Interaction of enantiomeric alkylacyl and diacylglycerophosphocholines with cholesterol in bilayer membranes

The sn-1 and sn-3 isomers of dioleoylglycerophosphocholine form vesicles of the same size as the racemic lipid. Identical permeability coefficients were found for the diffusion of glucose and chloride across bilayer membranes of vesicles consisting of these lipids. Vesicles made of mixtures of enantiomeric or racemic dioleoyllecithin with 30 mol% cholesterol have identical radii. Cholesterol reduces the permeability of bilayers for glucose and chloride irrespective of the steric configuration of the constituent phospholipid. Increasing concentrations of cholesterol (17, 33 and 50 mol%, respectively) broaden the (CH₂)_n signal in the ¹H-NMR-spectra (90 MHz) of unilamellar vesicles containing sn-1, sn-3 or rac alkyloleoylglycerophosphocholine to the same extent. These results indicate that the steric configuration of phospholipids has no gross effect on the arrangement of phospholipids and cholesterol in bilayer membranes.     

A comparison of the 8-hydroxydeoxyguanosine,chromosome aberrations and micronucleus techniques for the assessment of the genotoxicity of mercury compounds in human blood lymphocytes

We compared the mechanism of action of micronuclei (MN), unstable chromosome aberrations, and 8-hydroxydeoxyguanosine (8-OHdG) levels to evaluate the genotoxicity of methyl mercuric chloride (CH₃HgCl) and mercuric chloride (HgCl₂) in human peripheral lymphocytes. The chromosome aberrations in human peripheral lymphocytes exposed to various concentrations of CH₃HgCl or HgCl₂ increased in a concentration-dependent manner and were significantly higher than the control when the cells were incubated with 1 × 10⁻⁵ M (HgCl₂) or 2 × 10⁻⁶ M (CH₃HgCl). The increase in the incidence of micronucleated lymphocytes was significant among the exposed groups, being 2 × 10⁻⁵ M (HgCl₂) and 5 × 10⁻⁶ M (CH₃HgCl) compared with the control. CH₃HgCl was about 4-fold more potent than HgCl₂. We determined the 8-OHdG levels in human peripheral blood mononuclear cells(PBMC) and found that they were significantly higher in the exposed groups at 1 × 10⁻⁵ M (HgCl₂) and 5 × 10⁻⁶ M (CH₃HgCl) compared with the control. A detectable (p < 0.05) increase in the level of 8-OHdG was induced by CH₃HgCl at a concentration that was about 50% of the amount of HgCl₂ required to produce a similar response. The data confirmed the value of the MN and/or chromosome aberration assays for assessing of HgCl₂- and/or CH₃HgCl-induced genotoxicity, and indicated that they are about the same concentration as the 8-OHdG assay. The presence of genotoxic effects in peripheral blood lymphocytes exposed to the mercuric compounds indicated by the chromosome aberrations and the MN assays could be partly due either to the disturbance of the spindle mechanism, or to the elevated level of 8-OHdG brought by the generation of reactive oxygen species.     

The AQP-3 water channel is a pivotal modulator of glycerol-induced chloride channel activation in nasopharyngeal carcinoma cells

Aquaporin (AQP) and chloride channels are ubiquitous in virtually all living cells, playing pivotal roles in cell proliferation, migration and apoptosis. We previously reported that AQP-3 aquaglyceroporin and ClC-3 chloride channels could form complexes to regulate cell volume in nasopharyngeal carcinoma cells. In this study, the roles of AQP-3 in their hetero-complexes were further investigated. Glycerol entered the cells via AQP-3 and induced two different Cl⁻ currents through cell swelling-dependent or -independent pathways. The swelling-dependent Cl⁻ current was significantly inhibited by pretreatment with CuCl₂ and AQP-3-siRNA. After siRNA-induced AQP-3 knock-down, the 140 mM glycerol isoosmotic solution swelled cells by 22% (45% in AQP-3-intact cells) and induced a smaller Cl⁻ current; this current was smaller than that activated by 8% cell volume swelling, which induced by the 140 mM glycerol hyperosmotic solution in AQP-3-intact cells. This suggests that the interaction between AQP-3 and ClC-3 plays an important role in cell volume regulation and that AQP-3 may be a modulator that opens volume-regulated chloride channels. The swelling-independent Cl⁻ current, which was activated by extracellular glycerol, was reduced by CuCl₂ and AQP-3-siRNA pretreatment. Dialyzing glycerol into cells via the pipette directly induced the swelling-independent Cl⁻ current; however this current was blocked by AQP-3 down-regulation, suggesting AQP-3 is essential for the opening of chloride channels. In conclusion, AQP-3 is the pathway for water, glycerol and other small solutes to enter cells, and it may be an essential modulator for the gating of chloride channels.     

