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J Biol Chem, Vol. 273, Issue 16, 9369-9372, April 17, 1998
COMMUNICATION
Urea Transporter UT3 Functions as an Efficient Water Channel
DIRECT EVIDENCE FOR A COMMON WATER/UREA PATHWAY*
Baoxue
Yang and
A. S.
Verkman
From the Departments of Medicine and Physiology, Cardiovascular
Research Institute, University of California, San
Francisco, California 94143-0521
 |
ABSTRACT |
A family of molecular urea transporters (UTs) has
been identified whose members appear to have an exceptionally high
transport turnover rate. To test the hypothesis that urea transport
involves passage through an aqueous channel, osmotic water permeability was measured in Xenopus oocytes expressing UTs. The UT3
class of urea transporters functioned as efficient water channels.
Quantitative measurement of single channel water permeability
(pf) using epitope-tagged rat UTs gave
pf (in cm3/s × 10 14) of 0.14 ± 0.11 (UT2) and 1.4 ± 0.2 (UT3), compared with 6.0 and 2.3 for water channels AQP1 and AQP3,
respectively. Relative single channel urea permeabilities
(purea) were 1.0 (UT2), 0.44 (UT3),
and 0.0 (AQP1). UT3-mediated water and urea transport were weakly
temperature-dependent (activation energy <4 kcal/mol), inhibited > 75% by the urea transport inhibitor
1,3-dimethylthiourea, but not inhibited by the water transport
inhibitor HgCl2. To test for a common water/urea pore, the
urea reflection coefficient ( urea) was measured by
independent induced osmosis and solvent drag
methods. In UT3-expressing oocytes, the time course of oocyte volume in
response to different urea gradients (induced osmosis) gave
urea ~0.3 for the UT3 pathway, in agreement with
urea determined by the increase in uptake of
[14C]urea during osmotic gradient-induced oocyte swelling
(solvent drag). In oocytes of comparable water and urea permeability
coexpressing AQP1 (permeable to water, not urea) and UT2 (permeable to
urea, not water), urea = 1. These results indicate that
UT3 functions as a urea/water channel utilizing a common aqueous
pathway. The water transporting function and low urea reflection
coefficient of UT3 in vasa recta may be important for the formation of
a concentrated urine by countercurrent exchange in the kidney.
 |
INTRODUCTION |
Several related urea transporters
(UTs)1 have been cloned
recently. The UT2 transporter (rat form referred to as rUT2, Ref. 1)
was first identified in rabbit by expression cloning (2). The UT2
cDNA encodes a 397-amino acid glycoprotein that is expressed in the
medullary portion of descending limbs of Henle in kidney (3, 4). UT1 is
larger protein (929 amino acids) that contains the UT2 sequence at its
C terminus fused to a 67% identical amino acid sequence at its N
terminus (5). UT1 functions a cAMP-regulated urea transporter that is
expressed at the apical membrane of inner medullary collecting duct
cells. UT1 and UT2 are thought to be derived from a single gene by
alternative splicing. A 391-amino acid urea transporter expressed in
erythrocytes was initially cloned from human bone marrow (HUT11, Ref.
6) and subsequently from rat kidney (named UT3, Ref. 7). Rat UT3 has
62% amino acid identity to UT2 and is expressed strongly in kidney in
descending vasa recta in the inner stripe of outer medulla, as well as
in testis and brain (7, 8). It is thought that these urea transporters have an important role in the urinary concentrating mechanism to
establish a hypertonic renal medullary interstitium (9).
UT3 was initially recognized as the Kidd antigen (Jk) in erythrocytes
(10-12). Humans lacking the Kidd antigen (Jk / ) have low
erythrocyte urea permeability. These individuals are phenotypically grossly normal, but have a defect in their ability to produce a
maximally concentrated urine (13). From the number of Kidd antigen
proteins per erythrocyte and the erythrocyte urea permeability, it was
estimated that the UT3 turnover rate is 2-15 × 106
urea molecules/s (9, 14). This turnover rate is substantially higher
than that of usual solute carriers, suggesting a channel mechanism for
urea transport. Additional functional data involving urea concentration
dependence and trans-inhibition (15) support a channel-type
mechanism.
