Paleolimnological evidence for recent acidification of Big Moose Lake,Adirondack Mountains,N.Y. (USA)

Big Moose L. has become significantly more acidic since the 1950s, based on paleolimnological analyses of sediment cores. Reconstruction of past lakewater pH using diatom assemblage data indicates that from prior to 1800 to ca. 1950, lakewater pH was about 5.8. After the mid-1950s, the inferred pH decreased steadily and relatively quickly to about 4.6. Alkalinity reconstructions indicate a decrease of about 30 eq · l^-1 during the same period. There was a major shift in diatom assemblage composition, including a nearly total loss of euplanktonic taxa. Chrysophyte scale assemblages and chironomid (midge larvae remains also changed in a pattern indicating decreasing lakewater pH starting in the 1950s. Accumulation rates of total Ca, exchangeable and oxide Al, and other metals suggest recent lake-watershed acidification. Cores were dated using²¹⁰Pb, pollen, and charcoal. Indicators of watershed change (deposition rates of Ti, Si, Al) do not suggest any major erosional events resulting from fires or logging. Accumulation rates of materials associated with combustion of fossil fuels (polycyclic aromatic hydrocarbons, coal and oil soot particles, some trace metals, and sulfur) are low until the late 1800s-early 1900s and increase relatively rapidly until the 1920s–1930s. Peak rates occurred between the late 1940s and about 1970, when rates declined.The recent decrease in pH of Big Moose L. cannot be accounted for by natural acidification or processes associated with watershed disturbance. The magnitude, rate and timing of the recent pH and alkalinity decreases, and their relationship to indicators of coal and oil combustion, indicate that the most reasonable explanation for the recent acidification is increased atmospheric deposition of strong acids derived from combustion of fossil fuels.     

Manganese cycling in an acidic Adirondack lake

There is considerable interest in the chemistry of Mn in acidic waters because of its role in the generation of acid neutralizing capacity during reduction processes, as an adsorbent in element cycling, and as a potential toxicant to aquatic organisms. Temporal and spatial variations in the concentration of Mn were evident in acidic Dart's Lake (1.0–2.3 mol l^–1), located in the Adirondack Region of New York. Seasonal changes in pH and dissolved oxygen concentration had subtle effects on the chemistry and transport of Mn. Despite oversaturation with respect to the solubility of manganite during periods of stratification, vertical deposition of Mn was minimal. The conservative nature of Mn appears to be due to the acidic conditions in Dart's Lake.     

The oxidation of extracellular NADH by sugarcane cells: Coupling to ferricyanide reduction,oxygen uptake and pH change

Suspension-cultured cells of sugarcane (Saccharum sp. hybrids) did not oxidize exogenously supplied NADH in the absence of ferricyanide (potassium hexacyanoferrate [III]), whereas they did at a low rate in the presence of ferricyanide. Concomitantly, ferricyanide was reduced at a slow rate. Neither a pH change nor a change in respiration was caused by the addition of NADH and-or ferricyanide, but ferricyanide was a strong inhibitor of sugar transport. In contrast to cells, protoplasts rapidly oxidized exogenous NADH. This oxidation was accompanied by an increase in oxygen consumption and a net proton disappearance from the medium. Exogenous ferricyanide was reduced only slowly by protoplasts. Simultaneous presence of NADH and ferricyanide produced two effects: 1) a very rapid stoichiometric oxidation of NADH and reduction of ferricyanide until one of the reaction compounds was exhausted, and 2) a nearly instantaneous inhibition of the slower phase of NADH oxidation, which was observed in the presence of NADH but absence of ferricyanide. The extra oxygen consumption and the alkalinization of the medium, as observed with NADH, were also immediately stopped by ferric ions and ferrous ions. The presence of NADH and ferricyanide caused a fast stoichiometric acidification of the medium. These results were taken as evidence that the oxidation of NADH in the absence of ferricyanide is not related to the NADH-ferricyanide-coupled redox reaction. Furthermore, addition of NADH caused some uncoupling of the protoplasts, an effect which would explain the strong acidification of the cell cytoplasm and the inhibition of various transport systems. The NADH-oxidizing systems oxidized both the -configurated pyridine nucleotide and the -configurated form. Since NADH-linked dehydrogenases usually do not work with -NADH (with the exception of the endoplasmic-reticulum-bound electron-transport system), the observed activities could have been derived from contaminating membranes and dying protoplasts in the suspension. All reported reactions partly or predominantly occurred in the supernatant of the protoplast suspension and increased considerably during incubation of the protoplasts. The rates and quantities of oxygen consumption, pH change, and ferricyanide reduction fitted with NADH oxidation in a stoichiometric ratio, which implied that all these reactions occurred in the extracellular space, without involving transmembrane steps. No evidence for a physiological role in energization of the plasmalemma was found.Abbreviation NADH -nicotinamide adenine dinucleotide reduced form     

Nitrate reductase activity in nodules of pea inoculated with hydrogenase positive and hydrogenase negative strains of Rhizobium leguminosarum