Characterization of lipid efflux particles generated by seminal phospholipid-binding proteins

We reported recently that the choline phospholipid-binding proteins (BSP-A1/-A2, BSP-A3 and BSP-30-kDa) of bovine seminal plasma (BSP) stimulate cholesterol and choline phospholipid efflux from fibroblasts. In this study, we characterized the lipid efflux particles generated by BSP proteins. The density gradient ultracentrifugation of the efflux medium from radiolabeled fibroblasts incubated with BSP proteins showed a single peak of [³H]cholesterol between density (d) 1.12 and 1.14 g/ml, which is in the range of high-density lipoproteins. Size-exclusion chromatographic and immunoblot analysis revealed that the efflux particles have a large size equal to or bigger than very low-density lipoproteins and contained BSP proteins. Lipid analysis of density gradient and gel filtration fractions from efflux medium of simultaneously labeled fibroblasts ([³H]cholesterol and [³H]choline) incubated with BSP proteins showed that the efflux particles were homogeneous and composed of cholesterol and choline phospholipids. The lipid particles contained BSP proteins, cholesterol and choline phospholipids in molar ratio of 0.05:1.21:1, respectively. Agarose gel electrophoresis showed that the BSP-generated lipid particles had a γ migration pattern which is slower than low-density lipoproteins. The sonication of cholesterol and BSP proteins followed by gel filtration chromatographic analysis indicated no direct binding of cholesterol to BSP proteins. These results taken together indicate that BSP proteins induce a concomitant cholesterol and choline phospholipid efflux and generate large protein–lipid particles.     

Osmotic behavior of liposomes of phosphatidylcholine and phosphatidylsulfocholine as a function of lipid concentration

A relationship between the initial rate of liposome swelling, d(1/A)/dt and the reciprocal of the lipid concentration of the liposomes has been derived and then utilized to describe the osmotic swelling behavior of serially diluted liposomes and chloroplasts exposed to hypertonic urea solutions. The slopes of plots of d(1/A)/dt vs. the reciprocal of the lipid concentration of liposomes were not affected by differences in the initial absorbance of phosphatidylcholine-sterol bilayers, and were used to assess the ability of sterols to reduce the initial rates of urea permeation through dimyristoylphosphatidylcholine (DMPC) bilayers in the liquid-crystalline state. Multilamellar liposomes and sonicated vesicles were prepared from dimyristoylphosphatidylsulfocholine (DMPSC), in which the quaternary ammonium group of choline is replaced by -S⁺(CH₃)₂. Cholesterol reduced the initial rate of osmotic urea penetration into liposomes and the rate of 6-carboxyfluorescein efflux from vesicles at 35°C. The effect of cholesterol on bilayers of phosphatidylsulfocholine and phosphatidylcholine was very similar, suggesting that no strict structural requirements need be met in the choline moiety for lecithin-cholesterol interaction. The sulfonium analog could thus functionally replace phosphatidylcholine in natural membranes.     

Effect of stand age on greenhouse gas fluxes from a Sitka spruce [Picea sitchensis (Bong.) Carr.] chronosequence on a peaty gley soil

