KCl transport across and insect epithelium: I. Tracer fluxes and the effects of ion substitutions

Summary Models for active Cl transport across epithelia are often assumed to be universal although they are based on detailed studies of a relatively small number of epithelia from vertebrate animals. Epithelial Cl transport is also important in many invertebrates, but little is known regarding its cellular mechanisms. We used short-circuit current, tracer fluxes and ion substitutions to investigate the basic properties of Cl absorption by locust hindgut, an epithelium which is ideally suited for transport studies. Serosal addition of 1mm adenosine 35-cyclic monophosphate (cAMP), a known stimulant of Cl transport in this tissue, increased short-circuit current (I _sc) and net reabsorptive³⁶Cl flux (J _net ^Cl ) by 1000%. Cl absorption did not exhibit an exchange diffusion component and was highly selective over all anions tested except Br. Several predictions of Na- and HCO₃-coupled models for Cl transport were tested: Cl-dependentI _sc was not affected by sodium removal (<0.05mm) during the first 75 min. Also, a large stimulation ofJ _net ^Cl was elicited by cAMP when recta were bathed for 6 hr in nominally Na-free saline (<0.001 to 0.2mm) and there was no correlation between Cl transport rate and the presence of micromolar quantities of Na contamination. Increased unidirectional influx of³⁶Cl into rectal tissue during cAMP-stimulation was not accompanied by a comparable uptake of²²Na.J _net ^Cl was independent of exogenous CO₂ and HCO₃, but was strongly dependent on the presence of K. These results suggest that the major fraction of Cl transport across this insect epithelium occurs by an unusual K-dependent mechanism that does not directly require Na or HCO₃.     

Modes of Cl− transport across the mucosal and serosal membranes of urodele intestinal cells

Summary The characteristics of Cl^– movement across luminal and basolateral membranes ofAmphiuma intestinal absorptive cells were studied using Cl^–-sensitive microelectrodes and tracer³⁶Cl techniques. Intracellular Cl^– activity (a _Cl ⁱ ) was unchanged when serosal Cl^– was replaced; when luminal Cl^– was replaced cell Cl^– was rapidly lost. Accordingly, the steady statea _Cl ⁱ could be varied by changing the luminal [Cl]. As luminal [Cl] was raised from 1 to 86mM,a _Cl ⁱ rose in a linear manner, the mucosal membrane hyperpolarized, and the transepithelial voltage became serosa negative. In contrast, the rate of Cl^– transport from the cell into the serosal medium, measured as the SITS-inhibitable portion of the Cl^– absorptive flux, attained a maximum whena _Cl ⁱ reached an apparent value of 17mm, indicating the presence of a saturable, serosal transport step. The stilbeneinsensitive absorptive flux was linear with luminal [Cl], suggestive of a paracellular route of movement. Intracellulara _Cl was near electrochemical equilibrium at all but the lowest values of luminal [Cl] after interference produced by other anions was taken into account.a _Cl ⁱ was unaffected by Na replacement, removal of medium K, or elevation of medium HCO ₃ ^– . Mucosae labeled with³⁶Cl lost isotope into both luminal and serosal media at the same rate and from compartments of equal capacity. Lowering luminal [Cl] or addition of theophylline enhanced luminal Cl^– efflux. It is concluded that a conductive Cl leak pathway is present in the luminal membrane. Serosal transfer is by a saturable, stilbene-inhibitable pathway. Luminal Cl^– entry appears to be passive, but an electrogenic uptake cannot be discounted.     

