Bicarbonate-stimulated ATPase in the renal proximal tubule luminal (brush border) memebrane.

Brush border membranes of the rabbit renal tubule have an ATPase which was stimulated 60% by 50 mm HCO₃^?. The K_a for HCO₃^? was 36 mm. Kinetic studies of the “HCO₃^?-ATPase” indicate that HCO₃^? had no effect on the K_m for ATP and ATP did not alter the K_a for HCO₃^?. Several anions, notably SO₃^2?, also accelerated the rate of dephosphorylation of ATP. The V for “SO₃^2?-ATPase” was fivefold greater than that for “HCO₃^?-ATPase.” The K_a for SO₃^2? was 0.78 mm. Other anions including Cl^? and phosphates, did not enhance ATPase activity. Thus, of the anions present in the glomerular filtrate in appreciable concentrations only HCO₃^? stimulated the luminal membrane enzyme. The anion-stimulated ATPase activity increased sharply from pH 6.1 to 7.1 and moderately with higher pH. The renal ATPase was not inhibited by SCN^? nor methyl sulfonyl chloride and was relatively insensitive to oligomycin and quercetin. Carbonyl cyanide p-trifluoromethoxy phenylhydrazone increased the basal rate of the membranal ATPase, suggesting that the ATPase activity is limited by transmembrane H⁺ flux. Carbonic anhydrase significantly increased the HCO₃^?-stimulated ATPase activity. This increment was blocked by Diamox. These findings provide evidence consistent with the hypothesis that the brush border membrane ATPase is involved in the extrusion of H⁺ from tubular cell to lumen and support suggested interrelationships between HCO₃^?-stimulated ATPase, H⁺ secretion, and bicarbonate transport in the kidney.     

Element fluxes in watershed-lake ecosystems recovering from acidification: Čertovo Lake,the Bohemian Forest, 2001–2005

Fluxes of major ions and nutrients were measured in the watershed-lake ecosystem of a strongly acidified lake, ?ertovo jezero (?ertovo Lake), in the 2001 through 2005 hydrological years. Water balance was estimated from precipitation and throughfall amounts, and measured outflow from the lake. The average water input into and outflow from the watershed-lake ecosystem was 1461 mm and 1271 mm (40 L km^?2 s^?1), respectively, and the water residence time in the lake averaged 662 days. The ecosystem has been recovering from acidification since the late 1980s. Still, however, ?ertovo watershed was an average net source of 23 mmol m^?2 yr^?1 of SO ₄ ^2? . Nitrogen saturation of the watershed caused low retention of the deposited inorganic N (23% on average). After a dry summer in 2003 and a cold winter in 2004, the watershed became a net source of inorganic N (19 mmol m^?2 yr^?1). Nitrogen transformations and SO ₄ ^2? release were the dominant terrestrial sources of H⁺ (81 and 47 mmol m^?2 yr^?1, respectively) and the watershed was a net source of 42 mmol H⁺ m^?2 yr^?1. Ionic composition of tributaries showed seasonal variations with the most pronounced changes in NO ₃ ^? , base cations, DOC, and ionic Al (Al_i) concentrations. The in-lake biogeochemical processes reduced the incoming H⁺ by ～50% (i.e., neutralized on average 222 mmol H⁺ m^?2 yr^?1, on a lake-area basis). Denitrification, SO ₄ ^2? reduction, and photochemical and microbial decomposition of allochthonous organic matter were the most important in-lake H⁺ consuming processes (215, 85, and 122 mmol H⁺ m^?2 yr^?1, respectively), while hydrolysis of Al_i was the dominant H⁺ generating process (96 mmol H⁺ m^?2 yr^?1) in ?ertovo Lake. Photochemical liberation from organic complexes was an additional in-lake source of Al_i. The net in-lake retention or removal of nutrients (carbon, phosphorus, nitrogen, and silica) varied between 18% and 34% of their inputs.     

Element fluxes in watershed-lake ecosystems recovering from acidification: Plešné Lake,the Bohemian Forest, 2001–2005

