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首页> 外文期刊>American Mineralogist >Crystal-size and shape distributions of magnetite from uncultured magnetotactic bacteria as a potential biomarker
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Crystal-size and shape distributions of magnetite from uncultured magnetotactic bacteria as a potential biomarker

机译:未经培养的趋磁细菌中磁铁矿的晶体大小和形状分布作为潜在的生物标记

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摘要

We studied the sizes and shapes of magnetite nanocrystals produced by several types of uncultured magnetotactic bacteria to understand whether their size distributions can be used for identifying the biogenic origin of magnetite crystals in geological samples. The two-dimensional projections of the crystals were measured on transmission electron microscope (TEM) images, and features of crystal-size and shape-factor distributions (CSD and SFD, respectively) were analyzed. In agreement with previous results, most magnetite CSD curves are asymmetric and negatively skewed; however, one magnetotactic strain produced particles that have a normal size distribution. A statistical analysis of CSDs and SFDs (both from this and previous studies) reveals similarities among magnetite from magnetotactic strains from various locations. In particular, crystals in a cultured marine strain (MC-2) were indistinguishable from magnetite from a freshwater strain. We tested whether CSDs of distinct magnetosome types can be recovered from the shape and size data of all particles combined in samples that contain several types of magnetosomes; such samples can be used as models for rocks that contain magnetite nanocrystals of unknown and, presumably, various origins. If the SFDs of the distinct magnetosome types occurring in the same sample differ, the CSDs of individual magnetosome types can be retrieved from bulk data. In such cases the characteristic shape of the size distribution can be used for identifying magnetite as originating from magnetotactic bacteria.
机译:我们研究了几种未培养的趋磁细菌产生的磁铁矿纳米晶体的尺寸和形状,以了解 是否其尺寸分布可用于识别 地质样品中磁铁矿晶体的成因。 在透射电子显微镜(TEM)图像上测量晶体的二维投影 ,并具有 分析了晶体大小和形状因子分布(分别为CSD和SFD, )。与以前的结果一致, 大多数磁铁矿CSD曲线是不对称的并且是负偏斜的; 但是,一种趋磁应变产生的颗粒具有 正常尺寸分布。对CSDs和 SFDs(来自本研究和先前研究)的统计分析显示, 在磁铁矿中来自不同位置的趋磁应变。 养殖的海洋菌株(MC-2)中的晶体 与淡水菌株中的磁铁矿没有区别。我们 测试了是否可以从包含几种类型的磁小体的样品 中合并的所有颗粒的形状和大小数据中恢复不同磁小体类型的CSD ;这样的样本可以 用作包含磁铁矿纳米晶体的模型,这些磁铁矿的来源未知且可能是各种来源。如果 的SFD在同一样本中出现的不同磁小体类型 不同,则可以从批量数据中检索 单个磁小体类型的CSD。在这种情况下, 大小分布的特征形状可用于识别磁铁矿是 sup> 来自趋磁细菌。

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  • 来源
    《American Mineralogist》 |2005年第9期|00001233-00001240|共8页
  • 作者单位

    Department of Earth and Environmental Sciences, University of Veszprém, Veszprém, Hungary;

    Department of Earth and Environmental Sciences, University of Veszprém, Veszprém, Hungary;

    Max Planck Institute for Marine Microbiology, Bremen, Germany;

    Max Planck Institute for Marine Microbiology, Bremen, Germany;

    Department of Physics, California Polytechnic State University, San Luis Obispo, California 93407, U.S.A.;

    Departments of Geological Sciences and Chemistry/Biochemistry, Arizona State University, Tempe, Arizona 85287, U.S.A.;

    Department of Earth and Environmental Sciences, University of Veszprém, Veszprém, Hungary;

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