@article {1737, title = {Methane cycling. Nonequilibrium clumped isotope signals in microbial methane.}, journal = {Science}, volume = {348}, year = {2015}, month = {2015 Apr 24}, pages = {428-31}, abstract = {

Methane is a key component in the global carbon cycle, with a wide range of anthropogenic and natural sources. Although isotopic compositions of methane have traditionally aided source identification, the abundance of its multiply substituted "clumped" isotopologues (for example, (13)CH3D) has recently emerged as a proxy for determining methane-formation temperatures. However, the effect of biological processes on methane{\textquoteright}s clumped isotopologue signature is poorly constrained. We show that methanogenesis proceeding at relatively high rates in cattle, surface environments, and laboratory cultures exerts kinetic control on (13)CH3D abundances and results in anomalously elevated formation-temperature estimates. We demonstrate quantitatively that H2 availability accounts for this effect. Clumped methane thermometry can therefore provide constraints on the generation of methane in diverse settings, including continental serpentinization sites and ancient, deep groundwaters.

}, keywords = {Animals, Carbon Cycle, Carbon Isotopes, Cattle, Groundwater, Hydrogen, Methane, Methanomicrobiales, Temperature}, issn = {1095-9203}, doi = {10.1126/science.aaa4326}, author = {Wang, David T and Gruen, Danielle S and Lollar, Barbara Sherwood and Hinrichs, Kai-Uwe and Stewart, Lucy C and Holden, James F and Hristov, Alexander N and Pohlman, John W and Morrill, Penny L and K{\"o}nneke, Martin and Delwiche, Kyle B and Reeves, Eoghan P and Sutcliffe, Chelsea N and Ritter, Daniel J and Seewald, Jeffrey S and McIntosh, Jennifer C and Hemond, Harold F and Kubo, Michael D and Cardace, Dawn and Hoehler, Tori M and Ono, Shuhei} } @article {1206, title = {Hydrogen-limited growth of hyperthermophilic methanogens at deep-sea hydrothermal vents.}, journal = {Proc Natl Acad Sci U S A}, volume = {109}, year = {2012}, month = {2012 Aug 21}, pages = {13674-9}, abstract = {

Microbial productivity at hydrothermal vents is among the highest found anywhere in the deep ocean, but constraints on microbial growth and metabolism at vents are lacking. We used a combination of cultivation, molecular, and geochemical tools to verify pure culture H(2) threshold measurements for hyperthermophilic methanogenesis in low-temperature hydrothermal fluids from Axial Volcano and Endeavour Segment in the northeastern Pacific Ocean. Two Methanocaldococcus strains from Axial and Methanocaldococcus jannaschii showed similar Monod growth kinetics when grown in a bioreactor at varying H(2) concentrations. Their H(2) half-saturation value was 66 μM, and growth ceased below 17-23 μM H(2), 10-fold lower than previously predicted. By comparison, measured H(2) and CH(4) concentrations in fluids suggest that there was generally sufficient H(2) for Methanocaldococcus growth at Axial but not at Endeavour. Fluids from one vent at Axial (Marker 113) had anomalously high CH(4) concentrations and contained various thermal classes of methanogens based on cultivation and mcrA/mrtA analyses. At Endeavour, methanogens were largely undetectable in fluid samples based on cultivation and molecular screens, although abundances of hyperthermophilic heterotrophs were relatively high. Where present, Methanocaldococcus genes were the predominant mcrA/mrtA sequences recovered and comprised \~{}0.2-6\% of the total archaeal community. Field and coculture data suggest that H(2) limitation may be partly ameliorated by H(2) syntrophy with hyperthermophilic heterotrophs. These data support our estimated H(2) threshold for hyperthermophilic methanogenesis at vents and highlight the need for coupled laboratory and field measurements to constrain microbial distribution and biogeochemical impacts in the deep sea.

