Leaf δ<Superscript>13</Superscript>C variability with elevation,slope aspect,and precipitation in the southwest United States

Leaves from several desert and woodland species, including gymnosperms and angiosperms with both C₃ and C₄ physiology, were analyzed to detect trends in '¹³C_leaf with elevation and slope aspect along two transects in southeastern Utah and south-central New Mexico, USA. The main difference between the two transects is the steeper elevational gradient for mean annual and summer precipitation in the southern transect. For any given species, we found that isotopic differences between individual plants growing at the same site commonly equal differences measured for plants along the entire altitudinal gradient. In C₃ plants, '¹³C_leaf values become slightly enriched at the lowest elevations, the opposite of trends identified in more humid regions. Apparently, increasing water-use efficiency with drought stress offsets the influence of other biotic and abiotic factors that operate to decrease isotopic discrimination with elevation. For some species shared by the two transects (e.g., Pinus edulis and Cercocarpus montanus), '¹³C_leaf values are dramatically depleted at sites that receive more than 550 mm mean annual precipitation, roughly the boundary (pedalfer-pedocal) at which soils commonly fill to field capacity in summer and carbonates are leached. We hypothesize that, in summer-wet areas, this may represent the boundary at which drought stress overtakes other factors in determining the sign of '¹³C_leaf with elevation. The opposition of isotopic trends with elevation in arid versus humid regions cautions against standard correction for elevation in comparative studies of '¹³C_leaf.     

13C/12C Ratios of carbon dioxide from peanut and sunflower seedlings and tobacco leaves in light and in darkness

Shoots of intact peanut and sunflower seedlings evolved CO₂in the light which was enriched more than 10 per mille in ¹³Ccompared with simultaneous CO₂ evolution from the roots. Carbondioxide collected from tobacco leaves in the light was 10 permille enriched in ¹³C compared with that collected in the dark.Anaerobic conditions inhibited photorespiration but did notchange isotopic ratios of dark respiration. ¹ Department of Biology, Fresno State College, Fresno, California93710, U. S. A. ² Deceased. (Received February 29, 1972; )     

Dynamics of Carbon Photosynthetically Assimilated in Nodulated Soya Bean Plants under Steady-state Conditions 1. Development and Application of 13CO2 Assimilation System at a Constant 13C Abundance

A long-term, steady-state ¹³CO₂ assimilation system at a constantCO₂ concentration with a constant ¹³C abundance was designedand applied to quantitative investigations on the allocationof photoassimilated carbon in nodulated soya bean (Glycine maxL.) plants. The CO₂ concentration in the assimilation chamberand its ¹³C abundance were maintained constant with relativevariances of less than ±0.5 per cent during an 8-h assimilationperiod. At the termination of 8-h ¹³CO₂ assimilation by plantsat early flowering stage, the currently assimilated carbon relativeto total tissue carbon (measured by the degree of isotopic saturation)were for young leaves (including flower buds), 13.9 per cent;mature leaves, 15.7 per cent; stems+petioles, 5.9 per cent;roots, 5.4 per cent and nodules, 6.9 per cent, 48 h after theend of the ¹³CO₂ assimilation period, they were 12.3, 7.5, 7.4,6.8 and 6.1 per cent, respectively. The treatment with a highconcentration of nitrate in the nutrient media significantlydecreased the allocation of ¹³C into nodules. Experiments on¹³CO₂ assimilation by plants at the pod-filling stage were alsoconducted. Labelling by ¹³C was weaker than at the early floweringstage, but an intense accumulation of ¹³C into reproductiveorgans was observed. Glycine max L., nodulated soya bean plants, ¹³CO₂ assimilation, carbon dynamics     

The Uptake and Transport of Chromium by Barley Seedlings (Hordeum vulgare L.)

Uptake of ⁵¹CrO^2–₄ by intact barley seedlings was linearover 24 h and was stimulated by Ca2⁺ but inhibited by SO^2–₄and other Group VI anions. Uptake increased with increasingchromate concentration, but unless the concentration was high(100 µM) less than 1 per cent of the isotope absorbedwas transported to the shoots. The results of solvent extraction,subcellular fractionation and efflux studies indicated thatmost of the isotope accumulated by the roots was present ina soluble non-particulate form in the vacuoles. The possiblereasons for the restriction in chromate transport are discussedin relation to the metabolism of the element.     