Fluxes of major ions and nutrients were measured in the watershed-lake ecosystem of a strongly acidified lake, Ple?né jezero (Ple?né Lake), in the Czech Republic in hydrological years from 2001 through 2005. The lake is situated in a Norway spruce forest and has a steep watershed between elevations of 1090 and 1378 m. The average water input and output from the ecosystem was 1372 mm and 1157 mm (37 L km^?2 s^?1), respectively, and the water residence time averaged 306 days. Despite ecosystem recovery from acidification occurring since the late 1980s, the Ple?né watershed was an average net source of 25 mmol SO ₄ ^2? m^?2 yr^?1. Nitrogen saturation of the watershed caused low retention of the deposited inorganic N (< 44% on average) before 2004. Then, the watershed became a net source of 28–32 mmol m^?2 yr^?1 of inorganic N in the form of NO ₃ ^? due to climatic effects (a dry summer in 2003 and a cold winter in 2004) and forest dieback caused by a bark beetle attack in 2004. Nitrogen transformations and SO ₄ ^2? release were the dominant terrestrial sources of H⁺ (72 and 49 mmol m^?2 yr^?1, respectively) and the watershed was a net source of 24 mmol H⁺ m^?2 yr^?1. Ionic composition of surface inlets showed seasonal variations, with the most pronounced changes in NO ₃ ^? , ionic Al (Al_i), and DOC concentrations, while the composition of subsurface inlets was more stable. The in-lake biogeochemical processes reduced on average 59% of the incoming H⁺ (251 mmol H⁺ m^?2 yr^?1 on a lake-area basis). NO ₃ ^? assimilation and denitrification, photochemical and microbial decomposition of allochthonous organic acids, and SO ₄ ^2? reduction in the sediments were the most important aquatic H⁺ consuming processes (358, 121, and 59 mmol H⁺ m^?2 yr^?1, respectively), while hydrolysis of Al_i was the dominant in-lake H⁺ generating process (233 mmol H⁺ m^?2 yr^?1). Photochemical liberation from organic complexes was an additional in-lake source of Al_i. The net in-lake retention or removal of total phosphorus, total nitrogen, and silica were on average 50%, 27%, and 23%, respectively. The lake was a net source of NH ₄ ⁺ due to a cease in nitrification (pH < 5) and from NH ₄ ⁺ production by dissimilation exceeding its removal by assimilation.     

The excretion of hydrogen ion by the isolated amphibian skin: Effects of antidiuretic hormone and amiloride

H⁺ extrusion by the isolated skins of two amphibia, Rana ridibunda and Bufo bufo was studied in order to test for the presence of exchange mechanisms of the type Na⁺/H⁺ and Cl^?/HCO₃^?, which have been described in several epithelial structures. The preparations were mounted in chambers of the Ussing type, so that the short-circuit current could be used as a function of Na⁺ transport and the pH-stat technique was utilized to determine the rates of H⁺ extrusion under different experimental conditions. These conditions were either the withdrawal of the ions intervening in the mentioned exchanges (Cl^- or Na⁺, or the addition of drugs with well-known effects on Na⁺ uptake and transport (antidiuretic hormone and amiloride).In the frog skin, H⁺ excretion was detected in solutions containing either Cl^? or SO₄^2?, with identical rates. Again, Na⁺ substitution by Mg²⁺ had no effect on H⁺ excretion rates, neither did the suppression of Na⁺ influx by amiloride or its stimulation by antidiuretic hormone. These experiments were repeated with similar results in gland-free preparations of the epidermis of frog skin separated from the corion by the action of collagenase.Experiments in toad skin showed that H⁺ excretion could not be detected when Cl^? was present in the outer medium, but became apparent if an impermeant anion, SO₄^2?, was used. This observation is compatible with the existence of an exchange mechanism of the type Cl^?/HCO₃^?. Secondly, in these preparations H⁺ extrusion increased after stimulation with antidiuretic hormone and decreased when amiloride was used or when Na⁺ was substituted by Mg²⁺, suggesting that at least a fraction of the total H⁺ efflux is linked to Na⁺ influx. In the isolated frog skin this mechanism does not seem to be operative.     

Effect of sulphite on phosphoenolpyruvate carboxylase and malate formation in extracts of Zea mays

The effect of SO₃^2? on the activity of PEP-carboxylase and on subsequent malate formation has been studied in leaf extracts of Zea mays. PEP-carboxylase was assayed by incorporation of H¹⁴CO₃ - into oxaloacetate dinitrophenylhydrazone and by a spectrophotometric method. In contrast to ribulose diphosphate carboxylase, PEP-carboxylase was not inhibited by 10 mM SO₃^2? with respect to PEP. As was the case with ribulose diphosphate carboxylase, the activity of PEP-carboxylase was inhibited non-competitively with respect to Mg²⁺. However, the K_i value (84.5 mM) was found to be very high. With respect to HCO₃^?, like ribulose diphosphate carboxylase, PEP-carboxylase was inhibited competitively, but the K_i value (27 mM SO₃^2?) increased by about the same factor (× 9) as the K_m, (0·5 mM HCO₃^?) is decreased. This indicates that the replacement of HCO₃^? by SO₃^2?, common to both enzymes, is facilitated by decreasing the affinity of the enzyme for HCO₃^?. At substrate saturating conditions malate formation by the combined action of PEP-carboxylase and endogenous NADH-dependent malate dehydrogenase in leaf extracts was not inhibited by 10 mM SO₃^2?. Although the malate dehydrogenase is inhibited at this SO₃^2? concentration to about 85%, malate formation is unaffected, as PEP-carboxylase is the rate limiting step its turnover rate being only about 8% of NADH-dependent malate dehydrogenase.     