Leaching and crop recovery of15N from ammonium sulphate and labelled maize (Zea mays) material in lysimeters at a site in Zimbabwe

The fate of¹⁵N-ammonium sulphate fertilizer that was applied to four lysimeters in the 1990/91 summer was studied over three consecutive growing seasons during which either maize or wheat was grown. Aboveground portions of¹⁵N-labelled maize plants from the first harvest were applied to four other lysimeters at 5 t ha^–1. Two lysimeters in each of the sets of four were assigned a low and a high moisture treatment using irrigation. In both moisture treatments, plant recovery of fertilizer-¹⁵N in the first season was 27% and a further 2% was recovered by plants during the next two seasons. During the second and third seasons, total recovery of¹⁵N by aboveground plant portions from lysimeters that received¹⁵N-labelled maize material was equivalent to 2.5% of applied fertilizer-¹⁵N. This corresponded to ca. 18% recovery of the¹⁵N added in maize material. Leaching of fertilizer-N over the three growing seasons did not exceed 0.3% in total. During the first season, a maximum of 0.25 kg N ha^–1, equivalent to 0.25% of the applied fertilizer-N, was leached in the high moisture treatment. This represented 1.8% of the nitrate load in leachates. Less than 0.002% of the applied fertilizer-N was leached in the low moisture treatment during the first season.     

K+ and Cl− conductances in the apical membrane from secreting oxyntic cells are concurrently inhibited by divalent cations

Summary This study concerns the properties of rapid K⁺ and Cl transport pathways that are present in the (H⁺+K⁺)-ATPase membrane from stimulated, and secreting, gastric oxyntic cells. Ion permeabilities in the isolated stimulation-associated vesicles were monitored via the rates of H⁺ efflux under conditions of exclusive H⁺/K⁺ counterflux or H⁺–Cl co-efflux, as well as by comparison of equilibration rates for⁸⁶Rb and³⁶Cl under conditions of equilibrium exchange and unidirectional salt flux. These latter studies suggest that Rb⁺ and Cl pathways are conductive and independent. In spite of the functional independence of the ion pathways, several divalent cations inhibit Rb⁺ and Cl isotopic exchange as well as the H⁺ efflux that is dependent on either K⁺ or anion (Cl, SCN, NO₂) fluxes. Zn²⁺ is the more potent inhibitor, reducing by 50% the sensitive component of K⁺, Cl, and NO₂ fluxes at about 20 m; Mn²⁺ has a similar effect at 200 m. Ni²⁺ and Co²⁺ were roughly equipotent to Mn²⁺ while Mg²⁺ and Ca²⁺ had not inhibitory effect. These results suggest that the stimulation-induced permeabilities, while functioning independently, may be physically linked, i.e., residing within a single entity. In similar studies carried out in (H⁺+K⁺)-ATPase vesicles obtained from nonstimulated cells, no vestiges of sensitivity to the inhibitory divalent cations could be detected. The implications of these findings for the physiology of the oxyntic cell in the context of a model for membrane fusion are discussed.     

Membrane potentials and intracellular Cl− activity of toad skin epithelium in relation to activation and deactivation of the transepithelial Cl− conductance