Phosphate Uptake in the Cyanobacterium Synechococcus R-2 PCC 7942

Phosphate uptake rates in Synechococcus R-2 in BG-11 media (anitrate-based medium, not phosphate limited) were measured usingcells grown semi-continuously and in continuous culture. Netuptake of phosphate is proportional to external concentration.Growing cells at pH_o 10 have a net uptake rate of about 600pmol m^–2 s^–1 phosphate, but the isotopic flux for³²P phosphate was about 4 nmol m^–2 s^–1. There appearsto be a constitutive over-capacity for phosphate uptake. TheK_m and V_max, of the saturable component were not significantlydifferent at pH_o 7.5 and 10, hence the transport system probablyrecognizes both H₂PO^–₄and HPO^2–₄. The intracellularinorganic phosphate concentration is about 3 to 10 mol m^–3,but there is an intracellular polyphosphate store of about 400mol m^–3. Intracellular inorganic phosphate is 25 to 50kJ mol^–1 from electrochemical equilibrium in both thelight and dark and at pH_o 7.5 and 10. Phosphate uptake is veryslow in the dark ( 100 pmol m^–2 s^–1) and is light-activated(pH_o 7.51.3 nmol m^–2 s^–1, pH_o 10600 pmol m^–2s^–1). Uptake has an irreversible requirement for Mg²⁺in the medium. Uptake in the light is strongly Na⁺-dependent.Phosphate uptake was negatively electrogenic (net negative chargetaken up when transporting phosphate) at pH_o 7.5, but positivelyelectrogenic at pH_o 10. This seems to exclude a sodium motiveforce driven mechanism. An ATP-driven phosphate uptake mechanismneeds to have a stoichiometry of one phosphate taken up perATP (1 PO_{4 in}/ATP) to be thermodynamically possible under allthe conditions tested in the present study. (Received June 16, 1997; Accepted September 4, 1997)     

Respiratory Utilization of 13C-Labelled Photosynthate in Nodulated Root Systems of Soybean Plants

Kouchi, H., Akao, S. and Yoneyama, T. 1986. Respiratory utilizationof ¹³C-labelled photosynthate in nodulated root systems of soybeanplants.—J. exp. Bot. 37: 985–993. An improved method for the measurement of respiratory utilizationof current photosynthate in the nodulated root system of water-culturedsoybean (Glycine max L.) plants was developed using a steady-state¹³CO₂ labelling technique. Well-nodulated plants at the latevegetative stage were allowed to assimilate ¹³CO₂ for 10 h incontinuous light at a constant CO₂ concentration with a constant¹³C abundance. The respiratory evolution of ¹³CO₂ from rootsand nodules was measured continuously throughout the periodof ¹³CO₂ assimilation and during a subsequent 36 h chase periodby using a differential infrared ¹³CO₂ analyser. The plantswere grown with nitrogen-free or (15 mmol dm^–3)-containing culture solution for 3 d before¹³CO₂ assimilation. In plants grown without , nodule respiration averaged 69% of the total respiration of the undergroundparts over the full experimental period and the CO₂ respiredreached an apparent isotopic equilibrium at 80–85% labellingafter initiating ¹³CO₂ assimilation. By contrast, the CO₂ respiredfrom the roots did not reach an isotopic equilibrium and labellingwas only 56% at the end of exposure to ¹³CO₂ These findingsdemonstrated that nodule respiration is strongly dependent onrecently assimilated carbon compared with root respiration. Plants supplied with in the culture solution showed a decreased rate of nodule respirationand a slightly increased rate of root respiration. The extentsand time courses of labelling of respired CO₂ from both theroots and nodules were similar in the presence and absence of except that the maximum level of labelling of CO₂ derived from nodule respiration in plantswith was significantly higher (about 91%) than for plants growing without . Key words: Soybean (Glycine max L.), nodule respiration, ¹³CO₂, assimilation, carbon partitioning     