Trends in cation, nitrogen, sulfate and hydrogen ion concentrations in precipitation in the United States and Europe from 1978 to 2010: a new look at an old problem

Industrial emissions of SO₂ and NO_x, resulting in the formation and deposition of sulfuric and nitric acids, affect the health of both terrestrial and aquatic ecosystems. Since the mid-late 20th century, legislation to control acid rain precursors in both Europe and the US has led to significant declines in both SO₄–S and H⁺ in precipitation and streams. However, several authors noted that declines in streamwater SO₄–S did not result in stoichiometric reductions in stream H⁺, and suggested that observed reductions in base cation inputs in precipitation could lessen the effect of air pollution control on improving stream pH. We examined long-term precipitation chemistry (1978–2010) from nearly 30 sites in the US and Europe that are variably affected by acid deposition and that have a variety of industrial and land-use histories to (1) quantify trends in SO₄–S, H⁺, NH₄–N, Ca, and NO₃–N, (2) assess stoichiometry between H⁺ and SO₄–S before and after 1990, and (3) examine regional synchrony of trends. We expected that although the overall efforts of developed countries to reduce air pollution and acid rain by the mid-late 20th century would tend to synchronize precipitation chemistry among regions, geographically varied patterns of fossil fuel use and pollution control measures would produce important asynchronies among European countries and the United States. We also expected that control of particulate versus gaseous emission, along with trends in NH₃ emissions, would be the two most significant factors affecting the stoichiometry between SO₄–S and H⁺. Relationships among H⁺, SO₄–S, NH₄–N, and cations differed markedly between the US and Europe. Controlling for SO₄–S levels, H⁺ in precipitation was significantly lower in Europe than in the US, because (1) alkaline dust loading from the Sahara/Sahel was greater in Europe than the US, and (2) emission of NH₃, which neutralizes acidity upon conversion to NH₄ ⁺, is generally significantly higher in Europe than in the US. Trends in SO₄–S and H⁺ in precipitation were close to stoichometric in the US throughout the period of record, but not in Europe, especially eastern Europe. Ca in precipitation declined significantly before, but not after 1990 in most of the US, but Ca declined in eastern Europe even after 1990. SO₄–S in precipitation was only weakly related to fossil fuel consumption. The stoichiometry of SO₄–S and H⁺ may be explained in part by emission controls, which varied over time and among regions. Control of particulate emissions reduces alkaline particles that neutralize acid precursors as well as S-containing particulates, reducing SO₄–S and Ca more steeply than H⁺, consistent with trends in the northeastern US and Europe before 1990. In contrast, control of gaseous SO₂ emissions results in a stoichiometric relationship between SO₄–S and H⁺, consistent with trends in the US and many western European countries, especially after 1991. However, in many European countries, declining NH₃ emissions contributed to the lack of stoichiometry between SO₄–S and H⁺.Recent reductions in NO_x emissions have also contributed to declines in H⁺ in precipitation. Future changes in precipitation acidity are likely to depend on multiple factors including trends in NO_x and NH₃ emission controls, naturally occurring dust, and fossil fuel use, with significant implications for the health of both terrestrial and aquatic ecosystems.     

Growth,net photosynthesis and leaf nutrient status of <Emphasis Type="Italic">Fagus crenata</Emphasis> seedlings grown in brown forest soil acidified with H<Subscript>2</Subscript>SO<Subscript>4</Subscript> or HNO<Subscript>3</Subscript> solution