The influence of forest stand age in a Picea sitchensis plantation on (1) soil fluxes of three greenhouse gases (GHGs – CO₂, CH₄ and N₂O) and (2) overall net ecosystem global warming potential (GWP), was investigated in a 2‐year study. The objective was to isolate the effect of forest stand age on soil edaphic characteristics (temperature, water table and volumetric moisture) and the consequent influence of these characteristics on the GHG fluxes. Fluxes were measured in a chronosequence in Harwood, England, with sites comprising 30‐ and 20‐year‐old second rotation forest and a site clearfelled (CF) some 18 months before measurement. Adjoining unforested grassland (UN) acted as a control. Comparisons were made between flux data, soil temperature and moisture data and, at the 30‐year‐old and CF sites, eddy covariance data for net ecosystem carbon (C) exchange (NEE). The main findings were: firstly, integrated CO₂ efflux was the dominant influence on the GHG budget, contributing 93–94% of the total GHG flux across the chronosequence compared with 6–7% from CH₄ and N₂O combined. Secondly, there were clear links between the trends in edaphic factors as the forest matured, or after clearfelling, and the emission of GHGs. In the chronosequence sites, annual fluxes of CO₂ were lower at the 20‐year‐old (20y) site than at the 30‐year‐old (30y) and CF sites, with soil temperature the dominant control. CH₄ efflux was highest at the CF site, with peak flux 491±54.5 μg m⁻² h⁻¹ and maximum annual flux 18.0±1.1 kg CH₄ ha⁻¹ yr⁻¹. No consistent uptake of CH₄ was noted at any site. A linear relationship was found between log CH₄ flux and the closeness of the water table to the soil surface across all sites. N₂O efflux was highest in the 30y site, reaching 108±38.3 μg N₂O‐N m⁻² h⁻¹ (171 μg N₂O m⁻² h⁻¹) in midsummer and a maximum annual flux of 4.7±1.2 kg N₂O ha⁻¹ yr⁻¹ in 2001. Automatic chamber data showed a positive exponential relationship between N₂O flux and soil temperature at this site. The relationship between N₂O emission and soil volumetric moisture indicated an optimum moisture content for N₂O flux of 40–50% by volume. The relationship between C : N ratio data and integrated N₂O flux was consistent with a pattern previously noted across temperate and boreal forest soils.     

Reverse NaCa exchange requires internal Ca and/or ATP in squid axons

Classical NaCa exchange models are based on a symmetric carrier system where Na and Ca competing from the same site, can produce net movement of the other against its electrochemical gradient. We have explored this symmetric assumption by studying the Ca_o and Na_o-dependent Na efflux in dialyzed squid axons in which proper control of both external and internal medium was achieved. The results show: (1) In axons dialyzed without Ca_i and ATP, Ca_o-dependent Na efflux cannot be detected even in the absence of Na_o. Under these conditions, the level of Na efflux (1 pmol · cm⁻² · s⁻¹) is close to that predicted by an electrical ‘leak’. (2) In axons dialyzed with Ca_i (100 μM) and without ATP, Na efflux measured in 440 mM Na_o, is about 4–5 pmol · cm⁻² · s⁻¹ and rather insensitive to Ca_o between 0 and 10 mM. However, in the absence of Na_o, a Ca_o-dependent Na efflux is observed similar in magnitude to that found in the presence of external Na. (3) In the presence of both Ca_i and ATP, Na efflux into artificial sea-water (440 mM Na, 10 mM Ca) is 18 pmol · cm⁻² · s⁻¹. In the absence of Na_o the efflux of Na is 7.5 pmol · cm⁻² · s⁻¹. In the absence of both Na_o and Ca_o the efflux is close to ‘leak’. With full Na_o but no Ca_o, the Na efflux average 12.6 pmol · cm⁻² · s⁻¹. These results indicate a marked asymmetry in the modus operandi of the NaCa exchange system with respect to Ca_i and ATP. These two substrates are required from the cis side to promote Ca_o-dependent Na efflux (reversal NaCa exchange).     

Effect of Ca2+ on the retention of glycerol and amino acids in Dunaliella tertiolecta

When D. tertiolecta cells, previously incubated in a 0.5 kmol m⁻³ NaCl medium with 1mol m⁻³ Ca²⁺, were transferred to an isotonic NaCl medium without Ca²⁺, the intracellular glycerol, as well as intracellular amino acids, was transiently lost to the medium within 30 min. The transient leakage of glycerol and amino acids was enhanced by the addition of EGTA (1 mol m⁻³), while the addition of SrCl₂ (1 mol m ⁻³) or polyamines such as spermidine (5 mol m⁻³) and spermine (5 mol m⁻³) restrained the leakage caused by the lack of external Ca²⁺ of intracellular glycerol and amino acids.     