Biogeochemistry of platelet ice: its influence on particle flux under fast ice in the Weddell Sea, Antarctica

An array of four sediment traps and one current meter was deployed under a well-developed platelet layer for 15 days in the Drescher Inlet in the Riiser Larsen ice shelf, in February 1998. Traps were deployed at 10 m (just under the platelet layer), 112 m (above the thermocline), 230 m (below thermocline) and 360 m (close to sea floor). There was a substantial flux of particulate organic material out of the platelet layer, although higher amounts were collected in the traps either side of the thermocline. Material collected was predominantly composed of faecal pellets containing diatom species growing within the platelet layer. The size classes of these pellets suggest they derive from protists grazing rather than from larger metazoans. Sediment trap material was analysed for particulate organic carbon/nitrogen/phosphorus (POC/PON/POP) and '¹³C_POC (carbon isotopic composition of POC). These were compared with organic matter in the overlying platelet layer and the water column. In turn, the biogeochemistry of the platelet layer and water column was investigated and the organic matter characteristics related to inorganic nutrients (nitrate, nitrite, ammonium, silicate, phosphate), dissolved organic carbon/nitrogen (DOC/DON), pH, dissolved inorganic carbon (DIC), oxygen and '¹³C_DIC (carbon isotopic composition dissolved inorganic carbon).     

13C content of ecosystem respiration is linked to precipitation and vapor pressure deficit

Variation in the carbon isotopic composition of ecosystem respiration ('¹³C_R) was studied for 3 years along a precipitation gradient in western Oregon, USA, using the Keeling plot approach. Study sites included six coniferous forests, dominated by Picea sitchensis, Tsuga heterophylla, Pseudotsuga menziesii, Pinus ponderosa, and Juniperus occidentalis, and ranged in location from the Pacific coast to the eastern side of the Cascade Mountains (a 250-km transect). Mean annual precipitation across these sites ranged from 227 to 2,760 mm. Overall '¹³C_R varied from -23.1 to -33.1‰, and within a single forest, it varied in magnitude by 3.5-8.5‰. Mean annual '¹³C_R differed significantly in the forests and was strongly correlated with mean annual precipitation. The carbon isotope ratio of carbon stocks (leaves, fine roots, litter, and soil organic matter) varied similarly with mean precipitation (more positive at the drier sites). There was a strong link between '¹³C_R and the vapor saturation deficit of air (vpd) 5-10 days earlier, both across and within sites. This relationship is consistent with stomatal regulation of gas exchange and associated changes in photosynthetic carbon isotope discrimination. Recent freeze events caused significant deviation from the '¹³C_R versus vpd relationship, resulting in higher than expected '¹³C_R values.     

Soil nitrogen form and plant nitrogen uptake along a boreal forest productivity gradient

We present results from a study of soil solution concentrations of ammonium (NH₄⁺), nitrate (NO₃^-), and amino acid N over one growing season along a local 90-m-long plant productivity gradient in a boreal forest. Three forest types are found along the gradient: an ericaceous dwarf-shrub type between 0 and 40 m, a low-herb type between 40 and 80 m, and a tall-herb type at 90 m. Soil sampling of the mor layer was performed in June, July, August and October in the three forest types. In addition, plant uptake of NH₄⁺, NO₃^- and the amino acid glycine was investigated. A mixture of the three N forms was injected into the soil; one N form at a time was labeled with ¹⁵N, and in the case of glycine also with ¹³C. In the dwarf-shrub forest, where plant productivity was low, the soil N pool was strongly dominated by amino acid N. There, plants took up more NH₄⁺ than NO₃^-. Glycine uptake did not differ significantly from either NH₄⁺ or NO₃^- uptake. Along the gradient, soil concentrations of NH₄⁺ and NO₃^- increased, as did plant productivity. In the low-herb forest NH₄⁺ comprised a major portion of the soil N pool, and plants took up more NH₄⁺ than NO₃^- or glycine. In the tall-herb forest, NO₃^- was as abundant as NH₄⁺, and together these two N forms dominated the soil N pool. Here, plants took up nearly equal amounts of NO₃^- and NH₄⁺, and this uptake exceeded that of glycine severalfold. Apart from the overall preference for NH₄⁺ that plants exhibited throughout the gradient, the results show a correlation between soil concentrations of amino acids and NO₃^- and plant preferences for these N forms.     

