Simultaneous minute by minute determination of unidirectional and net water fluxes in frog urinary bladder. A reexamination of the two barriers in series hypothesis.

Unidirectional and net water fluxes were simultaneously estimated in frog urinary bladder. The minute by minute tritiated water (3HOH) transepithelial flux and the net volume of fluid traversing the tissue were employed. It was observed that: (1) the time course of the increase in the 3HOH flux induced by antidiuretic hormone had a very similar pattern to that reported for the increase in the net movement. (2) Unstirred layers strongly affected the magnitude of the antidiuretic hormone-induced increase in 3HOH fluxes while the time course of the response was almost non-affected. In non-stimulated bladders 3HOH fluxes were poorly modified by medium stirring. New steady-state conditions for 3HOH fluxes were established 1 min after stirring rate modifications. (3) The simultaneously determined net water flux was not affected by a modification in the unstirred layers, indicating that the variations in the measured net water fluxes are a good estimation of the changes in the mucosal border permeability. (4) The presence of an osmotic gradient during hormonal challenge (implying net water fluxes, cell swelling and dilation of the intracellular spaces) did not modify the time course of 3HOH movements. These results suggest that the time course of the increase in water permeability is an intrinsic characteristic of the experimental system that could result from the addition of permeability units that increase in number during the development of the hormonal action.     

Urea uptake and translocation in toad urinary bladder: The effect of antidiuretic hormone

Summary The uptake of C¹⁴-urea into everted and noneverted bladder sacs was compared, over short time periods (up to 2 min), with the transepithelial urea fluxes. This method allowed the study of the time course of urea uptake and distribution, while previously this problem was only studied in steady-state conditions. When mucosal uptake was studied no accumulation of C¹⁴-urea inside the tissue was observed, indicating that the mucosal border could be the limiting step. Comparative studies of urea and inulin uptake from the serosal side showed that urea equilibrated with the water epithelial cells in less than 30 sec. This accumulation suggested again that the mucosal border is an effective barrier for urea translocation. The kinetics of the increase in urea permeability induced by antidiuretic hormone was also studied and it was similar (T1/2:4.3 min) to the kinetics of the increase in water permeability induced by the hormone (T1/2:5.6 min). A strong parallelism was also observed between the time course of the increases in water and urea permeabilities induced by medium hypertonicity (T1/2 25 and 26 min, respectively). The values obtained for the permeability coefficientk _trans), either at rest or under ADH were similar to those previously reported employing steady-state techniques (28±8 and 432±25 cm·sec^–1·10^–7, respectively).     

Reversible inhibition by lanthanum of the hydrosmotic response to serosal hypertonicity in toad urinary bladder

Summary In the urinary bladder of amphibia, hypertonicity of the serosal bath (SH) evokes an increase in transepithelial water permeability, the characteristics of which resemble the response to antidiuretic hormone (ADH). The ionic dependency, in particular for Ca²⁺, appears very similar forSH- and ADH-induced water fluxes. In the present experiments La³⁺ was used as a probe to study the Ca²⁺-dependency of the hydrosmotic response toSH in isolated urinary bladder of the toadBufo marinus.Addition of La³⁺ (5mm) on the serosal side of the membrane produced a significant and reversible increase in basal transepithelial water flux. The hydrosmotic response elicited by adding 250mm mannitol to the serosal Ringer's solution was inhibited by 30% in the absence of serosal Ca²⁺. Similarly, the hydrosmotic response toSH was inhibited by 37%, 30% and 40% when 5mm La³⁺ was added to the serosal medium 30 min before, concommitantly with, or 60 min after induction ofSH. The inhibition of transepithelial water flux observed in the absence of serosal Ca²⁺ or in the presence of serosal La³⁺ was reversible.The results support a critical role for Ca²⁺ in the modulation of transepithelial water permeability in the urinary bladder of amphibia. Ca²⁺ presumably exerts its effects at a post-cyclic AMP step.     