Summary The potential dependence of unidirectional³⁶Cl fluxes through toad skin revealed activation of a conductive pathway in the physiological region of transepithelial potentials. Activation of the conductance was dependent on the presence of Cl^– or Br^– in the external bathing solution, but was independent of whether the external bath was NaCl-Ringer's, NaCl-Ringer's with amiloride, KCl-Ringer's or choline Cl-Ringer's To partition the routes of the conductive Cl^– ion flow, we measured in the isolated epithelium with double-barrelled microelectrodes apical membrane potentialV _a , and intracellular Cl^– activity,a _Cl ^c , of the principal cells indentified by differential interference contrast microscopy. Under short-circuit conditionsI _sc=27.0±2.0 A/cm², with NaCl-Ringer's bathing both surfaces,V _a was –67.9±3.8mV (mean ±se,n=24, six preparations) anda _Cl ^c was 18.0±0.9mM in skins from animals adapted to distilled water. BothV _a anda _Cl ^a were found to be positively correlated withI _sc (r=0.66 andr=0.70, respectively). In eight epithelia from animals adapted to dry milieu/tap waterV _a anda _Cl ^c were measured with KCl Ringer's on the outside during activation and deactivation of the transepithelial Cl^– conductance (G _Cl) by voltage clamping the transepithelial potential (V) at 40 mV (mucosa positive) and –100 mV. AtV=40 mV; i.e. whenG _Cl was deactivated,V _a was –70.1±5.0 mV (n=15, eight preparations) anda _Cl ^c was 40.0±3.8mm. The fractional apical membrane resistance (fR _a) was 0.69±0.03. Clamping toV=–100 mV led to an instantaneous change ofV _a to 31.3±5.6 mV (cell interior positive with respect to the mucosal bath), whereas neithera _Cl ^c norfR _a changed significantly within a 2 to 5-min period during whichG _Cl increased by 1.19±0.10 mS/cm². WhenV was stepped back to 40 mV,V _a instantaneously shifted to –67.8±3.9 mV whilea _Cl ^c andfR _a remained constant during deactivation ofG _Cl. Similar results were obtained in epithelia impaled from the serosal side. In 12 skins from animals adapted to either tap water or distilled water the density of mitochondria-rich (D _MRC) cells was estimated and correlated with the Cl current (I _Cl though the fully activated (V=–100mV) Cl^– conductance). A highly significant correlation was revealed (r=–0.96) with a slope of –2.6 nA/m.r. (mitochondria-rich cell and an I-axis intercept not significantly different from zero. In summary, the voltage-dependent Cl currents were not reflected infR _a anda _Cl ^a of the principal cells but showed a correlation with the m.r. cell density. We conclude that the pricipal cells do not contribute significantly to the voltage-dependent Cl conductance.     

Is KCl a reliable extractant of15NH 4 + added to coastal marine sediments?

The release of NH ₄ ⁺ and¹⁵N-labelled NH ₄ ⁺ by one-step KCl extraction was assessed in different types of coastal marine sediments. KCl was efficient to extract NH ₄ ⁺ from sandy sediments and less efficient in silt sediments, where an extended extraction period was required for obtaining a maximum NH ₄ ⁺ yield. Extraction at 0 or 20 °C had only a little effect on the efficiency of KCl. KCl gave always non complete recovery of¹⁵NH ₄ ⁺ in silt sediments. However, the added label could be fully recovered by addition of 80 mol·cm^–3 exogenous NH ₄ ⁺ prior to KCl, or when NaCl or ASW replaced KCl.¹⁵NH ₄ ⁺ was added to non-biological silt sediment, which was incubated at 0 °C up to 16 hours, to see the effect of physical processes on the partition of¹⁵NH₄ among porewater (29–49%) exchangeable (9–30%) and non-extractable, organic bound pools (24–42%). Total¹⁵N recovery was approximately 100%. KCl failed to remove¹⁵NH₄ which entered to unknown, bound pools in sediment. Only shortly after addition of¹⁵N (0.1 h), the extraction period resulted in significantly different¹⁵N recoveries (P < 0.05) in KCl extractable NH ₄ ⁺ , 17% versus 9% of label was recovered after 1 min or 60 min extraction of sediment, respectively. Two hours of incubation time were required for complete equilibrium of¹⁵NH ₄ ⁺ among porewater, exchangeable and organic bound pools. Sediments (silt) to which¹⁵NH ₄ ⁺ has been added in order to measure NH ₄ ⁺ turn-over and KCl is used as extractant, should be incubated for at least 2 hours, before taking a zero-time sample.     

Characterization of chloride channels in membrane vesicles from the kidney outer medulla

