Infrequent cavity-forming fluctuations in HPr from Staphylococcus carnosus revealed by pressure- and temperature-dependent tyrosine ring flips

Infrequent structural fluctuations of a globular protein is seldom detected and studied in detail. One tyrosine ring of HPr from Staphylococcus carnosus, an 88-residue phosphocarrier protein with no disulfide bonds, undergoes a very slow ring flip, the pressure and temperature dependence of which is studied in detail using the on-line cell high-pressure nuclear magnetic resonance technique in the pressure range from 3 MPa to 200 MPa and in the temperature range from 257 K to 313 K. The ring of Tyr6 is buried sandwiched between a beta-sheet and alpha-helices (the water-accessible area is less than 0.26 nm2), its hydroxyl proton being involved in an internal hydrogen bond. The ring flip rates 10(1)-10(5) s(-1) were determined from the line shape analysis of H(delta1, delta2) and H(epsilon1,epsilon2) of Tyr6, giving an activation volume DeltaV++ of 0.044 +/- 0.008 nm3 (27 mL mol(-1)), an activation enthalpy DeltaH++ of 89 +/- 10 kJ mol(-1), and an activation entropy DeltaS++ of 16 +/- 2 JK(-1) mol(-1). The DeltaV++) and DeltaH++ values for HPr found previously for Tyr and Phe ring flips of BPTI and cytochrome c fall within the range of DeltaV(double dagger) of 28 to 51 mL mol(-1) and DeltaH++ of 71 to 155 kJ mol(-1). The fairly common DeltaV++ and DeltaH++ values are considered to represent the extra space or cavity required for the ring flip and the extra energy required to create a cavity, respectively, in the core part of a globular protein. Nearly complete cold denaturation was found to take place at 200 MPa and 257 K independently from the ring reorientation process.     

Mass spectrometric method for detecting carbon 13 enrichment introduced by folate coenzymes in uric acid

Using [2-13C]uric acid as a test material, we developed a mass spectrometric procedure that detects and estimates the difference in 13C enrichment at the positions of carbons 2 and 8 of the purine ring. This method could replace radiochemical methods and could trace the incorporation of carbon fragments into the purine ring from 13C-labeled metabolites in humans.     

Mutation in collagen gene induces cardiomyopathy in transgenic mice

In many remodeling tissues, such as the heart, collagen degradation to provide new integrin-binding sites is required for survival. However, complete loss of integrin signaling due to disconnection from extracellular matrix (ECM) leads to apoptosis and dilatation. To test the hypothesis that a mutation in type I collagen gene induces cardiomyopathy, we employed a metalloproteinase-resistant collagen mutant homozygous transgenic male (B6,129-Colla-1) and compared with age-sex matched wildtype C57BL/J6 control mice. At the age of 38-42 weeks, aortic and left ventricle (LV) pressure were measured. The LV wall thickness and diameter were measured by a digital micrometer. The levels of matrix metalloproteinase-2 (MMP-2) activity and cardiospecific tissue inhibitor of metalloproteinase-4 (TIMP-4) were measured by zymography and Western blot analyses, respectively. The levels of collagenolysis were measured by Western blot using anti-collagen antibody. In transgenic and wildtype mice, end-diastolic pressure (EDP) was 8.3 +/- 1.7 and 6.5 +/- 1.1 mmHg; LV diameter was 3.43 +/- 0.07 and 2.94 +/- 0.05 mm; wall thickness was 1.18 +/- 0.03 and 1.28 +/- 0.04 mm; end-diastolic wall stress was 600 +/- 158 and 347 +/- 49 dynes/cm(2), respectively. The increase in LV wall stress was associated with increased MMP-2 activity, increased collagenolysis, and decreased levels of TIMP-4. This leads to reduced elastic compliance in collagen mutant transgenic mice. The occurrence of cardiomyopathy in adult Colla-1 mice may be a significant confounding factor as it may be indicative of increased basal levels of ECM disruption. This phenotype is what would be expected if collagen degradation normally supplies integrin ligands during cardiac muscle remodeling.     