The nitrate reductase (NR, EC 1.6.6.1) activity in root nodules formed by hydrogenase positive (Hup⁺) and hydrogenase negative (Hup⁻) Rhizobium leguminosarum strains was examined in symbioses with the pea cultivar Alaska ( Pisum sativum L.), Rates of activity were determined by the in vivo assay in nodules from plants that were only N₂-dependent or grown in the presence of 2 m M KNO₃. The rates varied widely among strains, regardless of the Hup phenotype of the R. leguminosarum strain used for inoculation, but the overall results indicated that nodules formed by Hup⁻ strains accumulated more nitrite in the incubation medium than did those with Hup⁻ phenotypes. Total plant dry weight and reduced nitrogen content of pea plants grown in the presence of 2 m M KNO₃ and inoculated with single Hup⁺ and Hup⁻ R. leguminosarum strains were statistically different among some strains. These observations suggest that the possible advantages derived from the presence of the Hup system on whole plant growth may be counteracted by the higher rates of NR activity in the Hup⁻ strains in the R. leguminosarum -pea symbiosis.     

Rhizobium strain effects on pea: The relation between nitrogen accumulation, phosphoenolpyruvate carboxylase activity in nodules and asparagine in root bleeding sap

Pisum sativum L. cv. Bodil was infected with various strains of Rhizobium leguminosarum (R501, 128c53, B155, 18a or 1044). The Rhizobium genotype influenced the activity of the plant enzyme phosphoenoipyruvate (PEP) carboxylase (EC 4.1.1.31), and the assimilation of fixed N in the root nodules. The specific activity of nodule PEP carboxylase was lowest in the symbioses, which accumulated the least total N (R501 and 128c53). The root bleeding sap of the less effective symbioses contained a lower proportion of asparagine and a higher proportion of glutamine than the more effective symbioses (B155,18a and 1044). The N yield of the symbioses was related neither to the net respiratory CO₂ evolution of the root system nor to the nitrogenase linked nodule respiration. The lower yielding symbioses accumulated a larger proportion of the fixed N in the nodules due to a higher proportion of total dry weight contained in the nodule tissue. However, the concentration of soluble protein in the nodules of the lower-yielding symbioses was lower than that recorded for the higher yileding symbioses. The effect of the Rhizobium strains on N yield was maintained at maturity, and reflected in seed yields.     

Chromosome aberration and ploidy equilibrium of Vicia faba in tissue culture

Summary Different phytohormone concentrations induced different fequencies of various chromosome aberrations in calli of Vicia faba. NAA 10 ppm plus KT 2.5 ppm produced more haploids and NAA 30 ppm plus NAA 7.5 ppm produced more tetraploids and breakage. The relationship among the aberrations was analyzed. The hypothesis of ploidy equilibrium was established. The chromosome doubling rate and reduction rate of each treated group were calculated in relation to the observed data and the hypothesis. The frequency of tetraploids and breakage are correlated with each other. The frequency of total aberrations is linearly correlated with that of micronucleus formation. The regression equation is x=31.92+ 10.67 y.     

Glycerol and dihydroxyacetone dissimilation in Desulfovibrio strains

During growth on glycerol two marine Desulfovibrio strains that can grow on an unusually broad range of substrates contained high activities of glycerol kinase, NAD(P)-independent glycerol 3-phosphate dehydrogenase and the other enzymes necessary for the conversion of dihydroxyacetone phosphate to pyruvate. Glycerol dehydrogenase and a specific dihydroxyacetone kinase were absent. During growth on dihydroxyacetone, glycerol kinase is involved in the initial conversion of this compound to dihydroxyacetone phosphate which is then further metabolized. Some kinetic properties of the partially purified glycerol kinase were determined. The role of NAD as electron carrier in the energy metabolism during growth of these strains on glycerol and dihydroxyacetone is discussed.Glycerol also supported growth of three out of four classical Desulfovibrio strains tested. D. vulgaris strain Hildenborough grew slowly on glycerol and contained glycerol kinase, glycerol 3-phosphate dehydrogenase and enzymes for the dissimilation of dihydroxyacetone phosphate. In D. gigas which did not grow on glycerol the enzymes glycerol kinase and glycerol 3-phosphate dehydrogenase were absent in lactate-grown cells.Abbreviations DHA dihydroxyacetone - DHAP dihydroxyacetone phosphate - G3P glycerol 3-phosphate - GAP glyceraldehyde 3-phosphate - 3-PGA 3-phosphoglycerate - 2-PGA 2-phosphoglycerate - 2,3-DPGA 2,3-diphosphoglycerate - PEP phosphoenolpyruvate - DH dehydrogenase - GK glycerol kinase - DHAK dihydroxyacetone kinase - TIM triosephosphate isomerase - PGK 3-phosphoglycerate kinase - PK pyruvate kinase - LDH lactate dehydrogenase - DTT dithiotreitol - HEPES 4-(2-hydroxyethyl)-1-piperazine ethane sulfonic acid - PIPES piperazine-1,1-bis(2-ethane sulfonic acid) - BV²⁺/BV⁺ oxidized/reduced benzylviologen - PMS phenazine methosulfate - DCPIP 2,6-dichlorophenolindophenol - MTT 3-(4,5-dimethylthiazol-2-yl)-2,4-diphenyltetrazolium bromide     