Summary The basolateral membrane of the thick ascending loop of Henle (TALH) of the mammalian kidney is highly enriched in Na⁺/K⁺ ATPase and has been shown by electrophysiological methods to be highly conductive to Cl^–. In order to study the Cl^– conductive pathways, membrane vesicles were isolated from the TALH-containing region of the porcine kidney, the red outer medulla, and Cl^– channel activity was determined by a³⁶Cl uptake assay where the uptake of the radioactive tracer is driven by the membrane potential (positive inside) generated by an outward Cl^– gradient. The accumulation of³⁶Cl^– inside the vesicles was found to be dependent on the intravesicular Cl^– concentration and was abolished by clamping the membrane potential with valinomycin. The latter finding indicated the involvement of conductive pathways. Cl^– channel activity was also observed using a fluorescent potential-sensitive carbocyanine dye, which detected a diffusion potential induced by an imposed inward Cl^– gradient. The anion selectivity of the channels was Cl^–>NO ₃ ^– =I^– gluconate. Among the Cl^– transport inhibitors tested, 5-nitro-2-(3-phenylpropylamino)-benzoic acid (NPPAB), 4,4-diisothiocyano-stilbene-2,2-disulfonate (DIDS), and diphenylamine-2-carboxylate (DPC) showed IC₅₀ of 110, 200 and 550 m, respectively. Inhibition of³⁶Cl uptake by NPPAB and two other structural analogues was fully reversible, whereas that by DIDS was not. The nonreactive analogue of DIDS, 4,4-dinitrostilbene-2,2-disulfonate (DNDS), was considerably less inhibitory than DIDS (25% inhibition at 200 m). The irreversible inhibition by DIDS was prevented by NPPAB, whereas DPC was ineffective, consistent with its low inhibitory potency. It is proposed that NPPAB and DIDS bind to the same or functionally related site on the Cl^– channel protein.     

Contributions to nitrogen leaching and pasture uptake by autumn-applied dairy effluent and ammonium fertilizer labeled with 15N isotope

The objective of this study was to compare the N leaching loss and pasture N uptake from autumn-applied dairy shed effluent and ammonium fertilizer (NH₄Cl) labeled with ¹⁵N, using intact soil lysimeters (80 cm diameter, 120 cm depth). The soil used was a sandy loam, and the pasture was a mixture of perennial ryegrass (Lolium perenne) and white clover (Trifolium repens). The DSE and NH₄Cl were applied twice annually in autumn (May) and late spring (November), each at 200 kg N ha^-1. The N applied in May 1996 was labeled with ¹⁵N. The lysimeters were either spray or flood irrigated during the summer. The autumn-applied DSE resulted in lower N leaching losses compared with NH₄Cl. However, the N applied in the autumn had a higher potential for leaching than N applied in late spring. Between 4.5–8.1% of the ¹⁵N-labeled mineral N in the DSE and 15.1–18.8% of the ¹⁵N-labeled NH₄Cl applied in the autumn were leached within a year of application. Of the annual N leaching losses in the DSE treatments (16.0–26.9 kg N ha^-1), a fifth (20.3–22.9%) was from the mineral N fraction of the DSE applied in the autumn, with the remaining larger proportion from the organic fraction of the DSE, soil N and N applied in spring. In the NH₄Cl treatments, more than half (53.8–64.8%) of the annual N leaching loss (55.9–57.6 kg N ha^-1) was derived from the autumn-applied NH₄Cl. DSE was as effective as NH₄Cl in stimulating pasture production. Since only 4.4–4.5% of the annual herbage N uptake in the DSE treatment and 12.3–13.3% in the NH₄Cl treatment were derived from the autumn-applied mineral N, large proportions of the annual herbage N uptake must have been derived from the N applied in spring, the organic N fraction in the DSE, soil N and N fixed by clover. The recoveries of ¹⁵N in the herbage were similar between the DSE and the NH₄Cl treatments, but those in the leachate were over 50% less from the DSE than from the NH₄Cl treatment. The lower leaching loss of ¹⁵N in the DSE treatment was attributed to the stimulated microbial activities and increased immobilization following the application of DSE. This revised version was published online in June 2006 with corrections to the Cover Date.     