Hydrologic regulation of gross methyl chloride and methyl bromide uptake from Alaskan Arctic tundra

The Arctic tundra has been shown to be a potentially significant regional sink for methyl chloride (CH₃Cl) and methyl bromide (CH₃Br), although prior field studies were spatially and temporally limited, and did not include gross flux measurements. Here we compare net and gross CH₃Cl and CH₃Br fluxes in the northern coastal plain and continental interior. As expected, both regions were net sinks for CH₃Cl and CH₃Br. Gross uptake rates (−793 nmol CH₃Cl m⁻² day⁻¹ and −20.3 nmol CH₃Br m⁻² day⁻¹) were 20–240% greater than net fluxes, suggesting that the Arctic is an even greater sink than previously believed. Hydrology was the principal regulator of methyl halide flux, with an overall trend towards increasing methyl halide uptake with decreasing soil moisture. Water table depth was one of the best predictors of net and gross uptake, with uptake increasing proportionately with water table depth. In drier areas, gross uptake was very high, averaging −1201 nmol CH₃Cl m⁻² day⁻¹ and −34.9 nmol CH₃Br m⁻² day⁻¹; in flooded areas, gross uptake was significantly lower, averaging −61 nmol CH₃Cl m⁻² day⁻¹ and −2.3 nmol CH₃Br m⁻² day⁻¹. Net and gross uptake was greater in the continental interior than in the northern coastal plain, presumably due to drier inland conditions. Within certain microtopographic features (low‐ and high‐centered polygons), uptake rates were positively correlated with soil temperature, indicating that temperature played a secondary role in methyl halide uptake. Incubations suggested that the inverse relationship between water content and methyl halide uptake was the result of mass transfer limitation in saturated soils, rather than because of reduced microbial activity under anaerobic conditions. These findings have potential regional significance, as the Arctic is expected to become warmer and drier due to anthropogenic climate forcing, potentially enhancing the Arctic sink for CH₃Cl and CH₃Br.     

The interaction of cholesterol with bilayers of phosphatidylethanolamine

The interaction of cholesterol with the glycerol backbone segments of phospholipids was studied in bilayers of phosphatidylethanolamine containing equimolar amounts of cholesterol. Glycerol selectively deuterated at various positions was supplied to the growth medium of Escherichia coli strain 131 GP which is defective in endogeneous glycerol synthesis. The procedure enables the stereospecific labeling of the three glycerol backbone segments of the membrane phospholipids. Phosphatidylethanolamine with wild-type fatty acid composition was purified from E. coli cells and deuterium magnetic resonance spectra were obtained either from dispersions of pure phosphatidylethanolamine or from equimolar mixtures of phosphatidylethanolamine with cholesterol. For comparative purposes 1,2-di[9,10-²H₂]elaidoyl-sn-glycero-3-phosphoethanolamine and [3-α-²H]cholesterol were synthesized in order to monitor the behavior of the fatty acyl chains and of the cholesterol molecule itself. For all deuterated segments the deuterium quadrupole splittings as well as the deuterium spin-lattice (T₁) relaxation times were measured as a function of temperature. The glycerol backbone was found to be a remarkably stable structural element of the phospholipid molecule. The quadrupole splittings of the backbone segments changed only by at most 2 kHz upon incorporation of 50 mol % cholesterol. This was in contrast to the fatty acyl chains where the same amount of cholesterol increased the quadrupole splitting by more than 20 kHz. The glycerol segments exhibited the shortest T₁ relaxation times of all CH₂ segments indicating that the glycerol backbone is the slowest motional moiety of the lipid molecule. Addition of cholesterol has no effect on the backbone motion but the fast reorientation rate of the trans-double bonds in 1,2-dielaidoyl-sn-glycero-3-phosphoethanolamine is increased dramatically.     

31P NMR Studies of the Binding of the Oligonucleotide (Ap)3A to an Oligodeoxythymidylate Covalently Linked to an Acridine Derivative

Abstract

³¹P NMR was used to study the specific interaction of an oligodeoxynucleotide containing four thymines and covalently attached to an acridine derivative through its 3-phosphate [(Tp)₄(CH₂)₅Acr] with a complementary oligoribonucleotide (Ap)₃A.³¹P-¹H and ¹H-¹H chemical shift correlation spectroscopies were jointly used to provide the assignment of the phosphorus resonances. A downfield shift of two phosphorus resonances of (Tp)₄(CH₂)₅Acr and of two phosphorus resonances of (Ap)₄A was observed upon complex formation. The assignment of the phosphorus resonances which are downfield shifted allowed us to propose a model involving an equilibrium between several 1:1 complexes where the acridine ring is intercalated between different A.T base pairs.     

