The biogeochemical cycle of the adsorbed template

Experimental results are presented for the verification of the first adsorption step of the ‘adsorbed template’ biogeochemical cycle, a simple model for a primitive prebiotic replication system. The adsorption of Poly-C, Poly-U, Poly-A, Poly-G, and 5′-AMP, 5′-GMP, 5′-CMP and 5′-UMP onto gypsum was studied. It was found that under the conditions of the experiment, the polymers have a very high affinity for the mineral surface, while the monomers adsorb much less efficiently.     

Self-condensation of activated dinucleotides on polynucleotide templates with alternating sequences

We have prepared substantial quantities of the alternating polymers poly(U-G) and poly(C-A) and have used them as templates for the self-condensation of ImpApC, ImpCpA, ImpGpU and ImpG. We find that the condensation of ImpGpU and ImpUpG on poly(C-A) is efficient, the condensation of ImpCpA on poly(U-G) is moderately efficient, while the condensation of ImpApC on poly(U-C) proceeds poorly. In many cases, the product is predominantly 3'-5'-linked. These reactions demonstrate unequivocally, for the first time, that template-directed reactions occur in double-helical structures. Furthermore, they describe for the first time a pair of reactions in which each of two complementary polymers facilitates the synthesis of the other. The prebiotic significance of these findings is discussed.     

Microbiological regulation of the biogeochemical nitrogen cycle

Most nitrogen transformations in soil are carried out by micro-organisms. An understanding of the microbiological processes is thus necessary in order for us to devise management practices in agricultural ecosystems, which will optimize plant root uptake of nitrogen and minimize nitrogen losses from the systems. Some aspects of the individual microbiological processes in the nitrogen cycle are discussed and their importance for an efficient management of agroecosystems. In soil various groups of organisms compete for available inorganic nitrogen and quantitative data are needed on the uptake kinetics for these various groups in order to be able to assess their competitive ability under different conditions. The influence of abiotic factors such as oxygen concentration, inorganic nitrogen concentration and pH is discussed in relation to the different processes. The importance of acetylene as a tool in nitrogen cycling studies is discussed briefly.     

On the association of reverse transcriptase with polynucleotide templates during catalysis.

The association of avian myeloblastosis virus (AMV) DNA polymerase with polynucleotide templates during catalysis has been studied. During the course of polymerization, different template-primer complexes were added and the ability of the enzyme to switch from one polynucleotide template to another was determined. At 37 degrees C as well as at 4 degrees C, the polymerase is able to switch from certain template-primer complexes to others. For example, the addition of poly(A)-oligo(dT) during the course of synthesis with poly(C)-oligo(dG) results in the immediate cessation of dGMP polymerization and the start of dTMP polymerization without any lag. Early during the course of polymerization, the size of the product, as determined by alkaline sucrose gradient centrifugation, is, in part, a function of the ratio of the template-primer complex to the enzyme. These cumulative experiments indicate that catalysis on polynucleotide templates with avian myeloblastosis virus DNA polymerase under the conditions tested is not processive in a classical sense. Similar to cellular DNA polymerases the enzyme can shift from one template-primer to another. Using autoradiography after gel electrophoresis to estimate the product size, it can be calculated that the enzyme switches from one template to another within 0.25 min at 37 degrees C which corresponds to the incorporation of greater than 25 nucleotides. At 4 degrees C, switching can be calculated to occur in less than three nucleotide addition steps. Thus, with certain homopolymers, conditions can be found by which AMV DNA polymerase can switch from one template-primer complex to another, perhaps after each nucleotide addition step.     

The effect of antibiotics on the T4 polynucleotide ligase catalyzed template dependent polymerization of oligodeoxythymidylates.

The poly(dA) dependent T4 polynucleotide ligase catalyzed polymerization of oligodeoxythymidylates is dependent upon duplex stability. The antibiotics ethidium bromide, netropsin and Hoechst 33258 stabilize the duplex poly(dA) . P(dT)n (n = 6-10) to thermal denaturation. Ethidium bromide to DNA ratio of 1.25 and netropsin or Hoechst 33258 to DNA ratio of 0.1 the Tm of d(pT) 10 . poly (dA) was increased by 10 degrees and 25 degrees C respectively. The T4 polynucleotide ligase activity was not inhibited under these conditions and temperature optimum of joining of d(pT) 10 . poly(dA) was increased 5 degrees to 10 degrees by the binding of the antibiotics. Duplexes containing shorter oligodeoxythymidylates required lower concentrations of the antibiotics netropsin or Hoechst 33258 to show no inhibition of T4 polynucleotide ligase. The temperature optima of joining the duplexes d(pT)6 . POLY(DA) and d(pT) 8 . poly(dA) were increased by 5 degrees C upon binding of the antibiotics. Polyacrylamide gel analysis of the T4 polynucleotide ligase catalyzed joining of the oligodeoxythymidylates showed that the presence of antibiotics affected the product distribution of the polymerized oligomers.     