Evidence against associative N2 fixation as a significant N source in long-term wheat plots

In monocropped cereal systems, annual N inputs from non-fertilizer sources may be more than 30 kg ha^-1. We examined the possibility that these inputs are due to biological N₂ fixation (BNF) associated with roots or decomposing residues. Wheat was grown under greenhouse conditions in pots (34 cm long by 10 cm diameter) containing soil from a plot cropped to spring wheat since 1911 without fertilization. The roots and soil were sealed from the atmosphere and exposed to a¹⁵N₂-enriched atmosphere for three to four weeks during vegetative, reproductive or post-reproductive stages. This technique permitted detection of as little as 1 μg fixed N plant^-1 in plant material and 40 μg fixed N plant^-1 in soil. No fixation of¹⁵N₂ occurred during either of the first two labelling periods. In the final labelling period, straw returned to the soil was significantly enriched in¹⁵N, especially in a pot with a higher soil moisture content. Total BNF in this pot was 13 μg N plant^-1, or about 30 g N ha^-1. In a separate experiment with soil from the same plot, we detected BNF only when soil was amended with glucose at a high soil moisture content. Measured associative BNF was insufficient to account for observed N gains under field conditions. Lethbridge Research Centre contribution no. 3879488. Lethbridge Research Centre contribution no. 3879488.     

Effect of salinity and its composition on the accumulation of selenium by alfalfa

Alfalfa (Medicago sativa L.) was grown in greenhouse sand culture to examine the effect of salinity composition and concentration on Se accumulation by plants. In a 2×2×4 factorial experiment, salinity was added as either C1⁻ or SO ₄ ²⁻ salts to the irrigating solution to achieve an electrical conductivity of 0.5, 1.5–3.0, or 6.0 dS m⁻¹. Selenium was added to the nutrient solution at a concentration of 0.25 or 1.0 mg Se(VI)I⁻¹. Following the third cutting, the roots were washed and all plant material analyzed for dry weight and Se. Plant biomass production decreased with additions of either Se or salinity, regardless of composition. In the presence of Se, the yield reduction was greater with Cl⁻ salinity than with SO ₄ ²⁻ salinity. Plant Se accumulation was reduced from 948 mg Se kg⁻¹ to 6 mg Se kg⁻¹ in the presence of SO ₄ ²⁻ salts (0.5 mmol SO ₄ ²⁻ l⁻¹ vs. 40 mmol SO ₄ ²⁻ l⁻¹) due to an apparent Se(VI) −SO ₄ ²⁻ antagonism. This Se−SO ₄ ²⁻ antagonism prevented accumulation of Se and reduced Se-induced toxicity. A lesser antagonistic effect on Se accumulation was observed between Cl⁻, and Se. A synergistic interaction between SO ₄ ²⁻ and Se(VI) increased plant S concentrations in the presence of the relatively low basal SO ₄ ²⁻ concentrations but not at the higher solution SO ₄ ²⁻ concentrations. In many areas, soil and water containing high Se concentrations also contain large amounts of SO ₄ ²⁻ . The occurrence of SO ₄ ²⁻ with Se reduces plant accumulation of Se(VI) and may lower the risk of Se overexposure to animals feeding on forage material grown in high Se−SO ₄ ²⁻ regions.     

Effect of Cl on Cd uptake by Swiss chard in nutrient solutions

Swiss chard (Beta vulgaris L., cv. Fordhook Giant) was grown in nutrient solution with Cl concentrations varying between 0.01 mM and 120 mM. Solution Na concentration and ionic strength were maintained in all treatments by compensating with NaNO₃. All solutions contained Cd (50 nM, spiked with ¹⁰⁹Cd). Three different Cd²⁺ buffering systems were used. In one experiment, Cd²⁺ activity was unbuffered; its activity decreased with increased Cl concentration as a result of the formation of CdCl_n ^2–n species. In the other experiments, Cd²⁺ activity was buffered by the chelator nitrilotriacetate (NTA, 50 M) and ethylene-bis-(oxyethylenenitrilo)-tetraacetate (EGTA, 50 M) at about 10^–9 M and 10^–11 M, respectively. Plant growth was generally unaffected by increasing Cl concentrations in the three experiments. In unbuffered solutions, Cd concentrations in plant tissue decreased significantly (p<0.01) (approximately 2.4-fold) as solution Cl concentration increased from 0.01 mM to 120 mM. However, this decrease was smaller in magnitude than the 4.7-fold decrease in Cd²⁺ activity as calculated by the GEOCHEM-PC program for the same range of Cl concentrations. In solutions where Cd²⁺ activity was buffered by NTA, Cd concentrations in plant tissue increased approximately 1.4-fold with increasing Cl concentration in solution, while the Cd²⁺ activity was calculated to decrease 1.3-fold. In solutions where Cd²⁺ activity was buffered by EGTA, Cd concentrations in the roots increased 1.3-fold with increasing Cl concentration in solution but there was no effect of Cl on shoot Cd concentrations. The data suggest that either CdCl_n ^2–nspecies can be taken up by plant roots or that Cl enhances uptake of Cd²⁺ through enhanced diffusion of the uncomplexed metal to uptake sites.Abbreviations DAS days after sowing - EGTA ethylene-bis-(oxyethylenenitrilo)-tetraacetate - HBED N,N-bis(2-hydroxybenzyl)-ethylenediamine-N,N-diacetate - NTA nitrilotriacetate     