Rhizobium meliloti inoculation of alfalfa selected for tolerance to acid,aluminum-rich soils

Alfalfa (Medicago sativa L.) growth and nodulation in acid soil is reduced because the plant and its bacterial symbiontRhizobium meliloti cannot tolerate acid, aluminum-rich soil. A study was conducted to determine if a relatively acid-tolerant alfalfa germplasm combined with a relatively acid-tolerantR. meliloti strain could overcome these limitations. In a light room study, an acid-tolerant alfalfa germplasm inoculated with a more acid-tolerantR. meliloti strain produced greater top growth, nodule number and weight, and acetylene reduction values in an unlimed soil (pH 4.6) than the same germplasm inoculated with a relatively acid-sensitiveR. meliloti strain or an acid-sensitive germplasm inoculated with either a relatively acid-tolerant or acid-sensitiveR. meliloti strain.     

Nitrite reduction and carbohydrate metabolism in plastids purified from roots of Pisum sativum L.

Nitrate reduction in roots and shoots and exchange of reduced N between organs were quantitatively estimated in intact 13-d-old seedlings of two-row barley (Hordeum vulgare L. cv. Daisengold) using the ¹⁵N-incorporation model (A. Gojon et al. (1986) Plant Physiol. 82, 254–260), except that NH ₊ ⁴ was replaced by NO _- ² . N-depleted seedlings were exposed to media containing both nitrate (1.8 mM) and nitrite (0.2 mM) under a light-dark cycle of 12:12 h at 20°C; the media contained different amounts of ¹⁵N labeling. Experiments were started either immediately after the beginning (expt. 1) or immediately prior to the end (expt. 2) of the light period, and plants were sampled subsequently at each light-dark transition throughout 36 h. The plants effectively utilized ¹⁵NO _- ³ and accumulated it as reduced ¹⁵N, predominantly in the shoots. Accumulation of reduced ¹⁵N in both experiments was nearly the same at the end of the experiment but the accumulation pattern in roots and shoots during each 12-h period differed greatly depending on time and the light conditions. In expt. 1, the roots accounted for 31% (light), 58% (dark), and 9% (light) of nitrate reduction by the whole plants, while in expt. 2 the contributions of the root were 82% (dark), 20% (light), and 29% (dark), during each of the three 12-h periods. Xylem transport of nitrate drastically decreased in the dark, but that of reduced N rather increased. The downward translocation of reduced ¹⁵N increased while nitrate reduction in the root decreased, whereas upward translocation decreased while nitrate reduction in the shoot increased. We conclude that the cycling of reduced N through the plant is important for N feeding of each organ, and that the transport system of reduced N by way of xylem and phloem, as well as nitrate reduction by root and shoot, can be modulated in response to the relative magnitude of reduced-N demands by the root and shoot, with the one or the other predominating under different circumstances.Symbols Anl accumulation of reduced ¹⁵N from ¹⁵NO _- ³ in ¹⁴NO _- ³ -fed roots of divided root system - Ar accumulation in root of reduced ¹⁵N from ¹⁵NO _- ³ - As accumulation in shoot of reduced ¹⁵N from ¹⁵NO _- ³ - Rr ¹⁵NO _- ³ reduction in root - Rs ¹⁵NO _- ³ reduction in shoot - Tp translocation to root of shoot-reduced ¹⁵N from ¹⁵NO _- ³ in phloem - Tx translocation to shoot of root-reduced ¹⁵N from ¹⁵NO _- ³ in xylem     

Citric acid excretion and precipitation of calcium citrate in the rhizosphere of white lupin (Lupinus albus L.)

Abstract. White lupin ( Lupinus albus L.) was grown for 13 weeks in a phosphorus (P) deficient calcareous soil (20% CaCO₃, pH(H₂O)7.5) which had been sterilized prior to planting and fertilized with nitrate as source of nitrogen. In response to P deficiency, proteoid roots developed which accounted for about 50% of the root dry weight. In the rhizosphere soil of the proteoid root zones, the pH dropped to 4.8 and abundant white precipitates became visible. X-ray spectroscopy and chemical analysis showed that these precipitates consisted of calcium citrate. The amount of citrate released as root exudate by 13-week-old plants was about 1 g plant⁻¹, representing about 23% of the total plant dry weight at harvest. In the rhizosphere soil of the proteoid root zones the concentrations of available P decreased and of available Fe, Mn and Zn increased. The strong acidification of the rhizosphere and the cation/anion uptake ratio of the plants strongly suggests that proteoid roots of white lupin excrete citric acid, rather than citrate, into the rhizosphere leading to intensive chemical extraction of a limited soil volume. In a calcareous soil, citric acid excretion leads to dissolution of CaCO₃ and precipitation of calcium citrate in the zone of proteoid roots.