Effect of polynucleotide adsorption on characteristics of a planar phosphatidylcholine bilayer membrane

Interaction of DNA with planar bilayer phosphatidylcholine membrane in the presence of CaCl2 increases electric conductance of the membrane several times as a result of the formation of DNA-membrane complex. The same effect was observed in the cases of ribosomal RNA and synthetic homopolymers polyA, polyU and polyA X polyU double helix.     

A template matching model for pattern recognition: Self-organization of templates and template matching by a disinhibitory neural network

A template matching model for pattern recognition is proposed. By following a previouslyproposed algorithm for synaptic modification (Hirai, 1980), the template of a stimulus pattern is selforganized as a spatial distribution pattern of matured synapses on the cells receiving modifiable synapses. Template matching is performed by the disinhibitory neural network cascaded beyond the neural layer composed of the cells receiving the modifiable synapses. The performance of the model has been simulated on a digital computer. After repetitive presentations of a stimulus pattern, a cell receiving the modifiable synapses comes to have the template of that pattern. And the cell in the latter layer of the disinhibitory bitory neural network that receives the disinhibitory input from that cell becomes electively sensitive to that pattern. Learning patterns are not restricted by previously learned ones. They can be subset or superset patterns of the ones previously learned. If an unknown pattern is presented to the model, no cell beyond the disinhibitory neural network will respond. However, if previously learned patterns are embedded in that pattern, the cells which have the templates of those patterns respond and are assumed to transmit the information to higher center. The computer simulation also shows that the model can organize a clean template under a noisy environment.     

生物地球化学锰循环中的微生物胞外电子传递机制

微生物是生物地球化学元素循环的重要驱动者,在锰等变价金属元素的氧化还原过程中起着至关重要的作用。近年来,Mn(Ⅲ)的发现以及在一些环境中的广泛存在,丰富了人们对Mn(Ⅲ)以及自然界锰循环过程的认识。研究发现,锰的生物地球化学循环,尤其是锰还原过程,与微生物胞外电子传递紧密相关,且目前已知的5种胞外电子传递机制均与锰还原有关联。因此,本文综述了锰的生物地球化学循环及其意义,并从微生物胞外电子传递的机制、微生物介导锰氧化、微生物介导锰还原等3个方面来介绍参与锰循环的微生物多样性;以及微生物地球化学锰循环的环境意义。对微生物参与锰循环过程的研究不仅可以进一步丰富相关理论,同时也能推动生物除锰、污染物原位修复及生物冶金等应用领域的发展。     

Precipitation of barite by Myxococcus xanthus: possible implications for the biogeochemical cycle of barium

Bacterial precipitation of barite (BaSO(4)) under laboratory conditions is reported for the first time. The bacterium Myxococcus xanthus was cultivated in a solid medium with a diluted solution of barium chloride. Crystallization occurred as a result of the presence of live bacteria and the bacterial metabolic activity. A phosphorous-rich amorphous phase preceded the more crystalline barite formation. These experiments may indicate the involvement of bacteria in the barium biogeochemical cycle, which is closely related to the carbon cycle.     

Single-cell determination of iron content in magnetotactic bacteria: implications for the iron biogeochemical cycle

Magnetotactic bacteria (MTB) are ubiquitous aquatic microorganisms that mineralize dissolved iron into intracellular magnetic crystals. After cell death, these crystals are trapped into sediments that remove iron from the soluble pool. MTB may significantly impact the iron biogeochemical cycle, especially in the ocean where dissolved iron limits nitrogen fixation and primary productivity. A thorough assessment of their impact has been hampered by a lack of methodology to measure the amount of, and variability in, their intracellular iron content. We quantified the iron mass contained in single MTB cells of Magnetospirillum magneticum strain AMB-1 using a time-resolved inductively coupled plasma-mass spectrometry methodology. Bacterial iron content depends on the external iron concentration, and reaches a maximum value of ~10⁻⁶ ng of iron per cell. From these results, we calculated the flux of dissolved iron incorporation into environmental MTB populations and conclude that MTB may mineralize a significant fraction of dissolved iron into crystals.     

