Amperometric method for monitoring anaerobic respiration with nitrous oxide as the terminal electron acceptor

A commercially available Clark-type electrode with a platinum cathode, commonly used for monitoring oxygen uptake, may also be used to monitor respiration with N₂O. The disadvantages of this system include a high sensitivity to O₂, which may be overcome by excluding O₂, and sensitivity to acetylene. The advantage of the method is that it may be used to monitor directly the reduction of N₂O by respiring cells.     

Effect of taurine on arterial, uterine and cardiac PGI2 and TXA2 synthesis in the rat

The influence of taurine (in drinking water for 6 weeks) on PGI₂ and TXA₂ synthesis by some female rat organs was investigated using radioimmunoassay and platelet antiaggregatory bioassay. Taurine 100 and 200 mg/kg/day increased aortic PGI₂ release from 0.59 ± 0.04 (control) to 0.85 ± 0.05 and 1.01 ± 0.06 ng/mg, respectively and that by the myometrium from 0.24 ± 0.02 (control) to 0.38 ± 0.01 and 0.50 ± 0.04 ng/mg wet tissue, respectively (P < 0.05, n = 6). It did not affect PGI₂ and TXA₂ production in the heart or TXA₂ in the aorta. Taurine 200 mg/kg depressed uterine TXA₂ synthesis from 148.6 ± 9.8 (control) to 85.4 ± 6.8 pg/mg (P < 0.05, n = 6). Furthermore taurine 0.4 and 0.8 mM in vitro stimulated PGI₂ released by the myometrial and aortic tissues from pregnant rats. The stimulant effect of taurine on PGI₂ may be related to its antioxidant effect whereas its inhibitory effect on uterine TXA₂ may result from direction of synthesis towards PGI₂. It is concluded that endogenous taurine may participate in regulation of PGs synthesis and that prostanoids may contribute to its known actions. On broad basis, taurine-induced release of PGI₂ may prove of potential value in those ailments characterised by deficiency in PGI₂ release.     

The regulation of symbiotic N2 fixation: a conceptual model of N feedback from the ecosystem to the gene expression level

Symbiotic nitrogen (N₂) fixation in legumes may give the host plant a distinct competitive advantage; at the same time it is mainly responsible for introducing N into terrestrial ecosystems which may ultimately benefit all organisms. Depending on environmental conditions, symbiotic N₂ fixation may be tuned to the plant's N demand or specifically inhibited (a disadvantage for plants which depend mainly on symbiotic N₂ fixation), or even prevented. Thus, the ecological range for symbiotic N₂ fixation can be narrower than that of the host plants. A shortage of mineral N is the only case in which adverse environmental conditions clearly favour symbiotic N₂ fixation. Variations in number or mass of nodules or nodule morphology are persistent features, that may represent one kind of regulation of N₂ fixation. In addition, varying O₂ permeability of nodules functions as a rapid and reversible control of N₂ fixation which may compensate partially or fully for poor nodulation. The plant's demand for symbiotically fixed N is thought to play a central role in modulating both nodulation and N₂ fixation activity; an N feedback mechanism is assumed. The control of symbiotic N₂ fixation operates through a series of ecophysiological triggers which are also influenced by complex interactions between legume plants and other organisms in the ecosystem. The proportion of legume biomass and the performance of symbiotic N₂ fixation in each individual legume are the main parameters which determine the amount of symbiotically fixed N introduced into a terrestrial ecosystem. The various triggers and N feedback mechanisms from the whole ecosystem to the gene expression level which regulate symbiotic N₂ fixation in terrestrial ecosystems are reviewed and discussed in terms of a conceptual model. Although the presented model is based primarily on our knowledge about the physiology of a few leguminous crop species and of ecosystem processes in managed, perennial grassland in temperate climatic conditions, it may stimulate thinking about functional relationships between symbiotic N₂ fixation and terrestrial ecosystems at various system levels.     

A Coupled Ecosystem-Climate Model for Predicting the Methane Concentration in the Archean Atmosphere

A simple coupled ecosystem-climate model is described that canpredict levels of atmospheric CH₄, CO₂, and H₂during the Late Archean, given observed constraints on Earth'ssurface temperature. We find that methanogenic bacteria shouldhave converted most of the available atmospheric H₂ intoCH₄, and that CH₄ may have been equal in importance to CO₂ as a greenhouse gas. Photolysis of this CH₄ may have produced a hydrocarbon smog layer that would have shielded the surface from solar UV radiation. Methanotrophic bacteria would have consumed some of the atmospheric CH₄,but they would have been incapable of reducing CH₄ to modern levels. The rise of O₂ around 2.3 Ga would have drastically reduced the atmospheric CH₄ concentrationand may thereby have triggered the Huronian glaciation.     