A novel 13C isotopic labelling strategy for probing the structure and dynamics of glycan chains in situ on glycoproteins

A protocol is described for uniform ¹³C labelling of terminalgalactose residues of the glycan chains of glycoproteins, usingan enzymatic method which does not perturb the protein. Thetechnique is illustrated by application to the biantennary N-linkedglycan chains attached at Asn 297 of immunoglobulin G (IgG).Isotope-edited NMR experiments on this glycoprotein yield datawhich suggest that the galactose residues on the glycan existin two discrete environments, with the galactose in one environmenthaving greater mobility than that in the other. These data arequalitatively consistent with crystallographic data on an Fcfragment, which suggest that one arm of the glycan is in contactwith the protein, while the other projects into the space betweenthe C2 domains. Quantitatively, however, these data cannot berationalized with the crystallographic data, which implies subtledifferences in oligosaccharide structure and dynamics betweenthe solution and crystal states of Fc. dynamics glycoprotein glycans in situ ¹³C isotopic labelling structure     

N2O Reduction by Azotobacter vinelandii with Emphasis on Kinetic Nitrogen Isotope Effects

A nitrogen-fixing bacterium Azotobacter vinelandii was successfullygrown in a specially designed system with constant partial pressuresof N₂O (0.2 atm) and O₂ (0.2 atm) in a nitrogen-free liquidmedium. Reduction of N₂O proceeded with the evolution of N₂in the gas phage. Large nitrogen isotope fractionation was found for both processes,reduction of N₂O to N₂ and N₂O-fixation. The kinetic isotopefractionation factors of these reactions were at most 1.039and 1.034, respectively. Furthermore, an unexpected inverseisotope effect (organic-N, the end-product, is more enrichedin ¹⁵N than N₂, the intermediate) strongly suggested that N₂Owas directly assimilated within the bacterial cells. Simultaneousassimilation of N₂O and N₂ was also confirmed by using a ¹⁵Ntracer technique. Three independent pathways were demonstrated for the nitrogenfixing system investigated in this study: (1) a direct reductionof N₂O to ammonium (apparently 8-electron reduction), (2) reductionof N₂ to ammonium (6-electron reduction) and (3) N₂O reductionto N₂ (2-electron reduction). ³ Present address: Department of Environmental Sciences, Facultyof Integrated Arts and Sciences, Hiroshima University, Hiroshima730, Japan ⁴ Present address: Department of Earth Sciences, Faculty ofScience, Toyama University, Gofuku, Toyama 930, Japan (Received June 18, 1986; Accepted December 16, 1986)     

Characterization of Two Proton Transport Systems in the Tonoplast of Plasmalemma-Permeabilized Nitella Cells

ATP-dependent and PP_i-dependent H⁺-transport systems of thetonoplast were characterized in plasmalemma-permeabilized Nitellacells, where direct access to the protoplasmic surface of thetonoplast was possible. Since H⁺ transport across the tonoplastcan be measured in situ, the identity of the membrane responsiblefor H⁺ pumping is unequivocal. H⁺ transport was evaluated bythe accumulation of neutral red. While both transport systemswere obligately dependent on Mg²⁺, the two transport systemsshowed completely different sensitivity to NO₃^– and K⁺,suggesting the presence of two types of H⁺-pumps in Nitellatonoplast. NO₃^– applied to the protoplasmic surface, completelyand reversibly inhibited ATP-dependent transport but had noeffect on PP_i-dependent transport. By contrast, NO₃^– appliedinto the vacuole by the vacuolar perfusion technique did notinhibit ATP-dependent or PP_i-dependent H⁺ transport. Replacementof K⁺ with the organic cation, BTP, inhibited PP_i-dependenttransport but not the ATP-dependent one, indicating that PP_i-dependenttransport is K⁺ dependent. The sensitivities of the H⁺ transportsystems found in the tonoplast of Nitella are quite similarto those of higher plant tonoplasts. ¹ Present address: Department of Botany, Faculty of Science,University of Tokyo, Hongo, Tokyo 113, Japan. (Received February 21, 1987; Accepted May 27, 1987)     