Some Physical and Chemical Properties of Water from an Undisturbed Tropical Catchment Area (Guma Dam,Sierra Leone)

The water had a very low content of total suspended solids (<1 mg l⁻¹), but its transparency was high (5–8 Hazen units). The concentration of Mg⁺⁺ and Ca⁺⁺ were below 1 mg l⁻¹, but that of SiO₂ was 5.3 mg l⁻¹. Free CO₂ was abundant (15.3 mg l⁻¹) and the pH was low (<6.5). These conditions were accompanied by low concentrations of PO₄-P, total iron and NO₃-N. The DO content of the water was always below 80 %, but the chloride concentration (8.4 mg l⁻¹) seems relatively high for this type of freshwaters. It is, however, much lower than that known for arid areas. It is concluded that the geology and vegetation dominate the chemistry of the water from the Guma Dam catchment area. The influence of man is acknowledged only in as far as he has protected the catchment area.     

Soil–atmosphere exchange of greenhouse gases in a Eucalyptus marginata woodland, a clover-grass pasture, and Pinus radiata and Eucalyptus globulus plantations

Soils provide the largest terrestrial carbon store, the largest atmospheric CO₂ source, the largest terrestrial N₂O source and the largest terrestrial CH₄ sink, as mediated through root and soil microbial processes. A change in land use or management can alter these soil processes such that net greenhouse gas exchange may increase or decrease. We measured soil–atmosphere exchange of CO₂, N₂O and CH₄ in four adjacent land‐use systems (native eucalypt woodland, clover‐grass pasture, Pinus radiata and Eucalyptus globulus plantation) for short, but continuous, periods between October 2005 and June 2006 using an automated trace gas measurement system near Albany in southwest Western Australia. Mean N₂O emission in the pasture was 26.6 μg N m⁻² h⁻¹, significantly greater than in the natural and managed forests (< 2.0 μg N m⁻² h⁻¹). N₂O emission from pasture soil increased after rainfall events (up to 100 μg N m⁻² h⁻¹) and as soil water content increased into winter, whereas no soil water response was detected in the forest systems. Gross nitrification through ¹⁵N isotope dilution in all land‐use systems was small at water holding capacity < 30%, and under optimum soil water conditions gross nitrification ranged between < 0.1 and 1.0 mg N kg⁻¹ h⁻¹, being least in the native woodland/eucalypt plantation < pine plantation < pasture. Forest soils were a constant CH₄ sink, up to −20 μg C m⁻² h⁻¹ in the native woodland. Pasture soil was an occasional CH₄ source, but weak CH₄ sink overall (−3 μg C m⁻² h⁻¹). There were no strong correlations (R < 0.4) between CH₄ flux and soil moisture or temperature. Soil CO₂ emissions (35–55 mg C m⁻² h⁻¹) correlated with soil water content (R < 0.5) in all but the E. globulus plantation. Soil N₂O emissions from improved pastures can be considerable and comparable with intensively managed, irrigated and fertilised dairy pastures. In all land uses, soil N₂O emissions exceeded soil CH₄ uptake on a carbon dioxide equivalent basis. Overall, afforestation of improved pastures (i) decreases soil N₂O emissions and (ii) increases soil CH₄ uptake.     

Methane efflux in relation to plant biomass and sediment characteristics in stands of three common emergent macrophytes in boreal mesoeutrophic lakes

Methane efflux was studied in stands of three emergent macrophyte species (Equisetum fluviatile, Schoenoplectus lacustris and Phragmites australis) commonly found in the littoral zone of boreal lakes. In vegetation stands with relatively low methane (CH₄) emissions (<0.3 mol m^?2 (ice‐free period)^?1), the seasonal variation of CH₄ efflux was better correlated with the dynamics of plant growth than variation in sediment temperature. In dense and productive vegetation stands that released high amounts of CH₄ (2.3–7.7 mol m^?2 (ice‐free period)^?1), the seasonal variation in CH₄ efflux was correlated with sediment temperature, indicating that methanogens were more limited by temperature than substrate supply. The bottom type at the growth site of the emergent plants significantly influenced the ratio of CH₄ efflux to aboveground biomass of plants (Eff : B). The lowest Eff : B ratio was found in E. fluviatile stands growing on sand bottom under experimental conditions and the highest in P. australis‐dominated littoral areas accumulating detritus from external sources. The future changes expected in the hydrology of boreal lakes and rivers because of climatic warming may impact the growth conditions of aquatic macrophytes as well as decomposition and accumulation of detritus and, thus, CH₄ effluxes from boreal lakes.     

