RESUMO
Two thermophilic, strictly chemolithoautotrophic, microaerophilic, hydrogen-oxidizing members of the Bacteria designated strain EX-H1T and strain EX-H2T were isolated from two separate deep-sea hydrothermal vent sites at 9 degrees N 104 degrees W in the Pacific Ocean and Guaymas Basin. The motile 2-4-microm-long rods were Gram-negative and non-sporulating. The temperature range for growth was between 55 and 80 degrees C for EX- H1T (optimum at 73 degrees C) and 55-75 C for EX-H2T (optimum at 70 C). Both strains grew fastest at 2.5% (w/v) NaCl and at pH 6, although growth was observed from pH 4.7 to pH 7.5. EX-H1T and EX-H2T were able to use elemental sulfur, thiosulfate or hydrogen as an electron donor, and oxygen (2-3%, v/v) or nitrate as an electron acceptor. EX-H1T was also able to use elemental sulfur as an electron acceptor. EX-H1T and EX-H2T further differed in their genomic G+C content (38.5 and 37.4 mol%, respectively) and 16S rRNA sequences (4% difference). Maximum-likelihood analysis of the 16S rRNA phylogeny placed both isolates within the Aquificales as a distinct lineage and showed them to be only about 85% similar to Aquifex pyrophilus. On the basis of phenotypic and phylogenetic characteristics, it is proposed that EX-H1T and EX-H2T belong to a new genus within the Aquificales, namely Persephonella gen. nov. It is further proposed that EX-H1T be named Persephonella marina sp. nov., the type species of the genus, and that EX-H2T be named Persephonella guaymasensis sp. nov., a second species in this genus.
Assuntos
Bactérias Gram-Negativas/classificação , Temperatura Alta , Hidrogênio/metabolismo , Água do Mar/microbiologia , Composição de Bases , DNA Ribossômico/análise , Bactérias Gram-Negativas/genética , Bactérias Gram-Negativas/crescimento & desenvolvimento , Bactérias Gram-Negativas/isolamento & purificação , México , Dados de Sequência Molecular , Oxirredução , Oceano Pacífico , Fenótipo , Filogenia , RNA Ribossômico 16S , Análise de Sequência de DNARESUMO
Hydrothermal petroleums and heavy tars have been analyzed for polycyclic aromatic hydrocarbons (PAH) with molecular weights greater than that of coronene (300 da). Samples from the hydrothermal systems in the Guaymas Basin (Gulf of California) and in the Escanaba Trough and Middle Valley (Northeastern Pacific) were analyzed by gas chromatography-mass spectrometry and high pressure liquid chromatography with diode-array absorbance detection. Mass spectra and fluorescence spectra were used to characterize the compounds. Several large PAHs with six and more rings were identified among the heavy PAH. Production routes via one-ring build-up and Scholl-condensation are proposed to explain the observed structures. The variations in PAH concentrations and distributions between samples from different locales are a consequence of the hydrothermal conditions of generation, migration, and post-depositional alteration.
Assuntos
Sedimentos Geológicos/química , Temperatura Alta , Petróleo/análise , Hidrocarbonetos Policíclicos Aromáticos/química , Água do Mar/química , Cromatografia Gasosa-Espectrometria de Massas , Sedimentos Geológicos/análise , México , Estrutura Molecular , Peso Molecular , Oceano Pacífico , Hidrocarbonetos Policíclicos Aromáticos/análise , Alcatrões/análise , Alcatrões/químicaRESUMO
The aliphatic, aromatic and polar (NSO) fractions of seabed petroleums and sediment bitumen extracts from the Guaymas Basin hydrothermal system have been analyzed by gas chromatography and gas chromatography-mass spectrometry (free and silylated). The oils were collected from the interiors and exteriors of high temperature hydrothermal vents and represent hydrothermal pyrolyzates that have migrated to the seafloor by hydrothermal fluid circulation. The downcore sediments are representative of both thermally unaltered and thermally altered sediments. The survey has revealed the presence of oxygenated compounds in samples with a high degree of thermal maturity. Phenols are one class of oxygenated compounds found in these samples. A group of methyl-, dimethyl- and trimethyl-isoprenoidyl phenols (C27-C29) is present in all of the seabed NSO fractions, with the methyl- and dimethyl-isoprenoidyl phenols occurring as major components, and a trimethyl-isoprenoidyl phenol as a minor component. A homologous series of n-alkylphenols (C13-C33) has also been found in the seabed petroleums. These phenols are most likely derived from the hydrothermal alteration of sedimentary organic matter. The n-alkylphenols are probably synthesized under hydrothermal conditions, but the isoprenoidyl phenols are probably hydrothermal alteration products of natural product precursors. The suites of phenols do not appear to be useful tracers of high temperature hydrothermal processes.