Uptake and retention in suckling rats of51chromium fed with human milk or infant formulas

Optimum concentration of Cr for infant formulas has not been established. Such components as soy protein or supplemental Fe could influence absorption and retention. Suckling rat pups were used to evaluate the influence of three commercial formulas and human milk, all of which had been incubated with⁵¹CrCl₃ for 1 h, on the uptake and retention of the added⁵¹Cr. After fasting 3 h, the pups were intubated with a single dose of 25 μCi⁵¹CrCl₃ in either a cow's milk-based formula, an Fe-supplemented cow's milk-based formula, a soy-based formula, or human milk. Six hours later,⁵¹Cr was counted in five organs, thymus, blood, and total urine. Absorption of⁵¹Cr was low. At 6 h, percent⁵¹Cr in blood was <0.2% of the dose, and total⁵¹Cr excretion in urine was <1.8%. The uptake and retention of⁵¹Cr and its concentration in any of the organs, thymus, blood, and urine were not influenced by different types of formula or by human milk.     

Effect of water stress on subsequent uptake of chloride by wheat plants

Summary Wheat plants that were grown for 30 days in flowing nutrient solution were transferred to CaSO₄ solution, and water stress was developed by increasing the evaporative demand on the tops and decreasing the amount of the root system in the solution. The stress was maintained for 3 or 9 h. Uptake of³⁶Cl by the plants was measured immediately after removal of the stress and at intervals up to 36 h later.The water potential of the leaves ranged from –5 bar in the control to –12 bar in stressed plants. Stressed plants transpired less water after removal of the stress than did unstressed plants.Chloride uptake immediately after the removal of water stress was unaffected by the stress, but when measurements were made 36 h later previously stressed plants absorbed only 2 M h^–1 chloride compared to 7 M h^–1 for unstressed plants.     

Nitrogen and phosphorus cycling in relation to stand age of Eucalyptus regnans F. Muell

Lupins, canola, ryegrass and wheat fertilized with Na₂ ³⁵SO₄ and either ¹⁵NH₄Cl or K¹⁵NO₃(N:S=10:1), were grown in the field in unconfined microplots, and the sources of N and S (fertilizer, soil, atmosphere, seed) in plant tops during crop development were estimated. Modelled estimates of the proportion of lupin N derived from the atmosphere, which were obtained independently of reference plants, were used to calculate the proportion of lupin N derived from the soil. Total uptake of N and S and uptake of labelled N and S increased during crop development. Total uptake of S by canola was higher than lupins, but labelled S uptake by lupins exceeded uptake by canola. The form of N applied had no effect on uptake of labelled and unlabelled forms of N or S. Ratios of labelled to unlabelled S and ratios of labelled to unlabelled N derived from soil sources decreased during growth, and were less for S than for N for each crop at each sampling time. Although ratios of labelled to unlabelled soil-derived N were similar between crops at 155, 176 and 190 days after sowing, ratios of labelled to unlabelled S for lupins were higher than for the reference crops and declined during this period. The ratios of labelled to unlabelled S in lupins and the reference plants therefore bore no relationship either to ratios of labelled to unlabelled soil-derived N in the plants, or to total S uptake by the plants. Therefore the hypothesis that equal ratios of labelled N to unlabelled soil-derived N in legumes (Rleg) and reference plants (Rref) would be indicated by equal ratios of labelled to unlabelled S was not supported by the data. The results therefore show that the accuracy of reference plant-derived values of Rleg cannot be evaluated by labelling with ³⁵S.     

