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The lack of a suitable flat epithelial preparation isolated directly from the freshwater fish gill has led, in recent years, to the development of cultured gill epithelia on semipermeable supports. To date, their minimal capacity to actively transport ions has limited their utility as ionoregulatory models. The current study describes a new method of culturing gill epithelia consisting either of an enriched population of pavement (PV) cells or a mixed population of PV cells and mitochondria-rich (MR) cells from the gills of adult rainbow trout. Although the cell culture approach is similar to the double-seeded insert (DSI) technique described previously, it makes use of Percoll density centrifugation to first separate populations of PV and MR cells, which are then seeded on cell culture supports in varying proportions on successive days so as to produce preparations enriched in one or the other cell types. Based on rhodamine staining, the MR cell-rich epithelia exhibited a threefold higher enrichment of MR cells compared to traditional DSI preparations. In general, MR cell-rich epithelia developed extremely high transepithelial resistances (TER; >30 kOmega cm(2)) and positive transepithelial potentials (TEP) under symmetrical conditions (i.e., L15 medium on both apical and basolateral sides). Apical exposure of cell cultures to freshwater reduced TER and produced a negative TEP in all the epithelial preparations, although MR cell-rich epithelia maintained relatively high TER and negative TEP for over 2 d under these asymmetrical conditions. Measurement of unidirectional Na(+) fluxes and application of the Ussing flux ratio criterion demonstrated active Na(+) uptake in PV cell-rich and MR cell-rich epithelia under both symmetrical and asymmetrical conditions. In comparison, Ca(2+) uptake and Na(+)/K(+)-ATPase activity were significantly elevated in MR cell-rich preparations relative to the traditional DSI or PV cell-rich cultures under symmetrical conditions. This new methodology enhances our ability to tailor cultured gill epithelia on semipermeable supports with different proportions of PV cells and MR cells, thereby illuminating the ionoregulatory functions of the two cell types.

Na(+) and Ca(2+) regulation were compared in two euryhaline species, killifish (normally estuarine-resident) and rainbow trout (normally freshwater-resident) during an incremental salinity increase. Whole-body unidirectional fluxes of Na(+) and Ca(2+), whole body Na(+) and Ca(2+), and plasma concentrations (trout only), were measured over 1-h periods throughout a total 6-h protocol of increasing salinity meant to simulate a natural tidal flow. Killifish exhibited significant increases in both Na(+) influx and efflux rates, with efflux slightly lagging behind efflux up to 60% SW, but net Na(+) balance was restored by the time killifish reached 100% SW. Whole body Na(+) did not change, in agreement with the capacity of this species to tolerate daily salinity fluctuations in its natural habitat. In contrast, rainbow trout experienced a dramatic increase in Na(+) influx (50-fold relative to FW values), but not Na(+) efflux between 40 and 60% SW, resulting in a large net loading of Na(+) at higher salinities (60-100% SW), and increases in plasma Na(+) and whole body Na(+) at 100% SW. Killifish were in negative Ca(2+) balance at all salinities, whereas trout were in positive Ca(2+) balance throughout. Ca(2+) influx rate increased two- to threefold in killifish at 80 and 100% SW, but there were no concomitant changes in Ca(2+) efflux. Ca(2+) flux rates were affected to a larger degree in trout, with twofold increases in Ca(2+) influx at 40% SW and sevenfold increases at 100% SW. Again, there was no change in Ca(2+) efflux with salinity, so plasma Ca(2+) concentration increased in 100% SW. As the killifish is regularly submitted to increased salinity in its natural environment, it is able to rapidly activate changes in unidirectional fluxes in order to ensure ionic homeostasis, in contrast to the trout.

A novel cell isolation technique was used to characterize cadmium and calcium uptake in distinct populations of gill cells from the adult rainbow trout (Oncorhynchus mykiss). A specific population of mitochondria-rich (MR) cell, termed the PNA+ MR cell (PNA is peanut lectin agglutinin), was found to accumulate over threefold more 109Cd than did PNA- MR cells, pavement cells (PV cells), and mucous cells during a 1-h in vivo exposure at 2.4 microg/l 109Cd. In vitro 109Cd exposures, performed in standard PBS and Cl- -free PBS, at concentrations from 1 to 16 microg/l 109Cd, were also carried out to further characterize Cd2+ uptake kinetics. As observed during in vivo experiments, PNA+ MR cells accumulated significantly more 109Cd than did other cell types when exposures were performed by an in vitro procedure in PBS. Under such conditions, Cd2+ accumulation kinetics in all cell types could be described with Michaelis-Menten relationships, with Km values of approximately 3.0 microg/l Cd (27 nM) for both MR cell subtypes and 8.6 microg/l Cd (77 nM) for PV cells. In similar experiments performed in Cl- -free conditions, a significant reduction in 109Cd accumulation in PNA+ MR cells was seen but not in PNA- MR or in PV cells. In vitro 45Ca fluxes were also performed to determine the cellular localization of Ca2+ transport in these functionally distinct populations of gill cells. 45Ca uptake was most pronounced in PNA+ MR cells, with levels over threefold higher than those found in either PNA(-) MR or in PV cells. Results from the present study suggest that the PNA+ MR cell type is a high-affinity and high-capacity site for apical entry of Cd2+ and Ca2+ in the gill epithelium of rainbow trout.

Na+ and Ca2+ regulation were compared in two euryhaline species, killifish (normally estuarine-resident) and rainbow trout (normally freshwater-resident) during an incremental salinity increase. Whole-body unidirectional fluxes of Na+ and Ca2+, whole body Na+ and Ca2+, and plasma concentrations (trout only), were measured over 1-h periods throughout a total 6-h protocol of increasing salinity meant to simulate a natural tidal flow. Killifish exhibited significant increases in both Na+ influx and efflux rates, with efflux slightly lagging behind efflux up to 60% SW, but net Na+ balance was restored by the time killifish reached 100% SW. Whole body Na+ did not change, in agreement with the capacity of this species to tolerate daily salinity fluctuations in its natural habitat. In contrast, rainbow trout experienced a dramatic increase in Na+ influx (50-fold relative to FW values), but not Na+ efflux between 40 and 60% SW, resulting in a large net loading of Na+ at higher salinities (60–100% SW), and increases in plasma Na+ and whole body Na+ at 100% SW. Killifish were in negative Ca2+ balance at all salinities, whereas trout were in positive Ca2+ balance throughout. Ca2+ influx rate increased two- to threefold in killifish at 80 and 100% SW, but there were no concomitant changes in Ca2+ efflux. Ca2+ flux rates were affected to a larger degree in trout, with twofold increases in Ca2+ influx at 40% SW and sevenfold increases at 100% SW. Again, there was no change in Ca2+ efflux with salinity, so plasma Ca2+ concentration increased in 100% SW. As the killifish is regularly submitted to increased salinity in its natural environment, it is able to rapidly activate changes in unidirectional fluxes in order to ensure ionic homeostasis, in contrast to the trout. [ABSTRACT FROM AUTHOR]