Evidence of basolateral water permeability regulation in amphibian urinary bladder

It is well known that arginine vasopressin (AVP) produces up to a 40-fold increase (0.1 to 4,0 μL/min·cm²) in net water flux across the amphibian urinary bladder under an osmotic gradient (mucosal side 10% hypotonic). No AVP effect is observed when the gradient is in the opposite direction (serosal hypotonic). Similar asymmetrical behavior to osmotic gradients occurs in the frog corneal epithelium. This rectification phenomenon has not been satisfactorily explained. We measured net water fluxes in bladder sacs and confirmed that AVP has no effect when the serosal bath is hypotonic. We reasoned that the ‘abnormal’ serosal osmolarity was inducing changes in membrane water permeability, the very parameter being measured. Thus, we studied the effect of solution osmolarity on diffusional water flow (J_dw) across the frog bladder using ³H₂O. As expected, AVP doubled J_dw (in either direction from 12 to 21 μL/min·cm²) when the serosal solution was iso-osmolar regardless of mucosal osmolarity. However, in the AVP-stimulated bladders, hypo-osmolarity of the serosal solution reduced J_dw by 42%, an effect that was reversible when normal osmolarity was re-established. Amphotericin B (instead of AVP) was used to irreversibly increase the permeability to water of the apical membrane. Under these conditions, basolateral hypotonicity also reversibly decreased J_dw by 32%, suggesting the basolateral membrane as the site where permeability is reduced. SEM and TEM of the tissue shows extreme swelling when it was exposed to serosal hypotonicity with or without AVP and typical surface morphology changes following hormone stimulation. We conclude that this swelling may initiate a signaling mechanism that reduces basolateral water permeability. These findings constitute evidence of basolateral water channel permeability regulation, which can also contribute to cell volume regulation.     

Net sodium fluxes change significantly at anatomically distinct root zones of rice (Oryza sativa L.) seedlings

Casparian bands of endodermis and exodermis play crucial roles in blocking apoplastic movement of ions and water into the stele of roots through the cortex. These apoplastic barriers differ considerably in structure and function along the developing root. The present study assessed net Na⁺ fluxes in anatomically distinct root zones of rice seedlings and analyzed parts of individual roots showing different Na⁺ uptake. The results indicated that anatomically distinct root zones contributed differently to the overall uptake of Na⁺. The average Na⁺ uptake in root zones in which Casparian bands of the endo- and exo-dermis were interrupted by initiating lateral root primordia (root zone III) was significantly greater than that at the root apex, where Casparian bands were not yet formed (root zone I), or in the region where endo- and exo-dermis with Casparian bands were well developed (root zone II). The measurement of net Na⁺ fluxes using a non-invasive scanning ion-selective electrode technique (SIET) demonstrated that net Na⁺ flux varied significantly in different positions along developing rice roots, and a net Na⁺ influx was obvious at the base of young lateral root primordia. Since sodium fluxes changed significantly along developing roots of rice seedlings, we suggest that the significantly distinct net Na⁺ flux profile may be attributed to different apoplastic permeability due to lateral root primordia development for non-selective apoplastic bypass of ions along the apoplast.     

Quantitative analysis of transpiration stream dynamics in an intact cucumber stem by a heat flux control method

Water flux of transpiration stream in an intact stem of the 10 leaf stage cucumber plant (Cucumis sativus L. cv. Chojitsu-Ochiai) was measured by a novel system of heat flux control method with a resolution of 1 × 10⁻³ grams per second and a time constant of 1 minute; two heat flux control sensors were attached to the seventh internode and the stem base. The transpiration stream responded clearly to leaf transpiration and root water absorption when the plant was exposed to light, and the water flux at the stem base corresponded to the transpiration rate per plant in steady state. Root water absorption lagged about 10 minutes behind leaf transpiration. Dynamics of water fluxes were affected by the lag of water absorption in roots, and temporary water loss caused by rapid increase in leaf transpiration was buffered by about 5% of the water content in the stem.     

Glutaraldehyde fixation preserves the permeability properties of the ADH-induced water channels

Summary Unidirectional and net water movements were determined, in frog urinary bladders, before and after glutraldehyde fixation. Experiments were performed in three experimental conditions: 1) in nonstimulated preparations, 2) after the action of antidiuretic hormone (ADH) and 3) in nonstimulated preparations to which amphotericin B was incorporated from the luminal bath. As previously observed for net water fluxes, the increase in the unidirectional water movement induced by ADH was well preserved by glutaraldehyde fixation. After correction for the effects of unstirred layers and nonosmotic pathways, the observed correlation between the ADH-induced increases in the osmotic (Pf) and diffusional (Pd) permeability coefficients was not modified by the fixative action (before glutaraldehyde: slope 11.19,r:0.87±0.07;n=12; after glutaraldehyde: slope 10.67,r:0.86±0.04,n=39). In the case of amphotericin B, Pf/Pd=3.08 (r: 0.83±0.08), a value similar to that observed in lipid bilayers or in nonfixed toad urinary bladders. It is concluded that 1) The experimental approach previously employed to study water channels in artificial lipid membranes and in amphibian urinary bladders, can be applied to the glutaraldehyde-fixed frog urinary bladder. 2) Glutaraldehyde fixation does not modify the permeability properties of the ADH-induced water channels. 3) Any contribution of exo-endocytic processes or cell regulatory mechanisms to the observed permeability parameters can probably be excluded. 4) Glutaraldehyde-fixed preparations are a good model to characterize these water pathways.     

