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首页> 外文期刊>Geomicrobiology Journal >Environmental Factors Affect Magnetite Magnetosome Synthesis in Magnetospirillum magneticum AMB-1: Implications for Biologically Controlled Mineralization
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Environmental Factors Affect Magnetite Magnetosome Synthesis in Magnetospirillum magneticum AMB-1: Implications for Biologically Controlled Mineralization

机译:环境因素影响Magnetospirillum magneticum AMB-1中磁铁矿磁铁小体的合成:对生物控制矿化的影响。

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It is widely believed that magnetotactic bacteria (MTB) form membrane-enveloped magnetite crystals (magnetosomes) under strict genetic control. In this study, the Magnetospirillum magneticum strain AMB-1 was cultured in the same growth medium, but under four different growth conditions: Anaerobic static, aerobic static, aerobic 80-rpm rotating, and aerobic 120-rpm rotating to investigate possible environmental influences on magnetite magnetosome formation. Integrated analyses, using transmission electron microscopy, X-ray diffraction and rock magnetism, indicate that, from the anaerobic static to aerobic 120-rpm rotating culture, the formed magnetite magnetosomes became more equidimensional, smaller in grain size, and higher in crystal twinning frequency. Magnetic properties of magnetite magnetosomes such as coercivity, remanence coercivity, remanence ratio and Verwey transition temperature systematically decreased from 22.0 mT to 5.2 mT, 31.3 mT to 9.3 mT, 0.45 to 0.31, and 108 K to 98 K, respectively. Comparison of additional anaerobic 120-rpm rotating cultures with anaerobic static cultures showed that the effect of rotating, at least up to 120 rpm, on the cell growth and magnetite magnetosome formation is weak and negligible. Given that all samples were prepared and measured in the same way, the changes in physical and magnetic properties indicate that environmental factors (oxygen) affected the biomineralization of magnetite magnetosomes in magnetotactic bacteria, which supports the previous findings. In all experiments, only magnetite with the geometry of truncated octahedron was formed within magnetosomes, which suggests that the mineral phase and crystal habit remain to be genetically controlled. These results also imply the physical and magnetic properties of magnetite magnetosomes may, to some extent, reflect the external growth environments.View full textDownload full textKeywordsmagnetotactic bacteria, M. magneticum AMB-1, environmental factor, biologically controlled mineralization, rock magnetismRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/01490451.2011.565401
机译:人们普遍认为,趋磁细菌(MTB)在严格的遗传控制下会形成膜包裹的磁铁矿晶体(磁小体)。在这项研究中,在同一生长培养基上培养了磁螺菌AMB-1菌株,但是在四种不同的生长条件下:厌氧静态,有氧静态,有氧80 rpm旋转和有氧120 rpm旋转以研究可能的环境影响。磁铁矿磁小体的形成。使用透射电子显微镜,X射线衍射和岩石磁学进行的综合分析表明,从厌氧静态到有氧120 rpm旋转培养,形成的磁铁矿磁小体变得更均等,晶粒尺寸更小,晶体孪生频率更高。磁铁矿小体的磁性,如矫顽力,剩磁矫顽力,剩磁比和Verwey转变温度,分别从22.0 mT降至5.2 mT,31.3 mT降至9.3 mT,0.45到0.31以及108 K到98K。将其他厌氧120-rpm旋转培养物与厌氧静态培养物进行比较表明,至少以120 rpm旋转,对细胞生长和磁铁矿磁小体形成的影响微弱且可忽略不计。假定所有样品均以相同的方式制备和测量,则物理和磁性能的变化表明环境因素(氧气)影响了趋磁细菌中磁铁矿磁小体的生物矿化作用,这支持了先前的发现。在所有实验中,在磁小体中仅形成了具有截顶八面体几何形状的磁铁矿,这表明矿物相和晶体习性尚待遗传控制。这些结果也暗示着磁铁矿磁小体的物理和磁性可能在一定程度上反映了外部生长环境。查看全文下载全文关键词趋磁细菌,M. magneticum AMB-1,环境因素,生物控制矿化,岩石磁性相关的var addthis_config = {ui_cobrand:“ Taylor&Francis Online”,servicescompact:“ citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,更多”,发布:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/01490451.2011.565401

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