The Effect of Atmospheric Carbon Dioxide Elevation on Plant Growth in Freshwater Ecosystems

We developed a dynamic model to investigate the effect of atmospheric carbon dioxide (CO₂) increase on plant growth in freshwater ecosystems. Steady-state simulations were performed to analyze the response of phytoplankton and submerged macrophytes to atmospheric CO₂ elevation from 350 to 700 ppm. We studied various conditions that may affect this response, such as alkalinity, the air–water exchange rate of CO₂, the community respiration rate, and the phosphorus (P) supply rate. The increase in atmospheric CO₂ could affect submerged plant growth only under relatively eutrophic conditions and at a low community respiration rate. Alkalinity had little effect on the response of the different species. When the air–water exchange was low, the proportional effect of the CO₂ increase on plant growth was higher. Under eutrophic conditions, algae and macrophytes using CO₂ and HCO₃^– may double their growth rate due to atmospheric CO₂ elevation, while the growth of macrophytes restricted to CO₂ assimilation may be threefold. The differences in response of the species under various conditions indicate that the elevation of atmospheric CO₂ may induce drastic changes in the productivity and species dominance in freshwater systems.     

ATP-dependent potassium channels of muscle cells: Their properties,regulation, and possible functions

ATP-dependent potassium channels are present at high density in the membranes of heart, skeletal, and smooth muscle and have a lowP _open at physiological [ATP]_i. The unitary conductance is 15–20 pS at physiological [K⁺] _o , and the channels are highly selective for K⁺. Certain sulfonylureas are specific blockers, and some K channel openers may also act through these channels. K_ATP channels are probably regulated through the binding of ATP, which may in turn be regulated through changes in the ADP/ATP ratio or in pH_i. There is some evidence for control through G-proteins. The channels have complex kinetics, with multiple open and closed states. The main effect of ATP is to increase occupancy of long-lived closed states. The channels may have a role in the control of excitability and probably act as a route for K⁺ loss from muscle during activity. In arterial smooth muscle they may act as targets for vasodilators.     

Discrete conductance fluctuations in lipid bilayer protein membranes

Discrete fluctuations in conductance of lipid bilayer membranes may be observed during the initial stages of membrane interaction with EIM ("excitability inducing material"), during destruction of the EIM conductance by proteolysis, and during the potential-dependent transitions between low and high conductance states in the "excitable" membranes. The discrete conductance steps observed during the initial reaction of EIM with the lipid membranes are remarkably uniform, even in membranes of widely varying lipid composition. They range only from 2 to 6 x 10_-10 ohm_-1 and average 4 x 10_-10 ohm_-1. Steps found during destruction of the EIM conductance by proteolysis are somewhat smaller. The transition between high conductance and low conductance states may involve steps as small as 0.5 x 10_-10 ohm_-1. These phenomena are consistent with the formation of a stable protein bridge across the lipid membrane to provide a polar channel for the transport of cations. T6he uniform conductance fluctuations observed during the formation of these macromolecular channels may indicate that the ions in a conductive channel, in its open state, are largely protected from the influence of the polar groups of the membrane lipids. Potential-dependent changes in conductance may be due to configurational or positional changes in the protein channel. Differences in lipid-lipid and lipid-macromolecule interactions may account for the variations in switching kinetics in various membrane systems.     

The enhancement of iron-dependent luminol peroxidation by 2,2′-Dipyridyl and nitrilotriacetate

The generation of radicals from luminol and H₂O₂, in the presence of iron and iron chelates was monitored by measuring the chemiluminescence produced by further oxidation of these radicals. 2,2′-Dipyridyl enhanced the production of chemiluminescence in the presence of FeSO₄, farritin and haemosiderin but not FeCI₃ or horseance of both FeSO₄ and FeCI₃ but not ferritin or haemosiderin. The enhancement of chemiluminescence by iron chelation may have analytical applications and the process by which these iron chelates are able to generate radicals from the nitrogenous base luminol may be similar to that responsible for their toxic effects on DNA.     