Studies on the Movement of Water through the Isolated Toad Bladder and Its Modification by Vasopressin

Measurements of diffusion permeability and of net transfer of water have been made across the isolated urinary bladder of the toad, Bufo marinus, and the effects thereon of mammalian neurohypophyseal hormone have been examined. In the absence of a transmembrane osmotic gradient, vasopressin increases the unidirectional flux of water from a mean of 340 to a mean of 570 µl per cm² per hour but the net water movement remains essentially zero. In the presence of an osmotic gradient but without hormone net transfer of water remains very small. On addition of hormone large net fluxes of water occur; the magnitude of which is linearly proportional to the osmotic gradient. The action of the hormone on movement of water is not dependent on the presence of sodium or on active transport of sodium. Comparison of the net transport of water and of unidirectional diffusion permeability of the membrane to water indicates that non-diffusional transport must predominate as the means by which net movement occurs in the presence of an osmotic gradient. An action of the hormone on the mucosal surface of the bladder wall is demonstrated. The effects of the hormone on water movement are most simply explained as an action to increase the permeability and porosity of the mucosal surface of the membrane.     

Vasopressin Regulates Water Flow in a Rat Cortical Collecting Duct Cell Line Not Containing Known Aquaporins

Transepithelial water movements and arginine-vasopressin (AVP)-associated ones were studied in a renal cell line established from a rat cortical collecting duct (RCCD₁). Transepithelial net water fluxes (J _w ) were recorded every minute in RCCD₁ monolayers cultured on permeable supports. Spontaneous net water secretion was observed, which was inhibited by serosal bumetanide (10⁻⁵ m), apical glibenclamide (10⁻⁴ m) and apical BaCl₂ (5 × 10⁻³ m). RT-PCR, RNAse protection and/or immunoblotting experiments demonstrated that known renal aquaporins (AQP1, AQP2, AQP3, AQP4, AQP6 and AQP7) were not expressed in RCCD₁ cells. AVP stimulates cAMP production and sodium reabsorption in RCCD₁ cells. We have now observed that AVP significantly reduces the spontaneous water secretory flux. The amiloride-sensitive AVP-induced increase in short-circuit current (I _sc ) was paralleled by a simultaneous modification of the observed J _w : both responses had similar time courses and half-times (about 4 min). On the other hand, AVP did not modify the osmotically driven J _w induced by serosal hypertonicity. We can conclude that: (i) transepithelial J _w occurs in RCCD₁ cells in the absence of known renal aquaporins; (ii) the ``water secretory component' observed could be linked to Cl⁻ and K⁺ secretion; (iii) the natriferic response to AVP, preserved in RCCD₁ cells, was associated with a change in net water flux, which was even observed in absence of AQP2, AQP3 or AQP4 and (iv) the hydro-osmotic response to AVP was completely lost. Received: 30 December 1999/Revised: 12 October 2000     

The effect of ethanol on ion transport in frog skin

Frog skin has been used as a model epithelial sodium-transporting system to study the effect of ethanol on ion transport. Treatment of the outside of frog skin with ethanol decreased the net sodium transport due to inhibition of ²²Na⁺ influx. Ethanol did not alter sodium outflux when bathing the outside of the skin. The inhibition was in proportion to the concentration of ethanol, 0.25 M resulting in 50% inhibition. The chloride permeability of the skin was increased several-fold when the skin was exposed to ethanol in either bathing solution. With 0.4 M ethanol in the inner bathing solution, all the unidirectional fluxes of Na⁺ and Cl^? were increased. The movement of Cl^? was evaluated by comparison of Cl^? flux with urea flux, since urea is thought to move passively across frog skin via an extracellular (shunt) pathway. Chloride flux was increased to a greater extent than urea flux. These experiments indicate that ethanol affects chloride permeability beyond an increase in extracellular ion flow and independent of its effect on Na⁺ transport.     