Evidence that human α-thrombin is a monovalent cation-activated enzyme

The activity of human α-thrombin (EC 3.4.21.5) on small peptide substrates was enhanced by NaCl or KCl while tetramethylammonium chloride ((CH₃)₄NCl) or choline chloride (HO(CH₂)₂N(CH₃)₃Cl) which were used as ionic strength controls were without effect. The steady-state kinetic parameters of thrombin amidolysis of several peptidyl p-nitroanilide substrates were measured. Na⁺ enhanced thrombin activity by decreasing the K_m,app (0.2 to 0.7-fold) of all substrates, as well as increasing thombin turnover (3.4 to 4.5-fold) of some substrates. The average K_A for Na⁺for the four substrates examined was 3.5 × 10^?2m. A comparison of the effects of Na⁺ vs K⁺ on thrombin hydrolysis of a single substrate indicated that both cations similarly decreased the K_m,app (0.2 to 04.-fold) and increased thek_cat,app (3.1 to 3.4-fold) except that higher K⁺ concentrations (K_A = 2.8 × 10^?1M) were required. The rate of inactivation of thrombin by the active site-directed inhibitor N-p-tosyl-lysine chloromethyl ketone under pseudo-first-order conditions was enhanced 3-fold by saturating NaCl. Also, the fibrinogen clotting activity of thrombin was enhanced by NaCl compared to the choline chloride control. Spectral studies demonstrated that thrombin titration by Na⁺ caused a positive ultraviolet difference spectrum with maxima at 281.5 and 288.5 nm (Δ?_288.5 = +1067). The K_m for Na⁺ was 2.3 × 10^?2m which agrees with the kinetically determined K_A for Na⁺. The results are consistent with Na⁺ binding to thrombin causing a conformational change in the active site. It is concluded that human α-thrombin is a monovalent cation-activated enzyme.     

Permeability properties of unilamellar vesicles containing choline plasmalogens and comparison with other choline glycerophospholipid species

The rates of non-electrolyte and ion diffusion across bilayer membranes consisting of choline plasmologens or of their alkyl and acyl analogs were studied. The influx of [¹⁴C]glucose, ⁸⁶Rb⁺ and ³⁶Cl^? into small unilamellar vesicles made from a semisynthetic choline plasmalogen and from synthetic diacyl, alkylacyl and dialkyl analogs with comparable side chain compositions were measured. Rates of glucose and Rb⁺ diffusion are about equal in alkenylacyl- and diacyl-glycerophosphocholine (GPC) bilayers, but are reduced in dialkyl-GPC membranes; the permeability coefficients correlate with the packing densities of the respective choline glycerophospholipids in monolayers at the air water interface. Rates of chloride diffusion are consistently higher in membranes formed from phospholipids containing alkenyl or alkyl other bonds as compared to the diacyl analogs. Highest rates of Cl^? diffusion are observed with choline plasmalogen vesicles. The phospholipid side chain composition has little influence on Cl^? permeation, but glucose and Rb⁺ diffusion are markedly affected. Incorporation of cholesterol (30 mol%) into choline plasmalogen membranes reduces their solute permeability by approximately 70%. A similar effect is found with the other choline phospholipid analogs. Thus, the choline phospholipid—cholesterol interaction, as far as it is reflected in reduced bilayer permeability, is not influenced by the presence of the alkenylether bond of plasmalogens.     

Using radon to quantify groundwater discharge and methane fluxes to a shallow,tundra lake on the Yukon-Kuskokwim Delta,Alaska