The purpose of this study was to test whether urea transporters of the
UT3-type (and possibly the UT2-type) transport urea by a channel
mechanism involving urea passage through an aqueous pore. It was found
that UT3 functions as an efficient water channel with water transport
rates comparable with those of aquaporin-type water channels. Water
movement through UT3 was weakly temperature-dependent and
inhibited by urea transport inhibitors but not by water transport inhibitors. A key finding was that the reflection coefficient for urea
was remarkably less than unity, providing strong evidence for a common
water and urea pathway through UT3. These results have important
implications regarding urea transporter structure and transporting
mechanism and suggest a novel role for UT3 in the urinary concentrating
mechanism as a facilitator of urea solvent drag in renal vasa
recta.
 |
MATERIALS AND METHODS |
cDNA Constructs--
Full-length cDNAs encoding rat AQP1
(GenBankTM accession number L07268), AQP3 (GenBankTM accession number
D17695), UT2 (GenBankTM accession number U09957), and UT3 (GenBankTM
accession number U81518) were polymerase chain reaction-amplified using rat kidney cDNA as template and primers (BamHI or
BglII and XbaI engineered restriction
sites underlined): AQP1 sense,
5'-CGGGATCCATGGCCAGCGAGTTAAAGAAGA-3'; AQP1-antisense,
5'-GCTCTAGATTTGGGCTTCATCTCCACCCTG-3'; AQP3 sense, 5'-CGGGATCCATGAACCGTTGCGGGGAGATGC-3'; AQP3-antisense,
5'-GCTCTAGAGATCTGCTCCTTGTGCTTCATG-3'; UT2 sense,
5'-CGAGATCTATGGAGGAGAGCTCTGAGATAA-3'; UT2 antisense, 5'-GCTCTAGAGGAGACGTCGTAGGCCTGGTAC-3'; UT3 sense,
5'-CGAGATCTATGGAAGATATTCCCACTATGG-3'; UT3 antisense,
5'-GCTCTAGATTACAGCGGGCGGTCGACCGCGCTT-3'.
Amplified DNA fragments was confirmed by sequence analysis and
subcloned into oocyte expression plasmid (pSP64T-N-c-Myc) (16). The
constructs encoded fusion proteins consisting of each full-length aquaporin or urea transporter fused downstream and in-frame from a
10-amino acid human c-Myc epitope (EQKLISEEDL).
RNA Transcription and Oocyte Expression--
Complementary RNA
was transcribed in vitro using SP6 polymerase (Life
Technologies, Inc.) and 5 µg of plasmid DNA in a 100-µl volume at
37 °C for 1 h in the presence of diguanosine triphosphate (1 A250 unit, Amersham Pharmacia Biotech). Plasmid
DNA was digested with RNase-free DNase (Invitrogen), extracted with
phenol-chloroform, precipitated twice in ethanol, and suspended in
distilled water. Stage V and VI oocytes from Xenopus laevis
were isolated and defolliculated with collagenase in Barth's buffer
(200 mosM). Oocytes were microinjected with 50-nl samples
of specified cRNAs (0-200 ng/µl) and incubated at 18 °C for 24 or
48 h.
Transport Measurements--
Osmotic water permeability
(Pf) was measured from the time course of oocyte
swelling at 10 °C in response to a 2- or 5-fold dilution of the
extracellular Barth's buffer with distilled water. Oocyte
Pf was calculated from the initial rate of
swelling as described previously (17). In some experiments, oocytes
were incubated with 1,3-dimethylthiourea or phloretin for 30 min or HgCl2 for 5 min at 20 °C prior to and during
permeability measurements. To determine urea reflection coefficient,
oocytes were partially swelled in 0.2 ml of 1:1 diluted Barth's (100 mosM) for 30 s, and then 0.2 ml of water containing
different concentrations of urea (0-1600 mM) was added
(see below). To measure urea uptake, groups of 10 oocytes were
incubated in 0.2 ml of Barth's buffer containing 3 µCi of
[14C]urea (nonradioactive urea added to give 1 mM final [urea]) at 23 °C. After 0 or 90 s, or
2 h (to determine equilibrium incorporation), oocytes were washed
four times rapidly in ice-cold Barth's buffer containing 1 mM unlabeled urea, and individual oocytes were dissolved in
5% SDS for scintillation counting. Data were expressed as percent 90-s
[14C]urea uptake, where 100% refers to 2-h uptake. In
some experiments, the incubation solution containing
[14C]urea was made hypoosmolar (40 or 100 mosM) by dilution with distilled water or hyperosmolar (400 mosM) by addition of sucrose.