The action of elastase on p-nitroanilide substrates

The action of elastase has been studied on four p-nitroanilides: BOC-(Ala)₂-NA, (Ala)₃-NA, Ac-(Ala)₃-NA and BOC-(Ala)₃-NA. The second order rate constant kcat/Km increases considerably with the chain length of these substrates. With (Ala)₃-NA, activation by excess substrate was observed. DMF and DMSO inhibit strongly the elastase catalyzed hydrolysis of Ac- and BOC-(Ala)₃-NA. The later substrate may be used to assess rapidly elastase activity: concentrations as low as 0.2 μg/ml may be determined accurately.     

The age of Rubisco: the evolution of oxygenic photosynthesis

The evolutionary history of oxygenesis is controversial. Form I of ribulose 1,5‐bisphosphate carboxylase/oxygenase (Rubisco) in oxygen‐tolerant organisms both enables them to carry out oxygenic extraction of carbon from air and enables the competitive process of photorespiration. Carbon isotopic evidence is presented from ~2.9 Ga stromatolites from Steep Rock, Ontario, Canada, ~2.9 Ga stromatolites from Mushandike, Zimbabwe, and ~2.7 Ga stromatolites in the Belingwe belt, Zimbabwe. The data imply that in all three localities the reef‐building autotrophs included organisms using Form I Rubisco. This inference, though not conclusive, is supported by other geochemical evidence that these stromatolites formed in oxic conditions. Collectively, the implication is that oxygenic photosynthesizers first appeared ~2.9 Ga ago, and were abundant 2.7–2.65 Ga ago. Rubisco specificity (its preference for CO₂ over O₂) and compensation constraints (the limits on carbon fixation) may explain the paradox that despite the inferred evolution of oxygenesis 2.9 Ga ago, the Late Archaean air was anoxic. The atmospheric CO₂:O₂ ratio, and hence greenhouse warming, may reflect Form I Rubisco's specificity for CO₂ over O₂. The system may be bistable under the warming Sun, with liquid oceans occurring in either anoxic (H₂O with abundant CH₄ plus CO₂) or oxic (H₂O with more abundant CO₂, but little CH₄) greenhouse states. Transition between the two states would involve catastrophic remaking of the biosphere. Build‐up of a very high atmospheric inventory of CO₂ in the 2.3 Ga glaciation may have allowed the atmosphere to move up the CO₂ compensation line to reach stability in an oxygen‐rich system. Since then, Form I Rubisco specificity and consequent compensation limits may have maintained the long‐term atmospheric disproportion between O₂ and CO₂, which is now close to both CO₂ and O₂ compensation barriers.     

Was low atmospheric CO2 during the Pleistocene a limiting factor for the origin of agriculture?

Agriculture originated independently in many distinct regions at approximately the same time in human history. This synchrony in agricultural origins indicates that a global factor may have controlled the timing of the transition from foraging to food-producing economies. The global factor may have been a rise in atmospheric CO₂ from below 200 to near 270 μol mol^?1 which occurred between 15,000 and 12,000 years ago. Atmospheric CO₂ directly affects photosynthesis and plant productivity, with the largest proportional responses occurring below the current level of 350 μol mol^?1. In the late Pleistocene, CO₂ levels near 200 μol mol^?1 may have been too low to support the level of productivity required for successful establishment of agriculture. Recent studies demonstrate that atmospheric CO₂ increase from 200 to 270 μol mol^?1 stimulates photosynthesis and biomass productivity of C₃ plants by 25% to 50%, and greatly increases the performance of C₃ plants relative to weedy C₄ competitors. Rising CO₂ also stimulates biological nitrogen fixation and enhances the capacity of plants to obtain limiting resources such as water and mineral nutrients. These results indicate that increases in productivity following the late Pleistocene rise in CO₂ may have been substantial enough to have affected human subsistence patterns in ways that promoted the development of agriculture. Increasing CO₂ may have simply removed a productivity barrier to successful domestication and cultivation of plants. Through effects on ecosystem productivity, rising CO₂ may also have been a catalyst for agricultural origins by promoting population growth, sedentism, and novel social relationships that in turn led to domestication and cultivation of preferred plant resources.     

The direct involvement of hydrogen peroxide in indoleacetic acid inactivation

Hydrogen peroxide appears to mask the chemical characteristics of indoleacetic acid. This was demonstrated by the Salkowski and Fluorescence tests. Stem elongation and root initiation were inhibited as a result of adding H₂O₂ to nutrient media containing IAA, however, upon the addition of purified catalase, most of the symptoms of IAA inactivation were reversed. It is suggested that in vivo IAA may be regulated partially by its conjugation with H₂O₂, and catalase may have a role in the IAA reactivation process. The accumulation of hydrogen peroxide in the cells as a result of catalase inhibition may lead to a temporary IAA inactivation, therefore effecting plant growth.     

