| 不同状态嗜盐古菌细胞及羧基微球诱导白云石沉淀 |
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| 引用本文： | 药彦辰,邱轩,王红梅,段勇.不同状态嗜盐古菌细胞及羧基微球诱导白云石沉淀[J].地球科学,2018,43(2):449-458. |
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| 作者姓名： | 药彦辰 邱轩 王红梅 段勇 |
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| 作者单位： | 1.中国地质大学生物地质与环境地质国家重点实验室, 湖北武汉 430074 |
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| 基金项目： | 国家自然科学基金项目41130207国家自然科学基金项目41502317中国地质大学（武汉）生物地质与环境地质国家重点实验室开放基金GBL21503 |
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| 摘 要： | 白云石是沉积岩中广泛存在的碳酸盐矿物，其成因机制一直备受关注.野外调研发现现生白云石多分布于高盐环境，模拟实验也表明嗜盐微生物能诱导形成白云石，但微生物诱导白云石沉淀的机理仍不明确.分别用嗜盐古菌Natrinema sp.J7-1对数后期的活细胞、失去代谢活性的J7-1完整细胞（经线粒体氧化磷酸化解偶联剂处理）、表面蛋白质变性的J7-1细胞（经多聚甲醛和戊二醛处理）和表面富含羧基的微球，在盐度为280‰的沉淀体系中诱导白云石沉淀.分别利用X射线衍射（XRD）分析矿物的物相，扫描电子显微镜（SEM）分析矿物、微生物以及羧基微球的形貌，傅立叶红外光谱（FT-IR）分析细胞变性前后表面的官能团.结果表明，失去代谢活性的J7-1细胞与正常的对数后期细胞均能够诱导原白云石形成；经过多聚甲醛/戊二醛固定后，细胞表面羧基含量降低，不能诱导白云石沉淀；羧基微球能够诱导形成原白云石.以上研究证实细胞表面的羧基可能是微生物促进白云石沉淀的一种关键因素，而细胞的生长代谢在本研究的条件下不是控制白云石沉淀的主要因素.
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| 关 键 词： | 白云石 嗜盐古菌 羧基 微生物 矿物学 |
| 收稿时间： | 2017-10-02 |
Dolomite Formation Mediated by Halophilic Archaeal Cells under Different Conditions and Carboxylated Microspheres |
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| Abstract: | Dolomite is a widespread carbonate mineral in sedimentary rocks, and its formation mechanism have always attracted much attention. Most modern dolomite occurred in hypersaline environments and several microbial isolates from these environments have been reported to be able to induce dolomite formation as well. However the detailed mechanism of microbial induced dolomite remains largely unclear to date. In this study, a halophilic archaea, Natrinema sp. J7-1, was used to investigate what exactly played an important role in the microbial dolomite formation. Normal cells of Natrinema sp. J7-1 in post-log phase, inactive cells treated with carbonyl cyanide 3-cholorophenylhydrazine (CCCP, amitochondrial inhibitor), denatured cells treated by paraformaldehyde and glutaraldehyde, as well as carboxylated microspheres were used to induce dolomite formation. The mineral phases were identified by X-ray Diffraction(XRD), the morphologies of minerals, cells and microspheres were observed by Scanning Electron Microscope(SEM) and the functional groups on the surface of normal cells and denatured cells were analyzed by Fourier Transform Infrared Spectroscopy(FT-IR). Results showed that normal cells, inactive cells and carboxylated microspheres induced proto-dolomite formation successfully at the salinity of 280‰. In contrast, denatured cells were not capable of inducing the formation of dolomite, and the percentage of carboxyl groups on their surface decreased compared with normal cells. It can be concluded that carboxyl is one critical factor for microbially mediated dolomite formation, but respiration may count for little under our conditions. |
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