To obtain basic information for evaluating critical loads of acid deposition for protecting Japanese beech forests, growth, net photosynthesis and leaf nutrient status of Fagus crenata seedlings grown for two growing seasons in brown forest soil acidified with H₂SO₄ or HNO₃ solution were investigated. The whole-plant dry mass of the seedlings grown in the soil acidified by the addition of H₂SO₄ or HNO₃ solution was significantly less than that of the seedlings grown in the control soil not supplemented with H⁺ as H₂SO₄ or HNO₃ solution. However, the degrees of reduction in the whole-plant dry mass and net photosynthetic rate of the seedlings grown in the soil acidified by the addition of H⁺ as H₂SO₄ solution at 100 mg l^–1 on the basis of air-dried soil volume (S-100 treatment) were greater than those of the seedlings grown in the soil acidified by the addition of H⁺ as HNO₃ solution at 100 mg l^–1 (N-100 treatment). The concentrations of Al and Mn in the leaves of the seedlings grown in the S-100 treatment were significantly higher than those in the N-100 treatment. A positive correlation was obtained between the molar ratio of (Ca+Mg+K)/(Al+Mn) in the soil solution and the relative whole-plant dry mass of the seedlings grown in the acidified soils to that of the seedlings grown in the control soil. Based on the results, we concluded that the negative effects of soil acidification due to sulfate deposition are greater than those of soil acidification due to nitrate deposition on growth, net photosynthesis and leaf nutrient status of F. crenata, and that the molar ratio of (Ca+Mg+K)/(Al+Mn) in soil solution is a suitable soil parameter for evaluating critical loads of acid deposition in efforts to protect F. crenata forests in Japan.     

Interaction of benthic microalgae and macrofauna in the control of benthic metabolism, nutrient fluxes and denitrification in a shallow sub-tropical coastal embayment (western Moreton Bay, Australia)

Benthic biogeochemistry and macrofauna were investigated six times over 1 year in a shallow sub-tropical embayment. Benthic fluxes of oxygen (annual mean ?918 μmol O₂ m^?2 h^?1), ammonium (NH₄ ⁺), nitrate (NO₃ ^?), dissolved organic nitrogen, dinitrogen gas (N₂), and dissolved inorganic phosphorus were positively related to OM supply (N mineralisation) and inversely related to benthic light (N assimilation). Ammonium (NH₄ ⁺), NO₃ ^? and N₂ fluxes (annual means +14.6, +15.9 and 44.6 μmol N m^?2 h^?1) accounted for 14, 16 and 53 % of the annual benthic N remineralisation respectively. Denitrification was dominated by coupled nitrification–denitrification throughout the study. Potential assimilation of nitrogen by benthic microalgae (BMA) accounted for between 1 and 30 % of remineralised N, and was greatest during winter when bottom light was higher. Macrofauna biomass tended to be highest at intermediate benthic respiration rates (?1,000 μmol O₂ m^?2 h^?1), and appeared to become limited as respiration increased above this point. While bioturbation did not significantly affect net fluxes, macrofauna biomass was correlated with increased light rates of NH₄ ⁺ flux which may have masked reductions in NH₄ ⁺ flux associated with BMA assimilation during the light. Peaks in net N₂ fluxes at intermediate respiration rates are suggested to be associated with the stimulation of potential denitrification sites due to bioturbation by burrowing macrofauna. NO₃ ^? fluxes suggest that nitrification was not significantly limited within respiration range measured during this study, however comparisons with other parts of Moreton Bay suggest that limitation of coupled nitrification–denitrification may occur in sub-tropical systems at respiration rates exceeding ?1,500 μmol O₂ m^?2 h^?1.     

Kinetics of nitrate and ammonium absorption and accompanying H+ fluxes in roots of Lolium perenne L. and N2-fixing Trifolium repens L.

Kinetic parameters for NH₄⁺ and NO₃^? uptake were measured in intact roots of Lolium perenne and actively N₂-fixing Trifolium repens. Simultaneously, net H⁺ fluxes between the roots and the root medium were recorded, as were the net photosynthetic rate and transpiration of the leaves. A Michaelis–Menten-type high-affinity system operated in the concentration range up to about 500 mmol m^?3 NO₃^? or NH₄⁺. In L. perenne, the V_max of this system was 9–11 and 13–14 μmol g^?1 root FW h^?1 for NO₃^? and NH₄⁺, respectively. The corresponding values in T. repens were 5–7 and 2 μmol g^?1 root FW h^?1. The K_m for NH₄⁺ uptake was much lower in L. perenne than in T. repens (c. 40 compared with 170 mmol m^?3), while K_m values for NO₃^? absorption were roughly similar (around 130 mmol m^?3) in the two species. There were no indications of a significant efflux component in the net uptake of the two ions. The translocation rate to the shoots of nitrogen derived from absorbed NO₃^?-N was higher in T. repens than in L. perenne, while the opposite was the case for nitrogen absorbed as NH₄⁺. Trifolium repens had higher rates of transpiration and net photosynthesis than L. perenne. Measurements of net H⁺ fluxes between roots and nutrient solution showed that L. perenne absorbing NO₃^? had a net uptake of H⁺, while L. perenne with access to NH₄⁺ and T. repens, with access to NO₃^? or NH₄⁺, in all cases acidified the nutrient solution. Within the individual combinations of plant species and inorganic N form, the net H⁺ fluxes varied only a little with external N concentration and, hence, with the absorption rate of inorganic N. Based on assessment of the net H⁺ fluxes in T. repens, nitrogen absorption rate via N₂ fixation was similar to that of inorganic N and was not down-regulated by exposure to inorganic N for 2 h. It is concluded that L. perenne will have a competitive advantage over T. repens with respect to inorganic N acquisition.     