Growing-season precipitation since 1872 in the coastal area of subtropical southeast China reconstructed from tree rings and its relationship with the East Asian summer monsoon system

Tree rings from temperate zones of the world have provided abundant palaeo- ecological and paleo-hydroclimatic information. However, tree rings from subtropical to tropical regions remain relatively scarce, which greatly limit our fully understanding about the climate change issues. In the present work, tree-ring-width (TRW) measurements of Masson pine from Fujian province, the coastal area of subtropical southeast China were successfully crossdated and a TRW STD chronology was developed from 1854 to 2012. Significantly positive correlation was identified between the tree rings and April–November total precipitation (r = 0.71, p < 0.01). The reconstructed April–November precipitation exhibited two comparatively wet (1876–1886 and 1957–1962) and one comparatively dry (1986–2004) periods. An evident drying trend since 1959 was seen and it was mitigated after 1993. Most of the extreme low-precipitation years in the reconstruction were supported by the historical records. As revealed by the spatial correlation patterns, our precipitation reconstruction was also consistent with other hydroclimatic records along the coastal areas of southeast China, proving its ability to capture the large-scale hydrological signal in southeast China (mainly refers to the south of the middle-lower reaches of Yangtze River). The reconstructed precipitation showed significant correlation with the East Asian summer Monsoon (EASM) index. Moreover, it also indicated simultaneous variation with the monsoon precipitation in North China on a decadal scale, implying that growing season precipitation variations in both regions were influenced by the EASM strength. This work highlights the potential of using tree-ring width to reconstruct precipitation in subtropical southeast China, while the relevant issues about precipitation variation in this region is far from resolved.     

Distinct Stages of Protein Evolution as Suggested by Protein Sequence Analysis

Evolution of proteins encoded in nucleotide sequences began with the advent of the triplet code. The chronological order of the appearance of amino acids on the evolution scene and the steps in the evolution of the triplet code have been recently reconstructed (Trifonov, 2000b) on the basis of 40 different ranking criteria and hypotheses. According to the consensus chronology, the pair of complementary GGC and GCC codons for the amino acids alanine and glycine appeared first. Other codons appeared as complementary pairs as well, which divided their respective amino acids into two alphabets, encoded by triplets with either central purines or central pyrimidines: G, D, S, E, N, R, K, Q, C, H, Y, and W (Glycine alphabet G) and A, V, P, S, L, T, I, F, and M (Alanine alphabet A). It is speculated that the earliest polypeptide chains were very short, presumably of uniform length, belonging to two alphabet types encoded in the two complementary strands of the earliest mRNA duplexes. After the fusion of the minigenes, a mosaic of the alphabets would form. Traces of the predicted mosaic structure have been, indeed, detected in the protein sequences of complete prokaryotic genomes in the form of weak oscillations with the period 12 residues in the form of alteration of two types of 6 residue long units. The next stage of protein evolution corresponded to the closure of the chains in the loops of the size 25–30 residues (Berezovsky et al., 2000). Autocorrelation analysis of proteins of 23 complete archaebacterial and eubacterial genomes revealed that the preferred distances between valine, alanine, glycine, leucine, and isoleucine along the sequences are in the same range of 25–30 residues, indicating that the loops are primarily closed by hydrophobic interactions between the ends of the loops. The loop closure stage is followed by the formation of typical folds of 100–200 amino acids, via end-to-end fusion of the genes encoding the loop-size chains. This size was apparently dictated by the optimal ring closure for DNA. In both cases the closure into the ring (loop) rendered evolutionarily advantageous stability to the respective structures. Further gene fusions lead to the formation of modern multidomain proteins. Recombinational gene splicing is likely to have appeared after the DNA circularization stage. Received: 21 December 2000 / Accepted: 28 February 2001     

burnr: Fire history analysis and graphics in R

We developed a new software package, burnr, for fire history analysis and plotting in the R statistical programming environment. It was developed for tree-ring fire-scar analysis, but is broadly applicable to other event analyses (e.g., avalanches, frost rings, or culturally modified trees). Our new package can read, write, and manipulate standard tree-ring fire history FHX files, produce fire—demography charts, calculate fire frequency and seasonality statistics, and run superposed epoch analysis (SEA). A key benefit of burnr is that it enables automation of analyses and plotting, especially for large data sets. The package also facilitates creative plotting, mapping, and analyses when combined with the thousands of packages available in R. In this paper, we describe the basic functionality of burnr and introduce users to fire history analyses in R.     