Computations--
Transport of water and urea across the oocyte
plasma membrane is described quantitatively by the Kedem-Katchalsky
equations of coupled water and solute transport (18) adapted for
channel-expressing oocytes,
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(Eq. 1)
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(Eq. 2)
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where Jv is the volume flux
(cm3/s) and Jurea the urea flux
(mol/s) (inward flux defined as positive), urea the urea
reflection coefficient, S the oocyte surface area (0.045 cm2), vw the partial molar volume of
water (18 cm3/mol), and Pf and
Purea the water and urea permeability
coefficients (cm/s, "lipid" and "channel" superscripts refer to
transport through lipid versus expressed channel).
Jvchannel in Equation 2 refers to
the second term in Equation 1. Concentration gradients of impermeant
solutes ( Ci) and urea ( [urea]) are
defined as outside-inside differences, and <urea> is taken here as
the outside urea concentration. Equations 1 and 2 were numerically integrated for determination of urea.
Pflipid and
Pfchannel were determined from
water permeability measurements without and with cRNA
expression, respectively;
Purealipid and
Pureachannel were determined
similarly from [14C]urea uptake measurements.
Immunoprecipitation--
Metabolic labeling was performed by
incubating groups of 10 oocytes for 24 h at 18 °C in 100 µl
of Barth's buffer containing 50 µCi of [35S]methionine
(Amersham Pharmacia Biotech). Oocytes were washed and plasma membrane
complexes were peeled and collected. As described in detail previously
(16), membranes were homogenized, solubilized in 100 mM
-octyl glucoside, and immunoprecipitated using a mouse monoclonal
anti-c-Myc antibody and protein A-Sepharose CL-4B beads. Immunoprecipitated proteins were released from the beads in SDS loading
buffer, resolved on 12% SDS-polyacrylamide gel electrophoresis, soaked
in 15% (w/v) 2,5-diphenyloxazole in Me2SO, and exposed to
hyperfilm (Amersham) at 70 °C for 5-14 days.
 |
RESULTS AND DISCUSSION |
Fig. 1A shows the time
course of osmotically induced swelling in control (water-injected)
oocytes, oocytes expressing aquaporin water channels AQP1 and AQP3, and
oocytes expressing urea transporters UT2 and UT3. Averaged water
permeability coefficients (Pf) are summarized in
Fig. 1B. The large increase in Pf in
oocytes expressing UT3 was an unexpected finding. Fig. 1C
shows the 90-s uptake of [14C]urea for the same groups of
oocytes. Urea permeability in oocytes expressing UT2 or UT3 was
>12-fold increased over that in control and AQP1-expressing
oocytes.

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Fig. 1.
Water and urea permeability in oocytes
expressing aquaporins and urea transporters. A, time course
of oocyte swelling at 10 °C in response to a 5-fold dilution of
extracellular Barth's buffer with distilled water. Oocytes were
injected with 50 nl of water (as control) or cRNAs (5 ng) encoding
AQP1, AQP3, UT2, or UT3. B, averaged water permeability
coefficients (Pf). Data are mean ± S.E.
for measurements on 9-12 oocytes from three separate sets of
experiments. C, percent 90-s uptake of
[14C]urea (expressed as percentage of uptake at 2 h,
mean ± S.E.) at 23 °C in oocytes from the same batches as used
in B. D, autoradiogram of proteins from oocyte plasma
membranes that were immunoprecipitated by c-Myc antibody.
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To determine the intrinsic (per channel) water and urea permeabilities
of the expressed AQPs and UTs, permeability values from Fig. 1,
B and C, were normalized to account for
differences in transporter expression at the plasma membrane. Oocytes
expressing c-Myc epitope-tagged AQPs and UTs were metabolically labeled
with [35S]methionine, and c-Myc-tagged proteins were
immunoprecipitated from microdissected oocyte plasma membranes. Fig.
1D shows a representative autoradiogram of
immunoprecipitated proteins. The protein sizes are in agreement with
cDNA sequence and published immunoblot data. Absolute single
channel water permeability coefficients
(pf) were computed as described
previously (16) using a reference pf of 6 × 10 14 cm3/s for AQP1.
Pf (in cm3/s × 10 14, S.E., n = 3) were: 0.14 ± 0.11 (UT2), 1.4 ± 0.2 (UT3), and 2.3 ± 0.1 AQP3. Single
channel urea permeabilities (purea),
relative to that of UT2 (defined as 1.0) were: 0.44 (UT3), 0.0 (AQP1)
and 0.02 (AQP3).