}, keywords = {Archaea, Biodiversity, Coculture Techniques, DNA, Ribosomal, Ecosystem, Gases, Geography, Hydrogen, Hydrothermal Vents, Kinetics, Methane, Molecular Sequence Data, Temperature, Time Factors, Water Microbiology}, issn = {1091-6490}, doi = {10.1073/pnas.1206632109}, author = {Ver Eecke, Helene C and Butterfield, David A and Huber, Julie A and Lilley, Marvin D and Olson, Eric J and Roe, Kevin K and Evans, Leigh J and Merkel, Alexandr Y and Cantin, Holly V and Holden, James F} } @article {372, title = {Metagenomic analysis of a permafrost microbial community reveals a rapid response to thaw.}, journal = {Nature}, volume = {480}, year = {2011}, month = {2011 Dec 15}, pages = {368-71}, abstract = {Permafrost contains an estimated 1672 Pg carbon (C), an amount roughly equivalent to the total currently contained within land plants and the atmosphere. This reservoir of C is vulnerable to decomposition as rising global temperatures cause the permafrost to thaw. During thaw, trapped organic matter may become more accessible for microbial degradation and result in greenhouse gas emissions. Despite recent advances in the use of molecular tools to study permafrost microbial communities, their response to thaw remains unclear. Here we use deep metagenomic sequencing to determine the impact of thaw on microbial phylogenetic and functional genes, and relate these data to measurements of methane emissions. Metagenomics, the direct sequencing of DNA from the environment, allows the examination of whole biochemical pathways and associated processes, as opposed to individual pieces of the metabolic puzzle. Our metagenome analyses reveal that during transition from a frozen to a thawed state there are rapid shifts in many microbial, phylogenetic and functional gene abundances and pathways. After one week of incubation at 5 {\textdegree}C, permafrost metagenomes converge to be more similar to each other than while they are frozen. We find that multiple genes involved in cycling of C and nitrogen shift rapidly during thaw. We also construct the first draft genome from a complex soil metagenome, which corresponds to a novel methanogen. Methane previously accumulated in permafrost is released during thaw and subsequently consumed by methanotrophic bacteria. Together these data point towards the importance of rapid cycling of methane and nitrogen in thawing permafrost.}, keywords = {Alaska, Arctic Regions, Bacteria, Carbon, Carbon Cycle, DNA, Freezing, Genes, rRNA, Metagenome, Metagenomics, Methane, Nitrogen, Nitrogen Cycle, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Soil, Soil Microbiology, Temperature, Time Factors}, issn = {1476-4687}, doi = {10.1038/nature10576}, author = {Mackelprang, Rachel and Waldrop, Mark P and Deangelis, Kristen M and David, Maude M and Chavarria, Krystle L and Blazewicz, Steven J and Rubin, Edward M and Jansson, Janet K} } @article {500, title = {Quantifying expression of a dissimilatory (bi)sulfite reductase gene in petroleum-contaminated marine harbor sediments.}, journal = {Microb Ecol}, volume = {55}, year = {2008}, month = {2008 Apr}, pages = {489-99}, abstract = {The possibility of quantifying in situ levels of transcripts for dissimilatory (bi)sulfite reductase (dsr) genes to track the activity of sulfate-reducing microorganisms in petroleum-contaminated marine harbor sediments was evaluated. Phylogenetic analysis of the cDNA generated from mRNA for a ca. 1.4 kbp portion of the contiguous dsrA and dsrB genes suggested that Desulfosarcina species, closely related to cultures known to anaerobically oxidize aromatic hydrocarbons, were active sulfate reducers in the sediments. The levels of dsrA transcripts (per mug total mRNA) were quantified in sediments incubated anaerobically at the in situ temperature as well as in sediments incubated at higher temperatures and/or with added acetate to increase the rate of sulfate reduction. Levels of dsrA transcripts were low when there was no sulfate reduction because the sediments were depleted of sulfate or if sulfate reduction was inhibited with added molybdate. There was a direct correlation between dsrA transcript levels and rates of sulfate reduction when sulfate was at ca. 10 mM in the various sediment treatments, but it was also apparent that within a given sediment, dsrA levels increased over time as long as sulfate was available, even when sulfate reduction rates did not increase. These results suggest that phylogenetic analysis of dsr transcript sequences may provide insight into the active sulfate reducers in marine sediments and that quantifying levels of dsrA transcripts can indicate whether sulfate reducers are active in particular sediment. Furthermore, it may only be possible to use dsrA transcript levels to compare the relative rates of sulfate reduction in sediments when sulfate concentrations, and possibly other environmental conditions, are comparable.