Local osmotic coupling to the active trans-endothelial bicarbonate flux in the rabbit cornea

The present experiments investigate HCO₃⁻, Cl⁻ and fluid fluxes across partially destromalised corneas. Although there is no net flux of Cl⁻, there is a net flux of HCO₃⁻ across the endothelium from stromal side to aqueous side which is accompanied by a flux of water in the same direction. Bulk phase osmosis cannot account for the initiation of the flux of fluid. Local osmotic coupling between ions and water is postulated to occur in the preparation. The exudate is hypertonic to the bathing Ringer solution.     

Effect of ouabain upon diuretic-sensitive K+ transport in cultured cells evidence for separate modes of operation of the transporter

(1) Unidirectional K⁺ (⁸⁶Rb) influx and efflux were measured in subconfluent layers of MDCK renal epithelial cells and HeLa carcinoma cells. (2) In both MDCK and HeLa cells, the furosemide-inhibitable and chloride-dependent component of K⁺ influx/efflux was stimulated 2-fold by a 30 min incubation in 1 · 10^?3 M ouabain. (3) Measurements of net K⁺ loss and Na⁺ gain in ouabain-treated cells at 1 h failed to show any diuretic sensitive component, confirming the exchange character of the diuretic-sensitive fluxes. (4) Prolonged incubations for 2.5 h in ouabain revealed a furosemide- and anion-dependent K⁺ (Cl^?) outward net flux uncoupled from net Na⁺ movement. Net K⁺ (Cl^?) outward flux was half-maximally inhibited by 2 μM furosemide. (5) After 2.5 h ouabain treatment, the anion and cation dependence of the diuretic-sensitive K⁺ influx/efflux were essentially unchanged when compared to untreated controls.     

Short circuit current in tight and leaky epithelia

The effect of short circuit current on the unidirectional fluxes of ions transported across tight and leaky epithelia was investigated. It was found that short circuiting of the frog gastric mucosa (classified as a tight epithelium) caused a decrease of the passive J_ms^C1 and a significant increase of the net Cl^? secretion. However, no significant change of H⁺ secretory rate was observed. On the other hand, short circuiting of the mouse intestine (a known leaky membrane) caused a simultaneous increase of both J_ms and J_sm fluxes of Na⁺ while the net fluxes of Na⁺ and Cl^? remained unchanged. Also, short circuiting did not change the water permeability of the mouse intestine. To explain some of these results a theoretical model is presented to demonstrate that while short circuiting can block the passive ionic movement, it will cause an increase in the energy consumption of the system and introduce certain important changes in the ionic barriers and e.m.fs. The simultaneous increase in the unidirectional fluxes of Na⁺ under short circuit conditions can best be explained by a decrease in the polarized nature of the transepithelial shunt, thereby increasing the diffusion coefficient of the ion(s). Such an increase is specially favorable to the Na⁺ rather than an anion.     

Large Canopy Exchange Fluxes of Inorganic and Organic Nitrogen and Preferential Retention of Nitrogen by Epiphytes in a Tropical Lowland Rainforest

Little is known about how tropical forest canopies interact with atmospheric nitrogen deposition and how this affects the internal nutrient dynamics and the processing of external nutrient inputs. The objectives of this study therefore were (1) to investigate gross and net canopy nitrogen (N) fluxes (retention and leaching) and (2) the effect of canopy components on net canopy N retention. Tracers were applied on detached branches in a tropical wet lowland rainforest, Costa Rica. A novel ¹⁵N pool dilution method showed that gross canopy fluxes (retention and leaching) of NO₃ ^?, NH₄ ⁺, and dissolved organic nitrogen (DON) were remarkably higher than net throughfall fluxes. Gross fluxes of NH₄ ⁺ and NO₃ ^? resulted in a negligible net flux whereas DON showed net uptake by the canopy. The highest quantity of ¹⁵N was recovered in epiphytic bryophytes (16.4%) although the largest biomass fraction was made up of leaves. The study demonstrates that tracer applications allow investigation of the dynamic and complex canopy exchange processes and that epiphytic communities play a major role in solute fluxes in tree canopies and therefore in the nutrient dynamics of tropical rain forests.     