CORTICAL F‐ACTIN REORGANIZATION AND A CONTRACTILE RING‐LIKE STRUCTURE FOUND DURING THE CELL CYCLE IN THE RED CRYPTOMONAD,PYRENOMONAS HELGOLANDII1

Cortical F‐actin reorganization during the cell cycle was observed in Pyrenomonas helgolandii U. J. Santore (SAG 28.87) for the first time in Cryptophyta using fluorescein‐isothiocyanate (FITC)–phalloidin staining. In interphase, a number of F‐actin bundles were observed as straight lines running parallel to the long axis of the cell on the cell cortical region. They extended from an F‐actin bundle that runs along the margin of the vestibulum. Although the F‐actin bundles running parallel to the long axis of the cell disappeared during anaphase, they gradually reappeared in telophase. By contrast, the F‐actin bundle along the vestibulum margin remained visible during cytokinesis and dynamically changed following the enlargement of the vestibulum, suggesting that F‐actin was involved in the mechanism of vestibulum enlargement. F‐actins were not found in the cytoplasmic and nucleoplasmic regions throughout the cell cycle. In addition, a contractile ring‐like structure appeared at the cleavage furrow during cytokinesis. Treatment with cytochalasin B and latrunculin B significantly inhibited the formation of cleavage furrow, resulting in forming an abnormal cell with two nuclei, suggesting that cytokinesis in P. helgolandii is controlled by the contractile ring‐like structure constituted of F‐actin.     

Origin and evolution of the chloroplast division machinery

Chloroplasts were originally established in eukaryotes by the endosymbiosis of a cyanobacterium; they then spread through diversification of the eukaryotic hosts and subsequent engulfment of eukaryotic algae by previously nonphotosynthetic eukaryotes. The continuity of chloroplasts is maintained by division of preexisting chloroplasts. Like their ancestors, chloroplasts use a bacterial division system based on the FtsZ ring and some associated factors, all of which are now encoded in the host nuclear genome. The majority of bacterial division factors are absent from chloroplasts and several new factors have been added by the eukaryotic host. For example, the ftsZ gene has been duplicated and modified, plastid-dividing (PD) rings were most likely added by the eukaryotic host, and a member of the dynamin family of proteins evolved to regulate chloroplast division. The identification of several additional proteins involved in the division process, along with data from diverse lineages of organisms, our current knowledge of mitochondrial division, and the mining of genomic sequence data have enabled us to begin to understand the universality and evolution of the division system. The principal features of the chloroplast division system thus far identified are conserved across several lineages, including those with secondary chloroplasts, and may reflect primeval features of mitochondrial division. Shin-ya Miyagishima is the recipient of the Botanical Society Award for Young Scientists, 2004.     

Biotransformation of biphenyl by the filamentous fungus <Emphasis Type="Italic">Talaromyces helicus</Emphasis>

The filamentous fungusTalaromyces helicus , isolated from oil-contaminated sludge, oxidizes biphenyl via 4-hydroxybiphenyl to the dihydroxylated derivatives 4,4-dihydroxybiphenyl and 3,4-dihydroxybiphenyl, which, to a certain extent, are converted to glycosyl conjugates. The sugar moiety of the conjugate formed from 4,4-dihydroxybiphenyl was identified as glucose. Further metabolites: 2-hydroxybiphenyl, 2,5-dihydroxylated biphenyl, and the ring cleavage product 4-phenyl-2-pyrone-6-carboxylic acid accumulated only in traces. From these results the main pathway for biotransformation of biphenyl in T. helicus could be proposed to be the excretion of dihydroxylated derivatives (>75%) and their glucosyl conjugates (<25%).     

大麻哈鱼胚胎耳石微结构及其群体环境标记

采用人工调控环境方法对黑龙江、绥芬河大麻哈鱼发眼期胚胎群体耳石日轮进行周期性持续标记。实验分４组: 1组为对照组, 2－3组为变温标记组, 4组为“暴气”-变温标记组, 实验用发眼卵1.2万粒。待胚胎发育至耳石日轮结构形成后实施标记。实验胚胎耳石随着标记期间环境周期性变化及其持续的时间, 形成相应变化节律的日轮标记区。获得各实验组设定环境的日轮标记图谱。人工环境标记的耳石日轮图谱, 暗带色度加深, 明带亮度增大, 并可形成生长轮距不同的标记轮, 与对照组耳石微结构有明显区别, 标记率达到100%。初步建立鱼类耳石标记及其识别技术, 适用于大麻哈鱼等鲑鳟鱼类群体标记。作为安全有效、成本低廉的群体标记技术方法, 鱼类耳石日轮标记在鱼类资源评估和增殖放流效果评价中将会得到广泛应用。