Daily Patterns under the Life Cycle of a Maize Crop

Together with photosynthesis, transpiration and respiration, the daily uptake of NO₃^?, NH₄⁺, H₂PO₄^?, K⁺, Ca²⁺, Mg²⁺, SO₄^2?, the root respiration, root volume increase and root excretions have been studied by daily measurements during the growth period of whole maize plants (Zea mays L. cv. INRA F7 × F2) raised until complete maturity on nutrient solution. The uptake patterns show a maximum absorption of NO₃^?, K⁺ and Ca²⁺ during the vegetative growth phase. The absorption of these ions declines during maturation while that of H₂PO₄^? reaches a maximum. Root respiration and particularly the uptake of NO₃^? and K⁺ are well correlated with the rate of root growth. Root excretion is more notable in young plants than in the old. It represents less than 0.2% of the net assimilation of adult plants.     

Contrasting responses of two Sitka spruce forest plots in Ireland to reductions in sulphur emissions: results of 20 years of monitoring

Long-term trends in ion concentrations of bulk precipitation, throughfall, forest floor leachate (humus water) and shallow and deep soil water were assessed at two Sitka spruce (Picea sitchensis) stands—one on an Atlantic peat bog in the west of Ireland (Cloosh), the other on the east coast on a peaty podzol (Roundwood). Deposition at Cloosh was dominated by marine ions (sodium, [Na⁺], chloride [Cl^?], and magnesium [Mg²⁺]), whereas bulk precipitation and throughfall at Roundwood was characterized by inputs of non-marine sulphate (nmSO₄ ^2?), acidity and inorganic nitrogen (NH₄ ⁺, NO₃ ^?). Significant declines in concentrations of nmSO₄ ^2? and acidity in bulk precipitation and throughfall were observed at both sites. The decline in throughfall nmSO₄ ^2? was significantly related to reductions in European sulphur dioxide (SO₂) emissions. At Roundwood, SO₄ ^2? declined significantly in humus, shallow and deep soil water. In deep soil water this was accompanied by a long-term increase in pH and a reduction in total aluminum (Al_tot). The recovery from acidification was delayed by high concentrations of NO₃ ^?, which strongly influenced acidity and Al_tot concentrations. At Cloosh, there was a significant decline in SO₄ ^2? in humus water but long-term trends were not evident in shallow or deep soil water; SO₄ ^2? concentrations at these depths fluctuated in response to drought-events. Marine ions strongly influenced soil water chemistry at both sites; at Cloosh soil water acidity was strongly related to Na⁺ and Cl^?, while at Roundwood, Na⁺, Cl^? and Mg²⁺ influenced Al_tot concentrations. Dissolved organic carbon increased significantly in humus and soil water at Roundwood, where it was associated with declining acidity. Soil water at both sites was influenced by a combination of anthropogenic sulphur (S) and nitrogen (N) deposition, drought and sea-salt events. The study highlights the value of long-term monitoring in assessing the response of forest soils to S and N deposition against a background of climate influences on soil water through drought and sea-salt events.     

CFTR-mediated anion secretion in parathyroid hormone-treated Caco-2 cells is associated with PKA and PI3K phosphorylation but not intracellular pH changes or Na+/K+-ATPase abundance

Parathyroid hormone (PTH) has previously been shown to enhance the transepithelial secretion of Cl^? and HCO₃^? across the intestinal epithelia including Caco-2 monolayer, but the underlying cellular mechanisms are not completely understood. Herein, we identified the major signaling pathways that possibly mediated the PTH action to its known target anion channel, i.e., cystic fibrosis transmembrane conductance regulator anion channel (CFTR). Specifically, PTH was able to induce phosphorylation of protein kinase A and phosphoinositide 3-kinase. Since the apical HCO₃^? efflux through CFTR often required the intracellular H⁺/HCO₃^? production and/or the Na⁺-dependent basolateral HCO₃^? uptake, the intracellular pH (pH_i) balance might be disturbed, especially as a consequence of increased endogenous H⁺ and HCO₃^? production. However, measurement of pH_i by a pH-sensitive dye suggested that the PTH-exposed Caco-2 cells were able to maintain normal pH despite robust HCO₃^? transport. In addition, although the plasma membrane Na⁺/K⁺-ATPase (NKA) is normally essential for basolateral HCO₃^? uptake and other transporters (e.g., NHE1), PTH did not induce insertion of new NKA molecules into the basolateral membrane as determined by membrane protein biotinylation technique. Thus, together with our previous data, we concluded that the PTH action on Caco-2 cells is dependent on PKA and PI3K with no detectable change in pH_i or NKA abundance on cell membrane.     