A comparison of nitrate transport in four different rice (Oryza sativa L.) cultivars

As rice can use both nitrate (NO₃^-) and ammonium (NH₄⁺), we have tested the hypothesis that the shift in the pattern of cultivars grown in Jiangsu Province reflects the ability of the plants to exploit NO₃^- as a nitrogen (N) source. Four rice cultivars were grown in solution culture for comparison of their growth on NO₃^- and NH₄⁺ nitrogen sources. All four types of rice, Xian You 63 (XY63), Yang Dao 6 (YD), Nong Keng 57 (NK) and Si You 917 (SY917), grew well and produced similar amounts of shoot biomass with 1 mmol/L NH₄⁺ as the only N source. However, the roots of NK were significantly smaller in comparison with the other cultivars. When supplied with 1 mmol/L NO₃^-, YD produced the greatest biomass; while NK achieved the lowest growth among the four cultivars. Electrophysiological measurements on root rhizodermal cells showed that the NO₃^--elicited changes in membrane potential (ΔE_m) of these four rice cultivars were significantly different when exposed to low external NO₃^- (<1 mmol/L); while they were very similar at high external NO₃^- (10 mmol/L). The root cell membrane potentials of YD and XY63 were more responsive to low external NO₃^- than those of NK and SY917. The ΔE_m values for YD and XY63 rhizodermal cells were almost the same at both 0.1 mmol/L and 1 mmol/L NO₃^-; while for the NK and SY917 the values became larger as the external NO₃^- increased. For YD cultivar, ΔE_m was measured over a range of NO₃^- concentrations and a Michaelis-Menten fit to the data gave a K_m value of 0.17 mmol/L. Net NO₃^- uptake depletion kinetics were also compared and for some cultivars (YD and XY63) a single-phase uptake system with first order kinetics best fitted the data; while other cultivars (ND and SY917) showed a better fit to two uptake systems. These uptake systems had two affinity ranges: one had a similar K_m in all the cultivars (0.2 mmol/L); the other much higher affinity system (0.03 mmol/L) was only present in NK and SY917. The expression pattern of twelve different NO₃^- transporter genes was tested using specific primers, but only OsNRT1.1 and OsNRT2.1 expression could be detected showing significant differences between the four rice cultivars. The results from both the physiological and molecular experiments do provide some support for the hypothesis that the more popular rice cultivars grown in Jiangsu Province may be better at using NO₃^- as an N source.     

Synthesis and Dissolution of Starch labelled with 14Carbon in Tobacco Leaf Tissue

Tobacco leaves depleted of starch, were detached and allowedto assimilate equal amounts of ¹⁴CO₂ and ¹²CO₂in succession,and vice versa. Distribution of radioactivity in starch, andsugars was determined after assimilation and after disks cutfrom the leaves had been kept in darkness for times up to 40hours. The amount and activity of the CO₂ was also determined.¹⁴C and ¹²C were incorporated in equal amounts into starch independentlyof the order in which they were supplied. In contrast sucrosehad high activity ¹⁴C was given last, and hexose a low one.The reverse was true when ¹²C was given last. Activity of respiratoryCO₂ was slightly higher when ¹⁴C was assimilated last as comparedwith ¹²C. In the dark only ¹⁴C or ¹²C was at first lost fromstarch, in accordance or removal of discrete layers. Analyticalresults show that starch is the main respiratory substrate andto account for the redistribution of radioactivity in passageto CO₂ it is concluded that sucrose occurs at two sites separatedinter-or intra-cellularly, one of which is in equilibrium withthe system intrconverting starch and CO₂ and at the other hexosesare produced by inversion. A starch-like polysaccharide is formedduring assimilation which persists in the dark and there isa significant contribution to respiration of carbon from non-carbohydratesources when leaf disks are kept on the dark.     