Selective adsorption of phosphoproteins on gel-immobilized ferric chelate

Ferric ions are very strongly adsorbed to iminodiacetic acid substituted agarose. This firmly immobilized complex acts as a selective immobilized metal affinity adsorbent for phosphoproteins. Chromatography based on this principle is illustrated by the adsorption-desorption behavior of egg yolk phosvitin before and after dephosphorylation as well as by the change in the chromatographic pattern before and after enzymic phosphorylation of selected histones. The strength of binding is dependent on the phosphate content. The difference in binding before and after phosphorylation of a single amino acid residue is demonstrated. Affinity elution can be accomplished by inclusion in the buffer of phosphoserine or a displacing metal ion such as Mg2+.     

Lack of steady-state in the global biogeochemical Si cycle: emerging evidence from lake Si sequestration

Weathering of silicate minerals releases dissolved silicate (DSi) to the soil-vegetation system. Accumulation and recycling of this DSi by terrestrial ecosystems creates a pool of reactive Si on the continents that buffers DSi export to the ocean. Human perturbations to the functioning of the buffer have been a recent research focus, yet a common assumption is that the continental Si cycle is at steady-state. However, we have no good idea of the timescales of ecosystem Si pool equilibration with their environments. A review of modelling and geochemical considerations suggests the modern continental Si cycle is in fact characterised in the long-term by an active accumulation of reactive Si, at least partially attributable to lakes and reservoirs. These lentic systems accumulate Si via biological conversion of DSi to biogenic silica (BSi). An analysis of new and published data for nearly 700 systems is presented to assess their contribution to the accumulating continental pool. Surface sediment BSi concentrations (n = 692) vary between zero and >60 % SiO₂ by weight, apparently independently of lake size, location or water chemistry. Using sediment core BSi accumulation rates (n = 109), still no relationships are found with lake or catchment parameters. However, issues associated with single-core accumulation rates should in any case preclude their use in elemental accumulation calculations. Based on lake/reservoir mass-balances (n = 34), our best global-scale estimate of combined lake and reservoir Si retention is 1.53 TMol year^?1, or 21–27 % of river DSi export. Again, no scalable relationships are apparent, suggesting Si retention is a complex process that varies from catchment to catchment. The lake Si sink has implications for estimation of weathering flux generation from river chemistry. The size of the total continental Si pool is poorly constrained, as is its accumulation rate, but lakes clearly contribute substantially. A corollary to this emerging understanding is that the flux and isotopic composition of DSi delivered to the ocean has likely varied over time, partly mediated by a fluctuating continental pool, including in lakes.     

影响荧光终止法PCR循环测序反应的因素

比较了一些影响荧光终止法ＰＣＲ循环测序反应的因素。实验结果显示在Ｂｅｃｋｍａｎ ＣＥＱ２０００自动测序仪上,可读序列长度随着ｐＵＣ１８模板量增加而逐渐增多,当模板量达到１２５ｎｇ时ＤＮＡ可读序列最长,以后随着ｐＵＣ１８量增加测序长度逐渐下降。当引物量是１μｌ时,其测序结果比用０．５μｌ引物时好。在同样模板量情况下,１０μｌ反应体积比５μｌ反应体积可读序列长。     

Study on the structure-function relationship of polynucleotide phosphorylase: model of a proteolytic degraded polynucleotide phosphorylase.

It is already known that modification of E. coli polynucleotide phosphorylase by endogenous proteolysis induces drastic changes in both phosphorolysis and polymerisation reactions. The structural parameters of the proteolysed polynucleotide phosphorylase are described. The phosphorolysis of polynucleotide, which is quite progressive for the native enzyme, is shown to be only partially progressive for the degraded enzyme, owing to the loss of polymer attachment sites.     

