Biochemical characterization of two glutamate dehydrogenases with different cofactor specificities from a hyperthermophilic archaeon Pyrobaculum calidifontis

Two putative glutamate dehydrogenase (GDH) genes (pcal_1031 and pcal_1606) were found in a sulfur-dependent hyperthermophilic archaeon, Pyrobaculum calidifontis. The two genes were then expressed in Escherichia coli, and both of the recombinant gene products showed GDH activity. The two enzymes were then purified to homogeneity and characterized in detail. Although both purified GDHs had a hexameric structure and neither exhibited allosteric regulation, they showed different coenzyme specificities: one was specific for NAD⁺, the other for NADP⁺ and different heat activation mechanisms. In addition, there was little difference in the kinetic constants, optimal temperature, thermal stability, optimal pH and pH stability between the two enzymes. The overall sequence identity between the two proteins was very high (81 %), but was not high in the region recognizing the 2′ position of the adenine ribose moiety, which is responsible for coenzyme specificity. This is the first report on the identification of two GDHs with different coenzyme specificities from a single hyperthermophilic archaeon and the definition of their basic in vitro properties.     

Novel Small Stable RNAs of Mycoplasma capricolum

Two stable RNA species and their genes have been isolated fromMycoplasma capricolum, and the nucleotide sequences have beendetermined by partial RNA sequencing and sequencing of the genes.The RNAs are 92 and 105 nucleotides in length, respectively.The two RNAs reveal no sequence similarity to any stable RNAso far reported, indicating that these are novel RNA species.The RNAs, designated MCS2 and MCS3 RNA, exist in small amountsin the soluble fraction of the cell extract.     

A simple in situ method for estimating fungal population size in the rumen

Sediment and the overlying water samples were collected from 67 fresh and 38 salt water sites in the UK. Only 13% (five) of the samples taken from salt water sites were negative for magnetotactic bacteria compared with 47·7% (32) of the fresh water ones. Of the seven types of salt water habitats examined, saltmarsh ponds were found to be most suited to magnetotactic bacteria, 96% (25/26) of sites being positive.     

Isolation and characterization of hemorrhagic factors a and b from the venom of the Chinese habu snake (Trimeresurus mucrosquamatus)

Hemorrhagic factors a and b were isolated from Trimeresurus mucrosquamatus venom by Sephadex G-100, CM-Sephadex C-50 and DEAE-Sephacel column chromatographies. The hemorrhagic factors were homogeneous, as established by a single band on acrylamide gel electrophoresis, isoelectric focusing and sodium dodecyl sulfate (SDS)-polyacrylamide gel electrophoresis. Molecular weights of 15 000 and 27 000 were found for hemorrhagic factors a and b, respectively. Factor a possesses proteolytic activity hydrolyzing the His(10)-Leu(11), Tyr(16)-Leu(17) and Arg(22)-Gly(23) bonds of oxidized insulin B chain, whereas, factor b hydrolyzed only the Ala(14)-Leu(15) bond. Hemorrhagic activity of these hemorrhagic factors was inhibited by ethylenediaminetetraacetic acid, 1,10-phenanthroline or p-chloromercuribenzoate, but not by soybean trypsin inhibitor or diisopropyl fluorophosphate. The hemorrhagic factors were injected into the skin of the back of albino rabbits, and the minimum hemorrhagic dose of factors a and b was 1.7 and 2.3 μg, respectively. These purified hemorrhagic factors were not lethal at 15 μg/g in mice. Factor a hydrolyzed the Bβ chain of fibrinogen, while factor b hydrolyzed the Aα chain. Hemorrhagic factor a was shown to differ immunologically from factor b. Factors a and b produced systemic hemorrhage in internal organs such as the heart and stomach of mice. Moreover, factor b produced hemorrhage in the liver.     

Natural infections of Pintomyia verrucarum and Pintomyia maranonensis by Leishmania (Viannia) peruviana in the Eastern Andes of northern Peru

The natural infection of sand flies by Leishmania was investigated in Andean areas located between the Central and Eastern Cordilleras of northern Peru where cutaneous leishmaniasis caused by Leishmania (Viannia) peruviana is endemic. Sand flies were captured at five locations along the Utcubamba River in the Department of Amazonas, and morphologically identified under a microscope. Among 422 female sand flies dissected, the most dominant species was Pintomyia verrucarum (320 flies), followed by Pi. maranonensis (83 flies), Pi. robusta (13 flies), and Lutzomyia castanea (6 flies). Genetic analysis of sand flies from these areas together with those from other areas revealed that individuals of Pi. verrucarum were closely related regardless of morphological variation of their spermathecae. On the other hand, individuals of Pi. maranonensis collected in the study area were distant from those of other areas with genetic distances over the intraspecific level but mostly below the interspecific level, suggesting the unique characteristics of sand flies in this area. The natural infection of sand flies by flagellate parasites was detected mainly in the hindgut of each one of Pi. verrucarum and Pi. maranonensis. Both parasite species were identified as L. (V.) peruviana based on cytochrome b and mannose phosphate isomerase gene analyses. In addition, parasite species obtained from the lesion of a patient with cutaneous leishmaniasis in the study area in this period was identified as L. (V.) peruviana. These results strongly suggest that Pi. verrucarum and Pi. maranonensis are responsible for the transmission of L. (V.) peruviana in these areas. This is the first report of the natural infection of Pi. maranonensis by L. (V.) peruviana.     

Ion exchange reactions on the stem surface of Chamaecyparis obtusa Sieb. et Zucc.

In order to clarify the sources of soil acidification below stands of hinoki (Chamecyparis obtusa Sieb. et Zucc.), artificial stemflow experiments were performed to separate out the role rainfall acidity has from that of the acidity potentially occurring during stemflow. Various solutions, including distilled water, NaCl, NH₄Cl, KCl and CaCl₂+MgCl₂ solutions, were added in a controlled manner to the upper stem and the solutions systematically collected at breast height. Although the original pH values of the salt solutions were around 5.5, the pH values of stemflow ranged from 3.8 to 4.2. The ion balance [anion (including bicarbonate ions) to cation concentration] decreased with initial stemflow but recovered after ca. 5 l of flow. At this point, pH values continued to decrease and this decrease was accompanied by a decrease in the cation concentration of the stemflow. These results indicate that there are two ways by which stemflow can be acidified. In the initial stage of flow, organic and inorganic acids are dissolved in the stemflow. Following this, ion exchange occurs between cations contained in the stemflow and hydrogen ions adsorbed in the stem. The last step appears most critical in the acidification process.