模拟酸沉降对鼎湖山季风常绿阔叶林地表径流水化学特征的影响

通过模拟酸沉降实验,研究了旱季期间(10-3月份)鼎湖山季风常绿阔叶林在4种不同pH模拟酸雨处理(对照、pH 4.0、pH 3.5、pH 3.0)下地表径流水化学输出特征.结果显示:(1)地表径流pH随酸处理强度增强呈“U”型变化模式,酸沉降对地表径流pH的影响不显著(P＞0.05),表明模拟酸沉降尚未引起地表水的酸化.(2)地表径流中NO3-、SO24-浓度随酸处理强度增强略有增加;HCO3-浓度的变化模式与地表径流pH类似.酸根离子浓度与地表径流pH相关性分析表明,SO24-、HCO3-有助于提高地表水抗酸化能力而NO3-则有助于促进地表水酸化.(3)地表径流中盐基离子对酸沉降的响应不尽相同.pH 3.0处理显著提高地表径流中Ca2+、Na+浓度;Mg2+浓度具有随酸处理梯度增强而增加的趋势;K+受模拟酸度的影响小.表明强酸(pH3.0)处理将导致土壤Na+、Ca2+、Mg2+盐基离子流失.(4)酸沉降具有诱发土壤可溶性有机碳(DOC)流失的倾向,增加地表水受有机污染的风险.     

Intra and interannual variability in the Madeira River water chemistry and sediment load

Concentrations of cations (Na⁺, Ca²⁺, Mg²⁺, K⁺, NH₄ ⁺), anions (HCO₃ ^?, Cl^?,?NO₃ ^?, SO₄ ^2?, PO₄ ^3?) and suspended sediments in the Madeira River water were?determined near the city of Porto Velho (RO), in order to assess variation in?water chemistry from 2004 to 2007. Calcium and bicarbonate were the dominant?cation and anion, respectively. Significant seasonal differences were found,?with highest concentrations occurring during the dry season, as expected from?the drainage of Andean carbonate-rich substratum. Interannual variations were?also observed, but became significant only when annual average discharge was?25% less than normal. Under this atypical discharge condition, bicarbonate was?replaced by sulfate, and higher suspended sediment concentrations and loads?were also observed. Compared to previously published studies, it appears that?no significant changes in water chemistry have occurred during the last 20?C30?years, although differences in approaches and sampling designs among this and previous studies may not allow detection of modest changes.?The calculated suspended sediment load reported here is close to the values presented elsewhere, reinforcing the relative importance of this river as a?sediment supplier for the Amazon Basin. Seasonality has a significant control?on the chemistry of Madeira River waters, and severe decrease in discharge due?to anthropogenic changes, such as construction of reservoirs or the occurrence?of drier years??a plausible consequence of global climate change??may lead?to modification in the chemical composition as well in the sediment deliver to?the Amazon River.     

The ascidian sperm reaction: evidence for Cl- and HCO3- involvement in acid release

Ascidia callosa sperm are triggered to undergo initiation of the sperm reaction (mitochondrial swelling) by increasing the pH or lowering the Na⁺ concentration of the medium. The optimal [Na⁺] for acid release is 20 mM with excellent correlation between acid release and initiation of morphological changes. Increasing the [K⁺] to around 20 mM inhibits acid release when applied up to 1 min after triggering the sperm but with less inhibition at 2 and 4 min, suggesting that K⁺ inhibits initiation of acid release rather than acid release itself. Acid release and the sperm reaction can also be triggered by Cl^?-free (NO^?₃ or glutamate substituted) seawater (SW). Cl^? efflux accompanies H⁺ efflux with twice as many Cl^? being released as H⁺. Both H⁺ and Cl^? release in Cl^?-free SW are dependent upon CO₂ being present in HCO^?₃-free medium, suggesting that H⁺ efflux is in part Cl^? and HCO^?₃-mediated. However, the chloride channel blocking agent SITS has no effect on H⁺ release and augments Cl^? release. Acid release results in a substantial increase in internal pH as determined by partitioning of 9-amino acridine. We envision acid release from ascidian sperm as involving two systems, the Na⁺-dependent acidification system of unreacted sperm and the Cl^?- and HCO^?₃-mediated H⁺ release at activation. The mechanism controlling acid release would then involve inactivation of the internal acidification process and activation of the chloride-bicarbonate-mediated alkalinization process.     

