was supported by Pittsburgh Supercomputing Center Grant MCB960003P.
Address for reprint requests: M. L. Zeidel, Laboratory of Epithelial Cell Biology, Renal Electrolyte Division, Department of Medicine, University of Pittsburgh Medical Center, 3550 Terrace St., Pittsburgh, PA 15213-1500.
Received 16 May 1997; accepted in final form 5 September 1997.
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