Cation regulation in the smooth muscle of frog stomach

Cation composition of frog smooth muscle cells was investigated. Fresh stomach muscle rings resembled skeletal muscle, but marked Na gain and K loss followed immersion. Mean Na (49.8–79.7 mM/kg tissue) and K (61.8–80.1 mM/kg tissue) varied between batches, but were stable for long periods in vitro. Exchange of 6–30 mM Na/kg tissue with ²²Na was extremely slow and distinct. Extracellular water was estimated from sucrose-¹⁴C uptake. Calculated exchangeable intracellular Na was 9 mM/kg cell water, and varied little. Thus steady-state transmembrane cation gradients appeared to be steep. K-free solution had only slight effects. Ouabain (10^-4 M) caused marked Na gain and reciprocal K loss; at 30°C, Na and K varied linearly with time over a wide range of contents, indicating constant net fluxes. Net fluxes decreased with temperature decrease. ²²Na exchange in ouabain-treated tissue at 20–30°C was rapid and difficult to analyze. The best minimum estimates of unidirectional Na fluxes at 30°C were 10–12 times the constant net flux; constant pump efflux may explain these findings. The rapidity of Na exchange may not reflect very high permeability, but it does require a high rate of transport work.     

Effect of Insulin on Potassium Flux and Water and Electrolyte Content of Muscles from Normal and from Hypophysectomized Rats

It was reported previously that insulin hyperpolarized rat skeletal muscle and decreased K⁺ flux in both directions. The observations on K⁺ flux are now extended to take advantage of the greater sensitivity to insulin of hyperphysectomized rats. Insulin caused a shift of water from extracellular to intracellular space if glucose was present, but not in its absence. Insulin caused net gain of muscle fiber K⁺, though not necessarily an increase in K⁺ concentration in fiber water. It probably also decreased intrafiber Na⁺ and Cl^-. Insulin decreased K⁺ efflux. The effect was dose-dependent. Muscles from hypophysectomized rats were more sensitive to the action of insulin on K⁺ flux than were those from normal rats. The effect was demonstrable within the time resolution of the system, suggesting that insulin's action is on cell surfaces. K⁺ influx was also decreased by insulin. Bookkeeping suggests that some K⁺ influx be called active. Insulin seemed to decrease active K⁺ influx and passive K⁺ efflux. It is not resolved whether insulin has a true dual effect or whether it acts only on passive fluxes in both directions (the apparent action on active K⁺ influx being an artefact of incomplete definition of passive flux) or whether a single alteration in the membrane may affect both active and passive fluxes.     

Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

Active processes of permafrost thaw in Western Siberia increase the number of soil subsidencies, thermokarst lakes and thaw ponds. In continuous permafrost zones, this process promotes soil carbon mobilisation to water reservoirs, as well as organic matter (OM) biodegradation, which produces a permanent flux of carbon dioxide (CO₂) to the atmosphere. At the same time, the biogeochemical evolution of aquatic ecosystems situated in the transition zone between continuous permafrost and permafrost-free terrain remains poorly known. In order to better understand the biogeochemical processes that occur in thaw ponds and lakes located in discontinuous permafrost zones, we studied ~30 small (1–100,000 m²) shallow (<1 m depth) lakes and ponds formed as a result of permafrost subsidence and thaw of the palsa bog located in the transition zone between the tundra and forest-tundra (central part of Western Siberia). There is a significant increase in dissolved CO₂ and methane (CH₄) concentration with decreasing water body surface area, with the largest supersaturation with respect to atmospheric CO₂ and CH₄ in small (<100 m²) permafrost depressions filled with thaw water. Dissolved organic carbon (DOC), conductivity, and metal concentrations also progressively increase from large lakes to thaw ponds and depressions. As such, small water bodies with surface areas of 1–100 m² that are not accounted for in the existing lake and pond databases may significantly contribute to CO₂ and CH₄ fluxes to the atmosphere, as well as to the stocks of dissolved trace elements and organic carbon. In situ lake water incubation experiments yielded negligible primary productivity but significant oxygen consumption linked to the mineralisation rate of dissolved OM by heterotrophic bacterioplankton, which produce a net CO₂ flux to the atmosphere of 5 ± 2.5 mol C m² year^?1. The most significant result of this study, which has long-term consequences on our prediction of aquatic ecosystem development in the course of permafrost degradation is CO₂, CH₄, and DOC concentrations increase with decreasing lake age and size. As a consequence, upon future permafrost thaw, the increase in the number of small water bodies, accompanied by the drainage of large thermokarst lakes to the hydrological network, will likely favour (i) the increase of DOC and colloidal metal stocks in surface aquatic systems, and (ii) the enhancement of CO₂ and CH₄ fluxes from the water surface to the atmosphere. According to a conservative estimation that considers that the total area occupied by water bodies in Western Siberia will not change, this increase in stocks and fluxes could be as high as a factor of ten.     