}, keywords = {Anaerobiosis, Desulfitobacterium, DNA, Bacterial, DNA, Ribosomal, Gene Expression, Geologic Sediments, Hydrogensulfite Reductase, Molecular Sequence Data, Petroleum, Phylogeny, RNA, Bacterial, RNA, Messenger, RNA, Ribosomal, 16S, Temperature}, issn = {0095-3628}, doi = {10.1007/s00248-007-9294-2}, author = {Chin, Kuk-Jeong and Sharma, Manju L and Russell, Lyndsey A and O{\textquoteright}Neill, Kathleen R and Lovley, Derek R} } @article {1212, title = {Characterization of malate dehydrogenase from the hyperthermophilic archaeon Pyrobaculum islandicum.}, journal = {Extremophiles}, volume = {11}, year = {2007}, month = {2007 Sep}, pages = {741-6}, abstract = {

Native and recombinant malate dehydrogenase (MDH) was characterized from the hyperthermophilic, facultatively autotrophic archaeon Pyrobaculum islandicum. The enzyme is a homotetramer with a subunit mass of 33 kDa. The activity kinetics of the native and recombinant proteins are the same. The apparent K ( m ) values of the recombinant protein for oxaloacetate (OAA) and NADH (at 80 degrees C and pH 8.0) were 15 and 86 microM, respectively, with specific activity as high as 470 U mg(-1). Activity decreased more than 90\% when NADPH was used. The catalytic efficiency of OAA reduction by P. islandicum MDH using NADH was significantly higher than that reported for any other archaeal MDH. Unlike other archaeal MDHs, specific activity of the P. islandicum MDH back-reaction also decreased more than 90\% when malate and NAD(+) were used as substrates and was not detected with NADP(+). A phylogenetic tree of 31 archaeal MDHs shows that they fall into 5 distinct groups separated largely along taxonomic lines suggesting minimal lateral mdh transfer between Archaea.

}, keywords = {Citric Acid Cycle, Hydrogen-Ion Concentration, Kinetics, Malate Dehydrogenase, Malates, Molecular Weight, NAD, NADP, Oxaloacetic Acid, Phylogeny, Protein Conformation, Protein Subunits, Pyrobaculum, Recombinant Proteins, Sequence Analysis, Protein, Substrate Specificity, Temperature}, issn = {1431-0651}, doi = {10.1007/s00792-007-0081-2}, author = {Yennaco, Lynda J and Hu, Yajing and Holden, James F} } @article {506, title = {Reclassification of Trichlorobacter thiogenes as Geobacter thiogenes comb. nov.}, journal = {Int J Syst Evol Microbiol}, volume = {57}, year = {2007}, month = {2007 Mar}, pages = {463-6}, abstract = {Reclassification of the species Trichlorobacter thiogenes as Geobacter thiogenes comb. nov. is proposed on the basis of physiological traits and phylogenetic position. Characteristics additional to those provided in the original description revealed that the type strain (strain K1(T)=ATCC BAA-34(T)=JCM 14045(T)) has the ability to use Fe(III) as an electron acceptor for acetate oxidation and has an electron donor and acceptor profile typical of a Geobacter species, contains abundant c-type cytochromes, and has a temperature optimum of 30 degrees C and a pH optimum near pH 7.0; traits typical of members of the genus Geobacter. Phylogenetic analysis of nifD, recA, gyrB, rpoB, fusA and 16S rRNA genes further indicated that T. thiogenes falls within the Geobacter cluster of the family Geobacteraceae. Based on extensive phylogenetic evidence and the fact that T. thiogenes has the hallmark physiological characteristics of a Geobacter species, Trichlorobacter thiogenes should be reclassified as a member of the genus Geobacter.}, keywords = {DNA, Bacterial, DNA, Ribosomal, Genes, Bacterial, Geobacter, Phylogeny, RNA, Ribosomal, 16S, Temperature}, issn = {1466-5026}, doi = {10.1099/ijs.0.63408-0}, author = {Nevin, Kelly P and Holmes, Dawn E and Woodard, Trevor L and Covalla, Sean F and Lovley, Derek R} } @article {749, title = {Desiccation responses and survival of Sinorhizobium meliloti USDA 1021 in relation to growth phase, temperature, chloride and sulfate availability.