Northern lakes are a source of greenhouse gases to the atmosphere and contribute substantially to the global carbon budget. However, the sources of methane (CH₄) to northern lakes are poorly constrained limiting our ability to the assess impacts of future Arctic change. Here we present measurements of the natural groundwater tracer, radon, and CH₄ in a shallow lake on the Yukon-Kuskokwim Delta, AK and quantify groundwater discharge rates and fluxes of groundwater-derived CH₄. We found that groundwater was significantly enriched (2000%) in radon and CH₄ relative to lake water. Using a mass balance approach, we calculated average groundwater fluxes of 1.2 ± 0.6 and 4.3 ± 2.0 cm day⁻¹, respectively as conservative and upper limit estimates. Groundwater CH₄ fluxes were 7—24 mmol m⁻² day⁻¹ and significantly exceeded diffusive air–water CH₄ fluxes (1.3–2.3 mmol m⁻² day⁻¹) from the lake to the atmosphere, suggesting that groundwater is an important source of CH₄ to Arctic lakes and may drive observed CH₄ emissions. Isotopic signatures of CH₄ were depleted in groundwaters, consistent with microbial production. Higher methane concentrations in groundwater compared to other high latitude lakes were likely the source of the comparatively higher CH₄ diffusive fluxes, as compared to those reported previously in high latitude lakes. These findings indicate that deltaic lakes across warmer permafrost regions may act as important hotspots for CH₄ release across Arctic landscapes.

     

Growth of Methanobacterium thermoautotrophicum on H2CO2: High CH4 productivities in continuous culture

The thermophilic methanogenic bacterium, Methanobacterium thermoautotrophicum, was grown on H₂CO₂. In continuous culture, high CH₄ productivities were obtained (288 litres litre⁻¹ day⁻¹) with 96% CH₄ in the effluent gas, i.e. the productivity was twice as high as that obtained previously by other authors, with pure or mixed cultures; the biomass was 3·6 g dry wt litre⁻¹.     

Further photophysical and photochemical characterization of flavins associated with single-shelled vesicles

Summary In order to investigate whether the loop diuretic sensitive, sodium-chloride cotransport system described previously in shark rectal gland is in fact a sodium-potassium chloride cotransport system, plasma membrane vesicles were isolated from rectal glands ofSqualus acanthias and sodium and rubidium uptake were measured by a rapid filtration technique. In addition, the binding of N-methylfurosemide to the membranes was investigated. Sodium uptake into the vesicles in the presence of a 170mm KCl gradient was initially about five-fold higher than in the presence of a 170mm KNO₃ gradient. In the presence of chloride, sodium uptake was inhibited 56% by 0.4mm bumetanide and 40% by 0.8mm N-methylfurosemide. When potassium chloride was replaced by choline chloride or lithium chloride, sodium uptake decreased to the values observed in the presence of potassium nitrate. Replacement of potassium chloride by rubidium chloride, however, did not change sodium uptake. Initial rubidium uptake into the membrane vesicles was about 2.5-fold higher in the presence of a 170mm NaCl gradient than in the presence of a 170mm NaNO₃ gradient. The effect of chloride was completely abolished by 0.4mm bumetanide. Replacement of the sodium chloride gradient by a lithium chloride gradient decreased rubidium uptake by about 40%; replacement by a choline chloride gradient reduced the uptake even further. Rubidium uptake was also strongly inhibited by potassium. Sodium chloride dependence and bumetanide inhibition of rubidium flux were also found in tracer exchange experiments in the absence of salt gradients. The isolated plasma membranes bound³[H]-N-methylfurosemide in a dose-dependent manner. In Scatchard plots, one saturable component could be detected with an apparentK _D of 3.5×10^–6 m and a number of sitesn of 104 pmol/mg protein. At 0.8 m, N-methylfurosemide binding decreased 51% when sodium-free or low-potassium media were used. The same decrease was observed when the chloride concentration was increased from 200 to 600mm or when 1mm bumetanide or furosemide were added to the incubation medium. These studies indicate that the sodium-chloride cotransport system described previously in the rectal gland is in fact a sodium-potassium chloride cotransport system. It is postulated that this transport system plays an essential role in the secondary active chloride secretion of the rectal gland.     

Halide interaction with phospholipids: proton magnetic resonance studies

Water dispersions of egg phosphatidyl choline, dioleoyl phosphatidyl choline and lyso egg phosphatidyl choline have been studied by means of 220 MHz proton magnetic resonance techniques. The N⁺(CH₃)₃ proton signal, for phosphatidyl choline vesicles, consists of two components. The two components are thought to arise from N⁺(CH₃)₃ groups interior and exterior to the phosphatidyl choline vesicle. Anions were found to increase the separation of the two components. The effectiveness of the anions follows their order in the lyotropic series. For a given anion, the increase in component separation depends on the nature of the phospholipid. Iodine was found to modify the anion effect. The results are related to the results of other workers on water transport across lipid bilayer membranes and on phospholipid-halide-binding.