The significant intrinsic water permeability of UT3 suggests the
existence of a continuous aqueous channel through the UT3 protein that
passes both water and urea. Studies of temperature dependence,
inhibitor specificity, and urea reflection coefficient were done to
test this possibility. Fig. 2A
shows a weak temperature dependence for UT3-mediated transport of both
water and urea. The low Arrhenius activation energy (<4 kcal/mol) is
consistent with an aqueous pore pathway and is in agreement with the
low activation energies found for several of the aquaporin-type water channels. Fig. 2B indicates that UT3-mediated water and urea
transport were each strongly inhibited by the urea analog
1,3-dimethylthiourea and by phloretin. Neither water nor urea transport
were inhibited by HgCl2, a potent inhibitor of most
aquaporin-type water channels. HgCl2, but not the urea
transport inhibitors, strongly inhibited water permeability in oocytes
expressing AQP1 (Fig. 2C). Together these results support a
common aqueous route for water and urea transport through UT3.

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Fig. 2.
Characterization of water and urea transport
of UT3. A, temperature dependence of water and urea
permeability of control and UT3-expressing oocytes. B,
inhibition of water and urea transport in UT3-expressing oocytes.
Oocytes were incubated with 1,3-dimethylthiourea (170 mM),
phloretin (0.7 mM), or HgCl2 (0.3 mM) before and during permeability measurements as
described under "Materials and Methods." C, inhibition
of water permeability in AQP1-expressing oocytes.
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The most direct evidence for a common water/solute pathway is the
finding of a low solute reflection coefficient (19, 20). Reflection
coefficient measurements have in general been challenging because of
the tight coupling between volume and solute transport as described by
Equations 1 and 2. Of note, different labs have reported substantially
different reflection coefficients for urea transport across
erythrocytes (21, 22) and NaCl transport across proximal tubule
(23-25). Our strategy to determine the urea reflection coefficient
( urea) in oocytes involved independent measurements of
induced osmosis and solvent drag, and
quantitative comparison of experimental results with numerical solution
of the Kedem-Katchalsky equations.
In the induced osmosis method, oocytes were briefly swelled
in 100 mM Barth's buffer (because oocytes do not shrink
well below their normal volume, Ref. 26) and then the external solution was switched to 50 mM Barth's buffer containing different
concentrations of urea. As seen in Fig.
3A (top), oocytes
expressing UT3 initially swelled for external [urea] of 200 and 400 mM and shrunk for [urea] of 600 and 800 mM,
suggesting urea 1. The same measurements were
simulated numerically using Equations 1 and 2 for different values of
urea (Fig. 3B). There was good agreement
between the simulated and experimental data set for urea
~0.3.

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Fig. 3.
Determination of urea reflection coefficient
of the UT3 pathway. A: top, oocytes expressing UT3 were
immersed in 0.2 ml of 1:1 diluted Barth's buffer (100 mosM) for 30 s to produce swelling (initial upward
slope). Where indicated, 0.2 ml of urea in distilled water was added to
give the indicated final urea concentrations (one set of experiments
typical of three); bottom, same protocol except that oocytes
coexpressed AQP1 and UT2 (1 ng of AQP1 cRNA + 4 ng of UT2 cRNA).
B, predicted time course of oocyte volume (computed from
Equations 1 and 2) for urea of 0.3 (top) and
1.0 (bottom). Parameters:
Pflipid = 0.001 cm/s,
Pfchannel = 0.006 cm/s,
Purealipid = 10 5
cm/s, Pureachannel = 10 4 cm/s. C, ninety second uptake of
[14C]urea in UT3-expressing oocytes in solutions of
indicated osmolalities (8-10 oocytes in two separate sets of
experiments). Values were corrected (maximum 5% correction) for
volume-dependent differences in oocyte surface measured in
oocytes from A (bottom) coexpressing AQP1 and
UT2. Shown also are predictions for relative 90-s
[14C]urea uptake computed from Equations 1 and 2 for the
same parameters used in B, for urea = 0.3 versus 1.0.
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An important control study was done to validate the above approach for
determination of urea and to show that the low
urea is not a consequence of apparent solvent/solute
coupling ("pseudo-solvent drag") due to unstirred layers. An
identical set of measurements (as in Fig. 3A, top) was done
in oocytes coexpressing AQP1, which is permeable to water but not urea,
and UT2, which is permeable to urea and not water. The amounts of
injected cRNAs encoding AQP1 and UT2 were adjusted to give oocyte water
and urea permeabilities comparable with those for UT3-expressing
oocytes. Fig. 3A (bottom) shows little initial
oocyte swelling or shrinking for external [urea] ~200
mM, suggesting that urea ~1. This result
was confirmed by the simulated curves in Fig. 3B
(bottom).