}, journal = {Lett Appl Microbiol}, volume = {42}, year = {2006}, month = {2006 Feb}, pages = {172-8}, abstract = {AIMS: To identify physical and physiological conditions that affect the survival of Sinorhizobium meliloti USDA 1021 during desiccation. METHODS AND RESULTS: An assay was developed to study desiccation response of S. meliloti USDA 1021 over a range of environmental conditions. We determined the survival during desiccation in relation to (i) matrices and media, (ii) growth phase, (iii) temperature, and (iv) chloride and sulfate availability. CONCLUSIONS: This study indicates that survival of S. meliloti USDA 1021 during desiccation is enhanced: (i) when cells were dried in the stationary phase, (ii) with increasing drying temperature at an optimum of 37 degrees C, and (iii) during an increase of chloride and sulfate, but not sodium or potassium availability. In addition, we resolved that the best matrix to test survival was nitrocellulose filters. SIGNIFICANCE AND IMPACT OF THE STUDY: The identification of physical and physiological factors that determine the survival during desiccation of S. meliloti USDA 1021 may aid in (i) the strategic development of improved seed inocula, (ii) the isolation, and (iii) the development of rhizobial strains with improved ability to survive desiccation. Furthermore, this work may provide insights into the survival of rhizobia under drought conditions.}, keywords = {Bacteriological Techniques, Chlorides, Desiccation, Models, Biological, Sinorhizobium meliloti, Sulfur Oxides, Temperature}, issn = {0266-8254}, doi = {10.1111/j.1472-765X.2005.01808.x}, author = {Vriezen, J A C and de Bruijn, F J and N{\"u}sslein, K} } @article {822, title = {Allele specific synthetic lethality between priC and dnaAts alleles at the permissive temperature of 30 degrees C in E. coli K-12.}, journal = {BMC Microbiol}, volume = {4}, year = {2004}, month = {2004}, pages = {47}, abstract = {BACKGROUND: DnaA is an essential protein in the regulation and initiation of DNA replication in many bacteria. It forms a protein-DNA complex at oriC to which DnaC loads DnaB. DNA replication forks initiated at oriC by DnaA can collapse on route to the terminus for a variety of reasons. PriA, PriB, PriC, DnaT, Rep and DnaC form multiple pathways to restart repaired replication forks. DnaC809 and dnaC809,820 are suppressors of priA2::kan mutant phenotypes. The former requires PriC and Rep while the latter is independent of them. RnhA339::cat mutations allow DnaA-independent initiation of DNA replication. RESULTS: It is shown herein that a priC303::kan mutation is synthetically lethal with either a dnaA46 or dnaA508 temperature sensitive mutation at the permissive temperature of 30 degrees C. The priC-dnaA lethality is specific for the dnaA allele. The priC303::kan mutant was viable when placed in combination with either dnaA5, dnaA167, dnaA204 or dnaA602. The priC-dnaA508 and priC-dnaA46 lethality could be suppressed by rnhA339::cat. The priC-dnaA508 lethality could be suppressed by a dnaC809,820 mutation, but not dnaC809. Neither of the dnaC mutations could suppress the priC-dnaA46 lethality. CONCLUSIONS: A hitherto unknown function for either DnaA in replication restart or PriC in initiation of DNA replication that occurs in certain dnaA temperature sensitive mutant strains at the permissive temperature of 30 degrees C has been documented. Models considering roles for PriC during initiation of DNA replication and roles for DnaA in replication restart were tested and found not to decisively explain the data. Other roles of dnaA in transcription and nucleoid structure are additionally considered.}, keywords = {Alleles, Bacterial Proteins, DNA Replication, DNA-Binding Proteins, Escherichia coli K12, Escherichia coli Proteins, Gene Expression Regulation, Bacterial, Genes, Lethal, Mutation, Temperature}, issn = {1471-2180}, doi = {10.1186/1471-2180-4-47}, author = {Hinds, Tania and Sandler, Steven J} } @article {546, title = {Potential role of a novel psychrotolerant member of the family Geobacteraceae, Geopsychrobacter electrodiphilus gen. nov., sp. nov., in electricity production by a marine sediment fuel cell.}, journal = {Appl Environ Microbiol}, volume = {70}, year = {2004}, month = {2004 Oct}, pages = {6023-30}, abstract = {Previous studies have shown that members of the family Geobacteraceae that attach to the anodes of sediment fuel cells are directly involved in harvesting electricity by oxidizing organic compounds to carbon dioxide and transferring the electrons to the anode. In order to learn more about this process, microorganisms from the anode surface of a marine sediment fuel cell were enriched and isolated with Fe(III) oxide. Two unique marine isolates were recovered, strains A1(T) and A2. They are gram-negative, nonmotile rods, with abundant c-type cytochromes. Phylogenetic analysis of the 16S rRNA, recA, gyrB, fusA, rpoB, and nifD genes indicated that strains A1(T) and