Atmospheric Deposition to the Turkey Lakes Watershed: Temporal Variations and Characteristics

We investigated the atmospheric concentrations and deposition fluxes of major ions to the Turkey Lakes Watershed (TLW) between 1980 and 1996. During that time, daily SO₄ ²⁻ concentrations in precipitation decreased markedly, while NO₃ ⁻, NH₄ ⁺, and H⁺ concentrations remained roughly constant. It appears that precipitation acidity did not decrease in spite of declining SO₄ ²⁻ concentrations due to a concurrent and counterbalancing decrease in the concentrations of Ca²⁺, Mg²⁺, and K⁺ in precipitation. The reasons for the decline in base cations are unknown, but this decline is probably related to decreasing emissions of soil-derived particles from agricultural, industrial, and road sources. A similar situation was seen during the same period in other parts of Canada, the eastern United States, and Europe. Wet, dry, and total (wet + dry) deposition fluxes of sulphur (S) and nitrogen (N) were estimated annually for the years 1980–96. The 17-year mean annual total (wet + dry) deposition of S to the watershed was estimated at 38.5 mmol m⁻² y⁻¹ (range 24.3–50.3). Total S deposition decreased by 35% from the early 1980s (1982–84) to the mid-1990s (1994–96), a decline consistent with the 23% decline in annual SO₂ emissions in eastern North America during the same period. In contrast, the annual total (wet + dry) deposition of oxidized N ranged from 39.8 to 60.4 mmol m⁻² y⁻¹, with a 15-year mean of 50.1 mmol m⁻² y⁻¹ and a net increase of 10% between the early 1980s (1983–85) and the mid-1990s (1994–96). This is in keeping with a 10% increase in NO_x emissions in eastern North America during the same period. For both S and N (oxidized), wet deposition dominated over dry deposition as the major mechanism for atmospheric input to the watershed. Annually, wet deposition accounted for approximately two-thirds of the total atmospheric deposition of both S and N. Dry S deposition was due more to gaseous SO₂ deposition (two-thirds of dry S deposition) than to particulate SO₄ ²⁻ deposition (one-third of dry S deposition). Dry deposition of oxidized N, however, was dominated (95%) by gaseous HNO₃ deposition, with minimal input from particulate NO₃ ⁻ deposition. Compared to several selected watershed/forest sites in Canada, the United States, and Europe, the estimated total deposition of S and N at the TLW was relatively high during the measurement period. Received 5 October 1999; accepted 1 March 2001.     

Understanding the gastrointestinal physiology and responses to feeding in air-breathing Anabantiform fishes

The Mekong Delta is host to a large number of freshwater species, including a unique group of facultative air-breathing Anabantiforms. Of these, the striped snakehead (Channa striata), the climbing perch (Anabas testudineus), the giant gourami (Osphronemus goramy) and the snakeskin gourami (Trichogaster pectoralis) are major contributors to aquaculture production in Vietnam. The gastrointestinal responses to feeding in these four species are detailed here. Relative intestinal length was lowest in the snakehead, indicating carnivory, and 5.5-fold greater in the snakeskin, indicating herbivory; climbing perch and giant gourami were intermediate, indicating omnivory. N-waste excretion (ammonia-N + urea-N) was greatest in the carnivorous snakehead and least in the herbivorous snakeskin, whereas the opposite trend was observed for net K⁺ excretion. Similarly, the more carnivorous species had a greater stomach acidity than the more herbivorous species. Measurements of acid–base flux to water indicated that the greatest postprandial alkaline tide occurred in the snakehead and a potential acidic tide in the snakeskin. Additional findings of interest were high levels of both PCO₂ (up to 40 mmHg) and HCO₃⁻ (up to 33 mM) in the intestinal chyme of all four of these air-breathing species. Using in vitro gut sac preparations of the climbing perch, it was shown that the intestinal net absorption of fluid, Na⁺ and HCO₃⁻ was upregulated by feeding but not net Cl⁻ uptake, glucose uptake or K⁺ secretion. Upregulated net absorption of HCO₃⁻ suggests that the high chyme (HCO₃⁻) does not result from secretion by the intestinal epithelium. The possibility of ventilatory control of PCO₂ to regulate postprandial acid–base balance in these air-breathing fish is discussed.     

