scholarly journals Microbial sulfide oxidation in the oxic–anoxic transition zone of freshwater sediment: involvement of lithoautotrophic Magnetospirillum strain J10

2009 ◽  
Vol 70 (1) ◽  
pp. 54-65 ◽  
Author(s):  
Jeanine S. Geelhoed ◽  
Dimitry Y. Sorokin ◽  
Eric Epping ◽  
Tatjana P. Tourova ◽  
Horia L. Banciu ◽  
...  
Author(s):  
Zhangzhang Xie ◽  
Surong Li ◽  
Weitie Lin ◽  
Jianfei Luo

A novel sulfur-oxidizing bacterium, designated strain LSR1T, was enriched and isolated from a freshwater sediment sample collected from the Pearl River in Guangzhou, PR China. The strain was an obligate chemolithoautotroph, using thiosulfate or sulfide as an electron donor and energy source. Growth of strain LSR1T was observed at 15–40 °C, pH 6.0–7.5 and NaCl concentrations of 0–1.5 %. Strain LSR1T was microaerophilic, with growth only at oxygen content less than 10 %. Anaerobic growth was also observed when using nitrate as the sole electron acceptor. The major cellular fatty acids were C16 : 0 and summed feature 3 (comprising C16 : 1 ω7c and/or C16 : 1 ω6c). The DNA G+C content of the draft genome sequence was 67.5 mol%. Phylogenetic analysis based on 16S rRNA gene sequences indicated that strain LSR1T formed a lineage within the family Thiobacillaceae , showing sequence identities of 92.87, 92.33 and 90.80 % with its closest relative genera Sulfuritortus , Annwoodia and Thiobacillus , respectively. The genome of strain LSR1T contained multiple genes encoding sulfur-oxidizing enzymes that catalyse thiosulfate and sulfide oxidation, and the gene encoding cbb 3-type cytochrome c oxidase and bd-type quinol oxidase, which enables strain LSR1T to perform sulphur oxidation under microaerophilic conditions. On the basis of phenotypic, genotypic and phylogenetic results, strain LSR1T is considered to represent a novel species of a new genus Parasulfuritortus within the family Thiobacillaceae , for which the name Parasulfuritortus cantonensis gen. nov., sp. nov. is proposed. The type strain is LSR1T (=GDMCC 1.1549=JCM 33645).


Author(s):  
B. B. Shkursky

Theoretical modeling of regular olivine grains misorientations in mimetic paramorphoses after ringwoodite and wadsleyite, the formation of which during the ascension of matter from the Mantle Transition Zone is expected, has been carried out. The coordinates of the misorientation axes and the misorientation angles, characterizing 10 operations of alignment in the pair intergrowths of olivine grains, eight of which are twins, are calculated. Possible conditions for the formation of mimetic paramorphoses predicted here, and the chances of their persistence are discussed. The calculated orientations are compared with the known twinning laws of olivine.


2010 ◽  
Vol 38 (4) ◽  
pp. 286-307
Author(s):  
Carey F. Childers

Abstract Tires are fabricated using single ply fiber reinforced composite materials, which consist of a set of aligned stiff fibers of steel material embedded in a softer matrix of rubber material. The main goal is to develop a mathematical model to determine the local stress and strain fields for this isotropic fiber and matrix separated by a linearly graded transition zone. This model will then yield expressions for the internal stress and strain fields surrounding a single fiber. The fields will be obtained when radial, axial, and shear loads are applied. The composite is then homogenized to determine its effective mechanical properties—elastic moduli, Poisson ratios, and shear moduli. The model allows for analysis of how composites interact in order to design composites which gain full advantage of their properties.


2017 ◽  
Vol 120 (3) ◽  
pp. 421-432 ◽  
Author(s):  
C. Browning ◽  
M. Reid

AbstractThe Lower Carboniferous, probably Tournaisian, Kweekvlei Formation is part of the Witteberg Group (Cape Supergroup) of South Africa. Together with the overlying Floriskraal Formation, it forms an upward-coarsening succession within the Lake Mentz Subgroup. Sedimentary features of the Kweekvlei Formation suggest deposition in a storm-wave dominated marine setting, within the storm-influenced, distal part of an offshore transition zone environment. This predominantly argillaceous formation preserves a low diversity trace fossil assemblage. Reworked vascular plant debris (including the problematic genus Praeramunculus sp.) and a shark spine have been reported for the Kweekvlei Formation. There are no known stratigraphic equivalents in South Africa.


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