A2 represent a unique phylogenetic cluster within the Geobacteraceae. Both strains were able to grow with an electrode serving as the sole electron acceptor and transferred ca. 90\% of the electrons available in their organic electron donors to the electrodes. These organisms are the first psychrotolerant members of the Geobacteraceae reported thus far and can grow at temperatures between 4 and 30 degrees C, with an optimum temperature of 22 degrees C. Strains A1(T) and A2 can utilize a wide range of traditional electron acceptors, including all forms of soluble and insoluble Fe(III) tested, anthraquinone 2,6-disulfonate, and S(0). In addition to acetate, both strains can utilize a number of other organic acids, amino acids, long-chain fatty acids, and aromatic compounds to support growth with Fe(III) nitrilotriacetic acid as an electron acceptor. The metabolism of these organisms differs in that only strain A1(T) can use acetoin, ethanol, and hydrogen as electron donors, whereas only strain A2 can use lactate, propionate, and butyrate. The name Geopsychrobacter electrodiphilus gen. nov., sp. nov., is proposed for strains A1(T) and A2, with strain A1(T) (ATCC BAA-880(T); DSM 16401(T); JCM 12469) as the type strain. Strains A1(T) and A2 (ATCC BAA-770; JCM 12470) represent the first organisms recovered from anodes that can effectively couple the oxidation of organic compounds to an electrode. Thus, they may serve as important model organisms for further elucidation of the mechanisms of microbe-electrode electron transfer in sediment fuel cells.}, keywords = {Bioelectric Energy Sources, Cytochromes, Deltaproteobacteria, Electron Transport, Genes, Bacterial, Geologic Sediments, Microscopy, Electron, Molecular Sequence Data, Phylogeny, RNA, Bacterial, RNA, Ribosomal, 16S, Temperature}, issn = {0099-2240}, doi = {10.1128/AEM.70.10.6023-6030.2004}, author = {Holmes, Dawn E and Nicoll, Julie S and Bond, Daniel R and Lovley, Derek R} } @article {1216, title = {Microbe-metal interactions in marine hydrothermal environments.}, journal = {Curr Opin Chem Biol}, volume = {7}, year = {2003}, month = {2003 Apr}, pages = {160-5}, abstract = {

Marine hydrothermal microorganisms respond rapidly to changes in the concentrations and availability of metals within their environment. Hyperthermophilic archaea appear to possess novel mechanisms for metal detoxification, dissimilatory metal reduction and metal assimilation that may be absent in their mesophilic and bacterial counterparts. For example, tungsten was found in high concentrations in a hydrothermal sulfide deposit where hyperthermophiles were also most abundant, consistent with the unique requirement of these organisms for this element. Furthermore, newly isolated genera of iron-reducing hyperthermophiles expand the scope of carbon cycling in hydrothermal environments. The advent of genome sequences and new molecular techniques will facilitate our further understanding of microbe-mineral interactions in these environments.

}, keywords = {Archaea, Bacteria, Environment, Marine Biology, Metals, Seawater, Temperature}, issn = {1367-5931}, author = {Holden, James F and Adams, Michael W W} } @article {606, title = {Differences in Fe(III) reduction in the hyperthermophilic archaeon, Pyrobaculum islandicum, versus mesophilic Fe(III)-reducing bacteria.}, journal = {FEMS Microbiol Lett}, volume = {195}, year = {2001}, month = {2001 Feb 20}, pages = {253-8}, abstract = {The discovery that all hyperthermophiles that have been evaluated have the capacity to reduce Fe(III) has raised the question of whether mechanisms for dissimilatory Fe(III) reduction have been conserved throughout microbial evolution. Many studies have suggested that c-type cytochromes are integral components in electron transport to Fe(III) in mesophilic dissimilatory Fe(III)-reducing microorganisms. However, Pyrobaculum islandicum, the hyperthermophile in which Fe(III) reduction has been most intensively studied, did not contain c-type cytochromes. NADPH was a better electron donor for the Fe(III) reductase activity in P. islandicum than NADH. This is the opposite of what has been observed with mesophiles. Thus, if previous models for dissimilatory Fe(III) reduction by mesophilic bacteria are correct, then it is unlikely that a single strategy for electron transport to Fe(III) is present in all dissimilatory Fe(III)-reducing microorganisms.}, keywords = {Cytochrome c Group, Electron Transport, Ferric Compounds, FMN Reductase, NADH, NADPH Oxidoreductases, NADP, Oxidation-Reduction, Temperature, Thermoproteaceae}, issn = {0378-1097}, author = {Childers, S E and Lovley, D R} } @article {1735, title = {[Spectral properties of porcine plasminogen: study of the acidic transition (author{\textquoteright}s transl)].}, journal = {Eur J Biochem}, volume = {63}, year = {1976}, month = {1976 Apr 1}, pages = {553-62}, abstract = {