Characterization of Photosynthetic 14Carbon Assimilation by Potamogeton lucens L.

Photosynthetic assimilation of exogenous ¹⁴CO₂ and H¹⁴CO₃^–by the aquatic angiosperm Potamogeton lucens L. is reported.Equivalent maximum rates of assimilation (1.5 µmol s^–1m^–2) were obtained in the presence of saturating levelsof ¹⁴CO₂ (1.0 mol m^–3, pH 5.3) or H¹⁴CO₃^– (1.5 molm^–3, pH, 9.2). Under subsaturating ¹⁴CO₂ levels, bothgaseous diffusion and H¹⁴CO₃^– transport were shown tooperate simultaneously, such that maximal photosynthetic rateswere established. An induction lag of approximately 3 min was observed when exogenous¹⁴CO₂ was assimilated. A longer lag of approximately 12 minwas required, however, before linear assimilation rates wereestablished when H¹⁴CO₃ acted as the carbon source. The light-activatedH¹⁴CO₃^– transport system was found to be quite labile.A brief (5 min) dark treatment returned the system to the inactivestate. Bicarbonate transport was shown to be competitively inhibitedby CO₃^2–ions. The possibility is discussed that this formof inhibition may be common to many HCO₃^– assimilators. Preliminary polar cation transport studies (from lower to upperleaf surface) indicated an almost exact one to one relationshipbetween the rates of Na⁺ influx and efflux and H¹⁴CO₃^–assimilation. The possible relationship(s) between these transportprocesses and the requirement for electrical neutrality is brieflydiscussed.     

The occurrence and properties of methenyltetrahydrofolate cyclohydrolase in plants

Methenyltetrahydrofolate cyclohydrolase (E.C. 3.5.4.9 [EC] ), whichis responsible for the enzymatic conversion of 5,10-methenyl-H₄FAto 10-formyl-H₄FA, has been found in various plant tissues.The enzyme was partially purified from pea seedlings and someof its properties were investigated. It was unstable, but wasstabilized by the addition of 25% glycerol. The enzyme was purifiedabout 60-fold by fractionation with ammonium sulfate and columnchromatography on DEAE-cellulose in the presence of 25% glycerol.Optimum pH for the reaction was 7.7. Michaelis constants for5,10-methenyl-H₄FA in the forward reaction, and for 10-formyl-H₄FAin the reverse reaction were 4x10^–5M and 2x10^–4M,respectively. The apparent equilibrium constant for the reactionwas calculated as 50. Enzyme activity was greatly inhibitedby the reduced forms of folate derivatives. The probable participationof this enzyme in the regulation of folate coenzyme levels inplant tissues has been suggested. ¹ Studies on the enzymatic synthesis and metabolism of folatecoenzymes in plants, VI. (For Part V, see Reference (5) ). Partof this paper was presented at the 22nd annual meeting of theJapan Vitamin Society held at Hiroshima on October 14, 1970. ² Present address: Sizuoka Eiwa Junior College, Ikeda, Shizuoka. (Received September 9, 1972; )     

Fractionation of Nitrogen Isotopes by Glutamine Synthetase Isolated from Spinach Leaves

The isotopic fractionation of nitrogen in the reaction in vitroof glutamine synthetase isolated from spinach (Spinacia oleraceaL.) leaves was calculated from the changes in natural ¹⁵N abundance(     

Calcification in the Green Alga Halimeda: II. THE EXCHANGE OF CA2+ AND THE OCCURRENCE OF AGE GRADIENTS IN CALCIFICATION AND PHOTOSYNTHESIS