Photosynthesis and inorganic carbon acquisition in the cyanobacterium Chlorogloeopsis sp. ATCC 27193

The ability of the morphologically complex cyanobacterium Chlorogloeopsis sp. ATCC 27193 to actively transport and accumulate inorganic carbon (C₁= CO₂+ HCO₃^?+ CO₃^2?) for photosynthetic CO₂ fixation was investigated. Mass-spectrometric assays revealed that Chlorogloeopsis cells grown under C₁ limitation rapidly took up CO₂ from the medium in a light-dependent reaction which was independent of CO₂ fixation. Ethoxyzolamide, a carbonic anhydrase (CA) inhibitor, inhibited CO₂ transport. Since electrometric and mass-spectrometric assays did not detect the presence of a periplasmic CA, it is suggested that CO₂ transport was mediated by a CA-like activity which converted CO₂ to HCO₃^? during passage across the membrane. Radiochemical assays, using H¹⁴CO₃ as substrate, showed that C₃-limited cells also had a high affinity (K_0.5 HCO₃^?= 37 μM), Na⁺-independent HCO₃^? uptake mechanism. HCO₃^?uptake was light dependent and occurred against its electrochemical potential indicating a carrier-mediated, active transport process. The rate of Na⁺-independent HCO₃^? transport was sufficient to account for the steady state rate of CO₂ fixation. Although not absolutely required. Na⁺ did specifically enhance the rate of HCO₃^? transport by up to 2-fold, but had no effect on the apparent affinity of the transport system for HCO₃^? Combined CO₂ and HCO₃^? transport resulted in C₁ accumulation as high as 25 mM and in excess of 300 times the external concentration. The C₁ pool was the source of CO₂ for photo-synthetic fixation and was generated, presumably, by the dehydration of HCO₃^? catalyzed by an intracellular CA. The collective evidence indicates that Chlorogloeopsis has a physiologically functional CO₂-concentrating mechanism which is essential for photosynthesis.     

Chemical composition and nutrient loading by precipitation in the Trachypogon savannas of the Orinoco llanos, Venezuela

Samples of bulk precipitation were collected in the Trachypogon savanna, Calabozo, Venezuela, during three consecutive years. In the first year, rain samples were taken daily; in the following years the samples were grouped on a monthly basis. In addition, samples of dry deposition were collected during the dry seasons. All samples were analyzed for the following water soluble cations and anions: P0₄-P, S0₄-S, N0₃-N, NH₄-N, Ca⁺², Mg⁺², K⁺, Na⁺ and H⁺. The mean annual input rate of chemical constituents (Kg ha^-1 year^-1) was: PO₄-P (0.42); SO₄-S (2.62); NO₃-N (0.21); NH₄-N (2.03); Ca₊₂ (3.50); Mg⁺² (11.31); K⁺ (3.60); Na⁺ (5.93) and H⁺ (0.03). The total mean input of particulate material to the savanna during the dry season was 2.06 Kg ha^-1 year^-1, with a soluble fraction of 30%. Possible sources of nutrients input were analyzed.     

Ribulose bisphosphate carboxylase and glycollate oxidase from jack pine: Effects of sulphur dioxide fumigation

Ribulose bisphosphate (RuBP) carboxylase and glycollate oxidase were partially purified from jack pine (Pinus banksiana Lamb.) needles. Preincubation of RuBP carboxylase with HCO₃^? and Mg²⁺ markedly stimulated its activity. RuBP carboxylase showed hyperbolic reaction kinetics with respect to HCO₃^?, Mg²⁺, and RuBP. Both SO₃^2- and SO₄^2- inhibited RuBP carboxylase, but SO₃^2- was more inhibitory than SO₄^2-. The SO₃^2- inhibition was competitive with respect to HCO₃^? (whether SO₃^2- was present during activation or was added to the activated enzyme), while the SO₄^2- inhibition was non-competitive with respect to HCO₃^?. Glycollate oxidase was inhibited more severely by low concentrations of SO₃^2- than by SO₄^2-. Fumigation of jack pine seedlings with 0.34 ppm sulphur dioxide for 24 and 48 hr produced a considerable decline in the activities of these enzymes, but 1 hr of fumigation produced no effect. During the longer exposures the sulphur content of the needles increased considerably, although the needles showed no visible injury. It is suggested that the accumulation of SO₃^2- and SO₄^2- in the needles following sulphur dioxide exposure influenced the enzyme activities.