Fluid reabsorption by Necturus proximal tubule perfused with solutions of normal and reduced osmolarity

Marine sponges discriminate between food bacteria and bacterial symbionts: electron microscope radioautography and in situ evidence

This study considered whether marine sponges are selective particle feeders, and whether they are capable of distinguishing between sponge bacterial symbionts and other bacteria. Four species of marine sponges ( Aplysina aerophoba, A. cavernicola, Pericharax heteroraphis and Spongia sp.) were fed in situ with tritium-labelled bacteria, either symbionts or other bacteria isolated from seawater. A large proportion of bacterial symbionts passed through the sponge and were expelled in the exhalant current, whereas seawater bacteria disappeared from the incubation water and were retained within the sponge. The seawater bacteria were observed in choanocytes and occasionally in pinacocytes after 30-40 min, whereas symbiont bacteria were rarely observed. Although sponges do have mechanisms to ingest particles such as food, they appear to be unable to consume bacterial symbionts, probably because their identity is masked by capsular sheaths. A specific mechanism for recognition and rejection of self-particulate matter is proposed for sponge epidermal cells.

Molecular mechanisms for passive and active transport of water

Water crosses cell membranes by passive transport and by secondary active cotransport along with ions. While the first concept is well established, the second is new. The two modes of transport allow cellular H2O homeostasis to be viewed as a balance between H2O leaks and H2O pumps. Consequently, cells can be hyperosmolar relative to their surroundings during steady states. Under physiological conditions, cells from leaky epithelia may be hyperosmolar by roughly 5 mosm liter-1, under dilute conditions, hyperosmolarities up to 40 mosm liter-1 have been recorded. Most intracellular H2O is free to serve as solvent for small inorganic ions. The mechanism of transport across the membrane depends on how H2O interacts with the proteinaceous or lipoid pathways. Osmotic transport of H2O through specific H2O channels such as CHIP 28 is hydraulic if the pore is impermeable to the solute and diffusive if the pore is permeable. Cotransport of ions and H2O can be a result of conformational changes in proteins, which in addition to ion transport also translocate H2O bound to or occlude in the protein. A cellular model of a leaky epithelium based on H2O leaks and H2O pumps quantitatively predicts a number of so-far unexplained observations of H2O transport.

Water permeability of ventricular cell membrane in choroid plexus epithelium from Necturus maculosus

1. The osmotic water permeability Lp and the relations between the flows of H2O, K+ and Cl- were studied in the ventricular membrane of the epithelium from the choroid plexus of Necturus maculosus. 2. The flows were induced by abrupt changes in external osmolarity of the ventricular solution. Solution changes were convective and no effects of unstirred layers could be detected on measured parameters. 3. The initial rate of change in intracellular concentrations of K+ and Cl- was monitored by double-barrelled ion-selective microelectrodes. 4. The initial rate of flux of H2O could be monitored as the changes in the concentration of intracellular choline ions (Ch+i). When 0.5 mmol l-1 of choline chloride was added to the external solutions, Ch+i attained values of 1-5 mmol l-1. The dilution or concentration of Ch+i could be recorded by K+ electrodes since the sensitivity of these to Ch+ is more than 50 times greater than to K+. 5. The Lp of the ventricular membrane of the epithelium was 1.4-2.1 x 10(-4) cm s-1 (osmol l-1)-1 and independent of the direction of the induced water flux. Lp was unchanged in tissues adapted to osmolarities of half the physiological value. 6. The efflux of H2O induced by mannitol was associated with an instantaneous efflux of K+ which was inhibited by furosemide. The fluxes had a ratio of 40 mmol l-1. The influx of H2O induced by the removal of NaCl from the ventricular solution was associated with an instantaneous influx of K+. The H2O influx had a ratio to the flux of K+ of 70 mmol l-1. 7. The efflux of H2O induced by mannitol was associated with an efflux of Cl- which was inhibited by furosemide. The ratio of the two fluxes was in the range 15-44 mmol l-1. 8. The conclusion is that the Ch+ method gives a reliable measure of the movement of H2O across the ventricular membrane. The magnitude of the Lp and its relevance to transepithelial transport are discussed. The osmotically induced H2O movement is accompanied by furosemide-sensitive fluxes of K+ and Cl- of the same magnitude. This suggests that co-transport between H2O and KCl can take place in the membrane.

Volume regulation in the early proximal tubule of the Necturus kidney

The ability of early proximal tubule cells of the Necturus kidney to regulate volume was evaluated using light microscopy, video analysis and conventional microelectrodes. Necturus proximal tubule cells regulate volume in both hyper- and hyposmotic solutions. Volume regulation in hyperosmotic fluids is HCO3- dependent and is associated with a decrease in the relative K+ conductance of the basolateral cell membrane and a decrease in the resistance ratio, Ra/Rbl. Volume regulation in hyposmotic solutions is also dependent upon the presence of HCO3- but is also inhibited by 2 mM Ba2+ in the basolateral solution. Hyposmotic regulation is accompanied by an increase in the relative K+ conductance of the basolateral cell membrane and an increase in Ra/Rbl. Neither hypo- nor hyposmotic regulation have any affect on the depolarization of the basolateral cell membrane potential induced by HCO3- removal. We conclude that volume regulation in the early proximal tubule of the kidney involves both HCO3(-)-dependent transport systems and the baso-lateral K+ conductance.

Pathways for volume flow and volume regulation in leaky epithelia

Continuous pathways must pierce the cell membrane to be used by water during osmotic equilibration between proximal straight tubular cells and the external medium, because a) the water osmotic permeability coefficient of the basolateral plasma membrane, Poscb, is high; b) its activation energy, Ea, is as that of free water movement and c) pCMBS inhibits markedly (but reversibly) Poscb and increases Ea to values similar to those observed in lipid bilayers without pores. d) Preliminary measurements of Pd the water diffusive permeability coefficient using NMR indicate that Poscb/Pd is near 4 - 5. The following two observations indicate that a significant paracellular water flow must exist in leaky epithelia. Namely, a) large extracellular solutes are dragged by water in four leaky epithelia: gall bladder, Necturus proximal tubule, rat proximal tubule and Rhodnius malpighian tubule. b) The transcellular water osmotic permeability coefficient is smaller than the transepithelial values available in the rabbit proximal straight tubule. This requires a significant paracellular permeability.

The continuous measurement of tubular volume changes in response to step changes in contraluminal osmolality

A new method to measure time dependent (t) volume (V) changes in proximal straight tubules (PST) is described. V is calculated from diameter (d) measurements for which a video camera and an integrating circuit are used. A tubular image of high optical contrast is recorded with the TV camera such that the scan lines run crosswise to the tubule. The video signal is analyzed by a special processor which adds 225 tubular diameters of each TV frame and feeds this analog signal to a pen recorder. The fractional error in d measurements is 10(-3). Diameter changes of less than 0.05 micron can be detected, as compared to the usual error of a single measurement of about 0.4 micron. Pcbos, the osmotic water permeability of the contraluminal cell membrane was measured by setting up osmotic steps across it in less than 0.1 s and following the ensuing delta d/delta t. The time delay between solution change and the linear part of the osmotic response was 0.51 +/- 0.05 s. Pcbos was found to be 50.4 (+/- 8.7) X 10(-4) cm3.cm-2 of basement membrane area .s-1.osmolar-1.