In Halimeda cylindracea and H. tuna segments, the concentrationof CaCO₃, MgCO₃, protein, and chlorophyll, as well as segmentvolume and wet and dry weight, increase with ‘age’i.e. from the apex of a branch downwards. Photosynthetic andcalcification rates decrease with age as does the degree oflight stimulation of calcification. Studies of the exchange of ⁴⁵Ca between the Halimeda thallusand the sea water under various conditions showed that mostof the Ca exchange is between the cell walls, the aragonitecrystals, and the intercellular space. The cell wall has twodistinguishable phases with half-times (t_0?5) of 200 and 35min while the CaCO₃ has a rapidly exchanging phase with a t_0?5of approximately 6 min. The t_0?5 of the exchange of Ca betweenthe intercellular space and the external medium is estimatedat about 6 min, on the basis of uptake studies. If the integrityof the barrier between the intercellular space and the externalsea water, created by the adpressed peripheral utricles is destroyedthe t_0?5 is smaller (<<3 min). These kinetic studies as well as comparative measurements ofcalcification rates by both isotopic and chemical methods showthat the ⁴⁵Ca method for measuring calcification rates overestimatesthe calcification rate, due to binding of ⁴⁵Ca in the cell wallsand retention of ⁴⁵Ca in the intercellular space. The ¹⁴C methodgives more accurate results and has the further advantage ofallowing simultaneous measurement of the photosynthetic andcalcification rate on the same segment.     

In vivo Treatments That Modulate PPi-Dependent H+ Transport Activity of Tonoplast-Enriched Membrane Vesicles from Barley Roots

The PP_i-dependent H⁺ transport activity of tonoplast-enrichedmembrane vesicles prepared from barley roots was greatly reducedwhen the plants were grown for 4 or 5 days with an additional3 raM KC1 in growth medium that contained only 0.1 mM CaCl₂in water. To characterize the mechanism of this reduction inactivity, we attempted to treat barley roots with K⁺ ions, Cl^-ions(or acetate), and A23187 [GenBank] (with or without Ca²⁺ ions), whichmight be expected to cause alkalization, acidification and mobilizationof Ca²⁺ ions in the cytoplasm, respectively. One-day treatmentof barley roots with K⁺ ions significantly decreased PP_i--dependentH⁺ transport activity of prepared tonoplast-enriched membranevesicles, while treatment with Cl^- ions or acetate significantlyincreased the activity. A similar increase in the activity alsooccurred by treatment with Ca²⁺ ions alone or in combinationwith A23187 [GenBank] . Determination of the PP_i-hydrolyzing activity ofmembrane vesicles showed that changes in this activity by thevarious treatments were similar to those in the PP_i-dependentH⁺ transport activity. The changes in ATP-dependent H⁺ transportactivity of membrane vesicles caused by these treatments weresmall. These results indicate that the in vivo treatments hadsignificant effects on the H⁺ transport activity of H⁺-PP_i-ase,one of the two active vacuolar H⁺-pumps (H⁺-PP_iase and H⁺-ATPase).In addition, these results suggest the possibility that changesin levels of cytoplasmic H⁺ or Ca²⁺ ions may be involved inmodulation of the H⁺ transport activity of the vacuolar H⁺-PP_iaseduring plant growth. (Received September 14, 1992; Accepted March 1, 1993)     

Odor detection curves for n-pentanoic acid in dogs and humans*

The ability of dogs and humans to detect vapor concentrationsof n-pentanoic (valeric) acid was measured under directly comparabletesting conditions. The minimum concentrations detected by dogswere 3.3 x 10⁶ molecules/cm³ by two German shepherds, and 8.8x 10⁸ molecules/cm³ by a Fox terrier. The average minimum detectedby humans was 5 x 10¹⁰ molecules/cm³. Detection curves for thetwo best performing human subjects showed double reversals inslope (a "notch") at approximately one-half log₁₀ unit of concentrationabove the minimum detectable level. Two distinct notches, separatedby about 2 log₁₀ units of concentration, occurred in the curvesfor the dogs; the lower notch, present in the curves of thetwo best performers, fell approximately 2 log₁₀ units abovethe lowest minimum concentration detected. Performance differencesproducing these latter notches were statistically significantand, according to one interpretation, could reflect the availabilityof less primary stimulus information at the two concentrationswhere they occur, a possible result of three slightly differentranges of receptor sensitivity.