Diffusion du15N2 dans le sol pendant la mesure de fixation biologique de l'azote

Summary The kinetic of¹⁵N₂ diffusion has been measured in a system similar to that for the estimation of N₂ fixation in plant microorganism associations cultivated in soil. The¹⁵N₂ enrichment of the soil atmosphere reached an homogenous value one hour after injection of¹⁵N₂ and is identical to that obtained by calculation, indicating that no adsorption occurs in the soil particles.

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Diffusion du¹⁵N₂ dans le sol pendant la mesure de fixation biologique de l'azote

Résumé La cinétique de diffusion du¹⁵N₂ est mesurée sur un système identique à ceux pouvant être utilisés pour la mesure de fixation de l'azote chez les associations plantes-microorganismes cultivées sur sol. L'enrichissement homogène de l'atmosphère du sol est obtenu une heure environ après l'injection de¹⁵N₂ et correspond à l'enrichissement calculé, ce qui indique qu'aucune adsorption n'a lieu dans les particules du sol.

     

Assessing Nitrification and Denitrification in the Seine River and Estuary Using Chemical and Isotopic Techniques

Downstream from metropolitan Paris (France), a large amount of ammonium is discharged into the Seine River by the effluents of the wastewater treatment plant at Achères. To assess the extent of nitrification and denitrification in the water column, concentrations and isotopic compositions of ammonium (δ¹⁵N–NH₄⁺) and nitrate (δ¹⁵N–NO₃⁻, δ¹⁸O–NO₃⁻) were measured during summer low-flow conditions along the lower Seine and its estuary. The results indicated that most of the ammonium released from the wastewater treatment plant is nitrified in the lower Seine River and its upper estuary, but there was no evidence for water-column denitrification. In the lower part of the estuary, however, concentration and isotopic data for nitrate were not consistent with simple mixing between riverine and marine nitrate. A significant departure of the nitrate isotopic composition from what would be expected from simple mixing of freshwater and marine nitrates suggested coupled nitrification and denitrification in the water, in spite of the apparent conservative behavior of nitrate. Denitrification rates of approximately 0.02 mg N/L/h were estimated for this part of the estuary.     

Quantitative and Qualitative Aspects of Dissolved Organic Carbon Leached from Senescent Plants in an Oligotrophic Wetland