Ozone effects on plants in natural ecosystems

Tropospheric ozone (O₃) is an important stressor in natural ecosystems, with well‐documented impacts on soils, biota and ecological processes. The effects of O₃ on individual plants and processes scale up through the ecosystem through effects on carbon, nutrient and hydrologic dynamics. Ozone effects on individual species and their associated microflora and fauna cascade through the ecosystem to the landscape level. Systematic injury surveys demonstrate that foliar injury occurs on sensitive species throughout the globe. However, deleterious impacts on plant carbon, water and nutrient balance can also occur without visible injury. Because sensitivity to O₃ may follow coarse physiognomic plant classes (in general, herbaceous crops are more sensitive than deciduous woody plants, grasses and conifers), the task still remains to use stomatal O₃ uptake to assess class and species’ sensitivity. Investigations of the radial growth of mature trees, in combination with data from many controlled studies with seedlings, suggest that ambient O₃ reduces growth of mature trees in some locations. Models based on tree physiology and forest stand dynamics suggest that modest effects of O₃ on growth may accumulate over time, other stresses (prolonged drought, excess nitrogen deposition) may exacerbate the direct effects of O₃ on tree growth, and competitive interactions among species may be altered. Ozone exposure over decades may be altering the species composition of forests currently, and as fossil fuel combustion products generate more O₃ than deteriorates in the atmosphere, into the future as well.     

Identity of the rhizotoxic aluminium species

The aluminium (III) released from soil minerals to the soil solution under acid conditions may appear as hexaaquaaluminium (Al(H₂O)₆ ³⁺, or Al³⁺ for convenience) or may react with available ligands to form additional chemical species. That one or more of these species is rhizotoxic (inhibitory to root elongation) has been known for many decades, but the identity of the toxic species remains problematical for the following reasons. 1. Several Al species coexist in solution so individual species cannot be investigated in isolation, even in artificial culture media. 2. The activities of individual species must be calculated from equilibrium data that may be uncertain. 3. The unexpected or undetected appearance of the extremely toxic triskaidekaaluminium (AlO₄Al₁₂(OH)₂₄(H₂O)₁₂ ⁷⁺ or Al₁₃) may cause misatribution of toxicity to other species, especially to mononuclear hydroxy-Al. 4. If H⁺ ameliorates Al³⁺ toxicity, or vice versa, then mononuclear hydroxy-Al may appear to be toxic when it is not. 5. The identity and activities of the Al species contacting the cell surfaces are uncertain because of the H⁺ currents through the root surface and because of surface charges. This article considers the implications of these problems for good experimental designs and critically evaluates current information regarding the relative toxicities of selected Al species. It is concluded that polycationic Al (charge >2) is rhizotoxic as are other polyvalent cations.     

THE EFFECT OF VITAMIN B12 ON THE ANEMIA AND COMBINED SYSTEM DISEASE OF ADDISONIAN PERNICIOUS ANEMIA

The effect of the parenteral administration of vitamin B₁₂ has been observed in eight patients with Addisonian pernicious anemia.Vitamin B₁₂ in initial doses of 50 micrograms or 25 micrograms induced satisfactory reticulocyte response and a return of erythrocyte count to within normal range in 60 days.In only two of the patients were secondary reticulocyte responses induced on a second injection of vitamin B₁₂.Concurrently with the hemopoietic response, the bone marrow changed from megaloblastic hyperplasia to normoblastic distribution.The paresthesias associated with combined system disease as well as disturbances in position sense and locomotor function may be entirely relieved or greatly diminished following injections of vitamin B₁₂.Maintenance injections of vitamin B₁₂ may be from 30 to 50 micrograms at intervals of one month, the amount depending upon the individual case.Vitamin B₁₂ may be used without untoward symptoms in patients previously sensitive to liver extract.     

Macrokinetics and operational stability of immobilized glucose oxidase and catalase

Glucose oxidation by immobilized glucose oxidase (GlO) and catalase (Cat) has been investigated in batch and continuous reactions for operational studies. The macrokinetics of the process depend on coupled reaction steps and diffusion rates. The problem may be approximated by a simple pseudohomogeneous model taking into account both substrates of glucose oxidase and the intermediate reaction product H₂O₂. The effectiveness of both enzymes is enhanced in the coupled reaction path, the overall effectiveness nevertheless is very low. H₂O₂ causes the inactivation of both GlO and Cat. The rates of deactivation depend on the oxidation rates of glucose that give different quasistationary levels of H₂O₂ concentration. As a first approximation, the deactivation rates may be described by first-order reactions with respect to H₂O₂.     