As an independent method to measure urea utilizing
solvent drag, the 90-s uptake of [14C]urea
into oocytes was measured for different external solution osmolalities.
For urea less than 1, the osmotic water influx induced
by a low external osmolality would result in increased [14C]urea uptake (compared with no osmotic gradient)
because of additive urea diffusion and solvent drag mechanisms
(Equation 2). Fig. 3C shows that [14C]urea
uptake was significantly enhanced by hypoosmolar external solutions and
depressed by a hyperosmolar solution. The model simulations for
urea = 0.3 determined above were in reasonable agreement
with the [14C]urea uptake data.
Our results provide strong evidence that the UT3 protein is associated
with an aqueous channel that transports water and urea in a coupled
manner. The high UT3-mediated urea turnover and the trans-stimulation
data cited in the Introduction are explainable by a common water/urea
channel. Although electron crystallography data suggest the location of
a putative aqueous pore through aquaporin-type water channels (27, 28),
there is no structural information about the UT proteins to suggest the
existence or location of an aqueous channel. Of note, the UT and AQP
proteins share no homology. Structure and mutagenesis studies are
needed to resolve the mechanism of UT3-mediated water and urea
transport.
Although not directly addressed in this study, we speculate about the
physiological implications of a common water/urea channel in UT3. UT3
is expressed in descending vasa recta in kidney (7, 8), where it
confers high transendothelial urea permeability (29). The
countercurrent exchange mechanism in the renal medulla requires the
delivery of large quantities of urea and water from the vasa recta to
the inner medullary interstitium (30-32). The UT3-mediated solvent
drag of urea could provide a simple and elegant solution to the problem
of insuring an adequate rate of urea exit from vasa recta to balance
osmotically driven water exit.
 |
ACKNOWLEDGEMENT |
We thank Dr. N. Periasamy for help in software
development. The program for computation of coupled water/solute flux
in oocytes is available from the authors on request.
 |
FOOTNOTES |
*
This work was supported by National Institutes of Health
Grants DK35124, HL42368, and DK43840.The costs of publication of this
article were defrayed in part by the
payment of page charges. The article
must therefore be hereby marked
"advertisement" in accordance with 18 U.S.C. Section
1734 solely to indicate this fact.
To whom correspondence should be addressed: 1246 Health Sciences
East Tower, Cardiovascular Research Institute, University of
California, San Francisco, CA 94143-0521. Tel.: 415-476-8530; Fax:
415-665-3847; E-mail: verkman{at}itsa.ucsf.edu.
1
The abbreviation used is: UT(s), urea
transporter(s).
 |
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T. L. Pannabecker and W. H. Dantzler
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B. Yang and L. Bankir
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H. Inoue, S. D. Jackson, T. Vikulina, J. D. Klein, K. Tomita, and S. M. Bagnasco
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L. Bankir, K. Chen, and B. Yang
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W. Zhang and A. Edwards
Theoretical effects of UTB urea transporters in the renal medullary microcirculation
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T. L. Pallone, M. R. Turner, A. Edwards, and R. L. Jamison
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T. L. Pallone, Z. Zhang, and K. Rhinehart
Physiology of the renal medullary microcirculation
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K. Edashige, Y. Yamaji, F.W. Kleinhans, and M. Kasai
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J. M. Sands
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B. Yang and A. S. Verkman
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N. MacAulay, U. Gether, D. A Klaerke, and T. Zeuthen
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B. Yang, L. Bankir, A. Gillespie, C. J. Epstein, and A. S. Verkman
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C. Dordas, M. J. Chrispeels, and P. H. Brown
Permeability and Channel-Mediated Transport of Boric Acid across Membrane Vesicles Isolated from Squash Roots
Plant Physiology,
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A.-M. Teichert, T. L. Miller, S. C. Tai, Y. Wang, X. Bei, G. B. Robb, M. J. Phillips, and P. A. Marsden
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A. S. Verkman and A. K. Mitra
Structure and function of aquaporin water channels
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F. Sidoux-Walter, N. Lucien, B. Olives, R. Gobin, G. Rousselet, E.-J. Kamsteeg, P. Ripoche, P. M. T. Deen, J.-P. Cartron, and P. Bailly
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A.-K. Meinild, D. A. Klaerke, and T. Zeuthen
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B. Yang, T. Ma, and A. S. Verkman
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Copyright © 1998 by the American Society for Biochemistry and Molecular Biology.
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