We conducted a series of experiments whereby dissolved organic matter (DOM) was leached from various wetland and estuarine plants, namely sawgrass (Cladium jamaicense), spikerush (Eleocharis cellulosa), red mangrove (Rhizophora mangle), cattail (Typha domingensis), periphyton (dry and wet mat), and a seagrass (turtle grass; Thalassia testudinum). All are abundant in the Florida Coastal Everglades (FCE) except for cattail, but this species has a potential to proliferate in this environment. Senescent plant samples were immersed into ultrapure water with and without addition of 0.1% NaN₃ (w/ and w/o NaN₃, respectively) for 36 days. We replaced the water every 3 days. The amount of dissolved organic carbon (DOC), sugars, and phenols in the leachates were analyzed. The contribution of plant leachates to the ultrafiltered high molecular weight fraction of DOM (>1 kDa; UDOM) in natural waters in the FCE was also investigated. UDOM in plant leachates was obtained by tangential flow ultrafiltration and its carbon and phenolic compound compositions were analyzed using solid state ¹³C cross-polarization magic angle spinning nuclear magnetic resonance (¹³C CPMAS NMR) spectroscopy and thermochemolysis in the presence of tetramethylammonium hydroxide (TMAH thermochemolysis), respectively. The maximum yield of DOC leached from plants over the 36-day incubations ranged from 13.0 to 55.2 g C kg⁻¹ dry weight. This amount was lower in w/o NaN₃ treatments (more DOC was consumed by microbes than produced) except for periphyton. During the first 2 weeks of the 5 week incubation period, 60–85% of the total amount of DOC was leached, and exponential decay models fit the leaching rates except for periphyton w/o NaN₃. Leached DOC (w/ NaN₃) contained different concentrations of sugars and phenols depending on the plant types (1.09–7.22 and 0.38–12.4 g C kg⁻¹ dry weight, respectively), and those biomolecules comprised 8–34% and 4–28% of the total DOC, respectively. This result shows that polyphenols that readily leach from senescent plants can be an important source of chromophoric DOM (CDOM) in wetland environments. The O-alkyl C was found to be the major C form (55±9%) of UDOM in plant leachates as determined by ¹³C CPMAS NMR. The relative abundance of alkyl C and carbonyl C was consistently lower in plant-leached UDOM than that in natural water UDOM in the FCE, which suggests that these constituents increase in relative abundance during diagenetic processing. TMAH thermochemolysis analysis revealed that the phenolic composition was different among the UDOM leached from different plants, and was expected to serve as a source indicator of UDOM in natural water. Polyphenols are, however, very reactive and photosensitive in aquatic environments, and thus may loose their plant-specific molecular characteristics shortly. Our study suggests that variations in vegetative cover across a wetland landscape will affect the quantity and quality of DOM leached into the water, and such differences in DOM characteristics may affect other biogeochemical processes.     

The bestrophin- and TMEM16A-associated Ca2+-activated Cl– channels in vascular smooth muscles

The presence of Ca²⁺-activated Cl^– currents (I_Cl(Ca)) in vascular smooth muscle cells (VSMCs) is well established. I_Cl(Ca) are supposedly important for arterial contraction by linking changes in [Ca²⁺]_i and membrane depolarization. Bestrophins and some members of the TMEM16 protein family were recently associated with I_Cl(Ca). Two distinct I_Cl(Ca) are characterized in VSMCs; the cGMP-dependent I_Cl(Ca) dependent upon bestrophin expression and the ‘classical’ Ca²⁺-activated Cl^– current, which is bestrophin-independent. Interestingly, TMEM16A is essential for both the cGMP-dependent and the classical I_Cl(Ca). Furthermore, TMEM16A has a role in arterial contraction while bestrophins do not. TMEM16A’s role in the contractile response cannot be explained however only by a simple suppression of the depolarization by Cl^– channels. It is suggested that TMEM16A expression modulates voltage-gated Ca²⁺ influx in a voltage-independent manner and recent studies also demonstrate a complex role of TMEM16A in modulating other membrane proteins.     

Use of anin situ labeling technique for the determination of seasonal14C distribution in Ponderosa pine

A¹⁴C labeling apparatus was developed to permit the labeling of four-year-old Ponderosa pine with¹⁴CO₂ in the field. The labeling system is a completely closed canopy system with¹⁴CO₂ monitored by a GM tube ratemeter apparatus. The level of¹⁴CO₂ corresponding to ambient levels is monitored by a microloggercomputer which controls a¹⁴CO₂ generating system. The generated¹⁴CO₂ is mixed in the canopy by circulating the atmosphere with 12V diaphram pumps. The portable system requires little operator attention. At approximately monthly intervals over a one-year period two four-year-old Ponderosa pine trees were labeled for three to five days using this labeling apparatus. After an assimilate distribution period, one tree was excavated and analyzed for¹⁴C distribution. During late spring and early summer most of the carbon assimilated (>60%) was found in the active growing tips and new needles, with little being allocated to the roots (<10%) or woody material (<20%). During mid to late fall there was an increase in root labeling along with an increase in carbon going to woody material. Over the winter period, most of the fixed carbon (65%) resided in the older leaves. The early spring labeling period showed another pulse of root labeling along with some labeling of woody tissues.