Quantitative surface studies of protein adsorption by infrared spectroscopy. II. Quantification of adsorbed and bulk proteins

Attenuated total reflectance Fourier transform infrared spectra of surface-adsorbed proteins are correlated with concentration measurements determined by 125I-labeled proteins. This paper demonstrates that linear correlations between the intensity of the major bands of proteins and the quantity of proteins can be obtained for human albumin and immunoglobulin G up to surface concentrations of approximately 0.25 microgram/cm2. A poorer correlation was observed for human fibrinogen. A linear correlation was also observed between the concentration in the bulk solution and the major bands of albumin up to a concentration of 60 mg/ml.     

The biogeochemical cycle of methane in the coastal zone and littoral of the Kandalaksha Bay of the White Sea

Microbiological and biogeochemical investigations of the processes of methane production (MP) and methane oxidation (MO) in the coastal waters and littoral of the Kandalaksha Bay of the White Sea were carried out. The studies were conducted in the coastal zones and in the water areas of the Kandalaksha Preserve, Moscow University White Sea Biological Station, and Zoological Institute (RAS) Biological Station in August, 1999, 2000, and 2001 and in March, 2001. The rate of CO2 assimilation in the shallow and littoral sediments was 35-27800 microg C/(dm3 day) in summer and 32.8-88.9 microg C/(dm3 day) in winter. The maximal rates of MP were observed in the littoral sediments in the zone of macrophyte decomposition, in local depressions, and in the estuary of a freshwater creak (up to 113 microl/(dm3 day)). The maximal level of MO was observed in the shallow estuarine sediments (up to 2450 microl/(dm3 day)). During the winter season, at the temperature of -0.5 to 0.5 degrees C, the MP rate in the littoral sediments was 0.02-0.3 microl/(dm3 day), while MO rate was 0.06-0.7 microl/(dm3 day). The isotopic data obtained indicate that the C(org) of the mats and of the upper sediment layers is enriched with the heavy 13C isotope by 1-4 per thousand as compared to the C(org) of the suspension, comprised on 33.5-34.3% of phytoplankton. A striking difference was found between the levels of methane emission by the typical littoral microlanscapes. In fine sediments, the average emission was 675 microl CH4/(m2 day), in the stormy discharge stretch sediments it was 1670 microl CH4/(m2 day), and under the stones and in silted pits, 1370 microl CH4/(m2 day). The calculation performed with consideration of the microlandscape areas with a high production allowed the CH4 production of 1 km2 of the littoral to be estimated as 192-300 1 CH4/(km2 day).     

Configuration-dependent properties of randomly coiling polynucleotide chains. II. The role of the phosphodiester linkage

The dependence of the unperturbed dimensions of randomly coiling polynucleotides on the rotations about the phosphodiester linkages of the chain has been examined in order to understand the conformational discrepancies, set forth in paper I, regarding these angles (ω′ and ω). Large values of the characteristic ratio 〈r²〉₀/nl² , which agree with the experimental behavior of the chain, are obtained only if a sizeable proportion of the polymer residues have trans ω′ values. The asymmetric torsional potential that is believed to arise from gauche effects associated with the P-O bonds has been approximated using a hard core model. The calculated characteristic ratio exhibits a strong dependence upon the magnitude of this torsional barrier (separating trans and gauche conformations) and shows agreement with experimental values for polyribonucleotides only if this energy difference is 1 kcal/mol or less.     

Cooperative nonenzymic base recognition. Kinetics of the binding of a base monomer to a complementary polynucleotide template

The kinetics of double-helix formation by poly U and the complementary monomer N-6,9-dimethyladenine (m⁶m⁹A) has been measured using a new fast temperature-jump apparatus. The cooperative binding kinetics are complicated by the extensive self-association of the monomers, but a satisfactory analysis using average relaxation times was possible in terms of three different models. Application of a model which considers only monomer binding yields the upper limit for the binding rate constant of an m⁶m⁹A monomer next to an already bound monomer on a poly U strand: (2 ± 0.4) × 10⁸ M^?1sec^?1. A lower limit is found by using a model which allows for binding of all m⁶m⁹A stacks to poly U with equal rate constants: (3 ± 0.3) × 10⁷ M^?1sec^?1. A third model with “weighted” rate constants consistent with the data: (7.5 ± 1.0) × 10⁷ M^?1sec^?1. The rate of cooperative binding of m⁶m⁹A to the trimer UpUpU has also been measured. The rate constants obtained with the trimer agree with those obtained with the polymer for each of the three models within experimental error.