宁夏六盘山4种典型森林伴随降水的无机氮通量变化特征

在宁夏六盘山香水河小流域,选择建立了4种典型森林的样地,测定了2011年生长季(5月24日—10月20日)大气降水(724.3 mm)、穿透水、干流、枯落物渗透水和主根系层(0—30 cm)土壤渗透水的无机氮(NH~+_4-N、NO~-_3-N)浓度及相应通量的变化。结果表明,在林外降水转化林下降水中,各样地林下降水携带的生长季NH~+_4-N通量(kg/hm~2)(华北落叶松人工林2.40、华山松次生林2.37、野李子灌丛2.29、桦木次生林2.09)均明显低于林外降水(3.04),NO~-_3-N通量(kg/hm~2)(华北落叶松人工林2.15、桦木次生林2.14、野李子灌丛2.09、华山松次生林1.92)更显著低于林外降水(4.27)。整体看来,阔叶林林冠的无机氮吸附(吸收)作用稍高于针叶林。在4种森林样地的枯落物层渗透水中,无机氮浓度变化在0.68—0.88 mg/L,稍高于林冠穿透水的无机氮浓度;4个样地的枯落物渗透水的无机氮通量(kg/hm~2)(野李子灌丛4.10、桦木次生林3.24、华山松次生林3.22、华北落叶松人工林2.77)均低于林下降水。在华山松次生林和华北落叶松人工林的主根系层(0—30 cm)土壤渗透水中,无机氮浓度均高于枯落物渗漏水;因土壤淋出作用,华山松次生林和华北落叶松人工林的土壤渗透水的无机氮输出通量分别为16.34 kg/hm~2和18.93 kg/hm~2,均显著高于枯落物渗透水的输入通量。整体来看,林外降水在林地无机氮输入中占有重要地位,在研究年份生长季,林冠层和枯落物层的吸附(吸收)作用使降水输入的无机氮通量明显降低,但主根系层土壤淋出作用显著增大了土壤渗透水携带的无机氮输出通量,表现为土壤层氮素流失。     

Effects of ouabain on chloride movements across the seawater eel intestine

Summary Simultaneous measurements of transepithelial potential difference (PD) and net water flux were made in the stripped intestine of seawater eels, and the effects of ouabain on these two parameters were examined in normal Ringer solution or under a chloride concentration gradient. Ouabain reduced the serosa-negative PD and the net water flux in normal Ringer solution with a linear relationship between the PD and the net water flux. Removal of K⁺ from the Ringer solution on both serosal and mucosal sides also reduced the PD and the net water flux to approximately zero. On the other hand, blocking the Na⁺–K⁺ pump by ouabain, K⁺-free or Na⁺-free Ringer solution increased the diffusion potential for Cl^–. Inhibition of Cl^– transport and increment in Cl^– permeability by ouabain occurred almost simultaneously. It is likely, therefore, that Cl^– transport as well as Cl^– permeability is dependent on Na⁺–K⁺ pump activity. A possible mechanism of dependence of Cl^– transport on the Na⁺–K⁺ pump is discussed in relation to the increment in Cl^– permeability.     

Na+-dependent co-transport of α-methyl d-glucoside across the mucosal border of rabbit descending colon

(1) The uptake and bidirectional fluxes of 1-α-methyl d-glucoside were studied in isolated rabbit colonic mucosa. (2) The uptake of α-methyl d-glucoside was linear over the first 30 min and reached maximum after 1 h; was a saturable function of sugar concentration and was Na⁺-dependent. (3) An increase in sugar uptake across the mucosal border and net transepithelial sugar flux across sheets of colon was observed in the presence of 10^?4 M amiloride. (4) Phlorizin (10^?4 M) inhibited sugar uptake into the tissue water and abolished net sugar flux. Amiloride-stimulated sugar uptake was also abolished by 10^?4 M phlorizin. (5) Ouabain (10^?4 M) prevented the effect of amiloride on sugar uptake and inhibited sugar uptake into the tissue. (6) These results corroborate the findings of Henriques de Jesus et al.(Henriques de Jesus, C., Da Gracia Emilio, M. and Santos, M.A. Gastroenterol. Clin. Biol. 3, 172–173) who found a sugar-dependent increase in short-circuit current in colonic mucosa exposed to amiloride.