Inhibition of ribulose-1,5-bisphosphate carboxylase/oxygenase by ribulose-1,5-bisphosphate epimerization and degradation products

Xylulose-1,5-bisphosphate in preparations of ribulose-1,5-bisphosphate (ribulose-P₂) arises from non-enzymic epimerization and inhibits the enzyme. Another inhibitor, a diketo degradation product from ribulose-P₂, is also present. Both compounds simulate the substrate inhibition of ribulose-P₂ carboxylase/oxygenase previously reported for ribulose-P₂. Freshly prepared ribulose-P₂ had little inhibitory activity. The instability of ribulose-P₂ may be one reason for a high level of ribulose-P₂ carboxylase in chloroplasts where the molarity of active sites exceeds that of ribulose-P₂. Because the K_D of the enzyme/substrate complex is ≤1 μM, all ribulose-P₂ generated in situ may be stored as this complex to prevent decomposition.     

Population genetic structure of the gynodioecious Thymus vulgaris L. (Labiatae) in southern France

In a self-compatible gynodioecious species, the abundance of female plants (which are obligate outcrossers) relative to hermaphrodites (which may self and outcross) may be a critical factor influencing genetic diversity and population structure. In the gynodioecious Thymus vulgaris L., female frequency varies from 5 to 95%, providing a suitable model to examine this issue. In this study, we use allozyme markers to (1) evaluate the relationship between female frequency, genetic diversity and population structure, (2) determine whether females and hermaphrodites vary in heterozygote deficiency and (3) examine whether other factors such as plant density are related to heterozygote deficiency. Twenty three natural populations, with female frequencies ranging from 11 to 92%, were sampled in and around the St-Martin-de-Londres basin in southern France. Based on four polymorphic allozyme loci, we found no significant correlation between female frequency and heterozygote deficiency. A significant (P < 0.05) F_IS value over loci and over populations of 0.11 was detected. The F_IS value per population showed a significant heterozygote deficiency in 11 of the 23 populations. However, no significant difference between female and hermaphrodite F_IS values was found. A significant heterozygote deficiency only occurred in populations of intermediate density. There was little differentiation among populations (F_ST = 0.038) nor among subpopulations within each population. The significant F_IS values are thus mostly due to inbreeding effects. The lack of a correlation between F_IS values and female frequency may be due to outcrossing in hermaphrodites and/or restoration of male fertility which may occur to a greater extent at low female frequency. The similarity of female and hermaphrodite F_IS values indicates that females may occasion high levels of biparental inbreeding.     

The effect of caffeine on prostaglandin output from the perfused mesenteric vascular bed of the rat

Caffeine significantly (p < 0.05) increased the output of prostacyclin (PGI₂) from the perfused rat mesenteric vascular bed. The outputs of PGE₂ and PGF_2α were also increased by caffeine. This stimulatory response to caffeine did not show rapid desensitization. Ryanodine also increased PG output, suggesting that caffeine may be acting via the stimulation of a ryanodine receptor. The increased production of a vasodilator such as PGI₂ from blood vessels following exposure to caffeine may explain why caffeine has a beneficial effect in angina.     

Pliocene climates: the nature of the problem

The Pliocene may have been the last time period when global temperatures were greater than present. The Pliocene data base is sufficiently complete to provide a valuable test for climate model predictions for warm time periods. This paper reviews some key issues with respect to understanding and verifying theories for the origin of Pliocene warmth. There are two main factors cited to explain Pliocene warmth—higher CO₂ levels or higher levels of ocean heat transport. The two explanations may not be exclusive; for example CO₂ increases may drive ocean heat transport changes. However, initial proxy-CO₂ reconstructions suggest that the CO₂ perturbation is very small (~100 ppm) to effect such large changes in climate. Considerably more data are needed to evaluate the magnitude of Pliocene CO₂ changes. Although more modeling work is also required, it is necessary to continue evaluation of input data used to force model results (particularly sea surface temperatures). Continued simulations and evaluation of pCO₂ and SST results should enable us to better understand how the earth responds during a global warming and determine whether our models are properly simulating such changes.