The acidic transition of porcine plasminogen, prepared by affinity chromatography, was studied by non-destructive methods. These methods are based on the analysis of the behaviour of the tryptophyls under various conditions. The perturbation of the absorption and emission spectra by pH or temperature and the dynamic quenching of the intrinsic fluorescence are used to obtain information on structural changes which affect the environment of these residues. It is shown that by decreasing pH the fluorescence emission spectra are shifted toward the long wavelengths, with a broadening of the fluorescence band. The same effect can be obtained at constant pH by heating the protein solution. In order to analyze these phenomena, it is assumed that the fluorescence intensities at 355 nm and 328 nm reflect the proportion of the tryptophans which are exposed to the solvent, and buried, respectively. The plot of the ratio of the fluorescence intensities at these wavelengths versus pH or temperature leads to a titration curve showing an unmasking of tryptophans. The proportion of exposed tryptophans is measured by the dynamic fluorescence quenching technique and the data analyzed according to Lehrer. The plot of the fraction of exposed tryptophyls versus pH also shows the unmasking of these chromophores. Thermal perturbation of a solution of plaminogen at neutral pH induces a difference absorption spectrum whose amplitudes at the maxima are proportional to the number of exposed aromatic residues. The comparison with a solution of fully denatured plasminogen in 6 M guanidium chloride, where all the tryptophyls are exposed, shows that the percentage of exposure is equal to 59\%. This number is significantly higher than the percentage found by the fluorescence quenching technique (20\%), indicating that some tryptophyls are located in crevices, exposed to the solvent but not to the iodide. At acidic pH the absorption difference spectra induced by thermal perturbation are not classical, since they show an inversion and a new band between 300 nm and 305 nm. This band is mentioned in the literature as a minor band of tryptophan which appears when this chromophore is located in an asymmetric environment. On plotting the maximum amplitude of these spectra obtained at acidic pH versus temperature, we obtain a curve indicating that two types of antagonistic interactions are involved in the perturbation of the chromophores spectra. The spectrophotometric titration of plasminogen gives classical absorption difference spectra. By plotting the maximum amplitude at 292 nm versus pH, we obtain a titration curve with an apparent pK of 2.9 units. This pK is acidic which respect to the pK value of a normal carboxyl. This low value can be due to a positively charged group in the neighbourhood of a carboxyl, which interacts with one or more chromophores. When the carboxyl becomes protonated, this positively charged group is free and available to perturb the environment of some chromophores...

}, keywords = {Animals, Binding Sites, Guanidines, Hydrogen-Ion Concentration, Plasminogen, Protein Binding, Protein Conformation, Spectrometry, Fluorescence, Spectrophotometry, Spectrophotometry, Ultraviolet, Swine, Temperature}, issn = {0014-2956}, author = {Rodier, F} } @article {1711, title = {Comparison between procaine and isocarboxazid metabolism in vitro by a liver microsomal amidase-esterase.}, journal = {Biochem Pharmacol}, volume = {24}, year = {1975}, month = {1975 Aug 15}, pages = {1517-21}, keywords = {Amidohydrolases, Animals, Esterases, Hydrogen-Ion Concentration, In Vitro Techniques, Isocarboxazid, Kinetics, Male, Metals, Microsomes, Liver, Phospholipids, Procaine, Proteins, Rats, Subcellular Fractions, Temperature}, issn = {0006-2952}, author = {Moroi, K and Sato, T} } @article {1710, title = {Delineation of the intimate details of the backbone conformation of pyridine nucleotide coenzymes in aqueous solution.}, journal = {Biochem Biophys Res Commun}, volume = {66}, year = {1975}, month = {1975 Oct 27}, pages = {1173-9}, keywords = {Fourier Analysis, Magnetic Resonance Spectroscopy, Models, Molecular, Molecular Conformation, NAD, NADP, Structure-Activity Relationship, Temperature}, issn = {0006-291X}, author = {Bose, K S and Sarma, R H} }