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Microbial Kinetic Controls on Calcite Morphology in Supersaturated Solutions

机译:过饱和溶液中方解石形态的微生物动力学控制

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摘要

Recognizing microbial imprints in the morphology of calcium carbonate minerals that form in very supersaturated solutions containing a high level of dissolved inorganic carbon (DIC) is challenging. To better define criteria for this purpose, we have analyzed the influence of sulfate-reducing bacterium Desulfovibrio desulfuricans strain G20 on the morphology of calcite in such solutions. G20 does not induce large shifts of pH or alkalinity under these conditions, but its uptake of millimolar sulfate and lactate decreases the number of anhedral crystals and stimulates growth of subhedral spar crystals relative to the abiotic controls. In addition, organic compounds associated with the basal growth medium, purified exopolymeric substances produced by G20 and lypopolysaccharide, stimulate the growth of anhedral crystals and crystals with rounded edges at low supersaturation index (SI) of calcite. The effect of organic compounds is reduced at higher SI, where rhombohedral habits dominate. Our results suggest that the local production and uptake of kinetic inhibitors within microbial biofilms may be an important control on calcite morphology in supersaturated solutions.
机译:识别在含有高水平溶解无机碳(DIC) 的非常过饱和溶液中形成的碳酸钙矿物质形态上的微生物印记具有挑战性。为了更好地为此目的定义标准,我们分析了硫酸盐还原菌 Desulfovibrio desulfuricans G20菌株对方解石中 形态的影响。解决方案。在这些条件下,G20不会引起pH或碱度的大变化,但对毫摩尔硫酸盐和乳酸盐的吸收会减少无面体 晶体和相对于非生物对照刺激 的亚面晶石生长。此外,与基础生长培养基相关的有机化合物,由G20和脂多糖产生的纯化的外聚合物质,刺激无规晶体和晶体的生长。sup> 方解石的 低过饱和指数(SI)具有圆形边缘。有机 化合物的作用在较高SI时降低,其中菱形体习惯 占主导地位。我们的结果表明,微生物生物膜内局部抑制剂的产生和动力学抑制剂的摄取可能是 控制过饱和 溶液中方解石形态的重要控制因素。 >

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  • 来源
    《Journal of Sedimentary Research》 |2005年第2期|00000190-00000199|共10页
  • 作者

    Tanja Bosak; Dianne K. Newman;

  • 作者单位

    Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, U.S.A.;

    Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, U.S.A.dkn@gps.caltech.edu;

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