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软 X 射线能谱断层摄影术研究蓝藻生物矿化的成核作用。

Soft X-ray spectro-tomography study of cyanobacterial biomineral nucleation.

机构信息

Center for Applied Geoscience, Tuebingen University, Tuebingen, Germany.

出版信息

Geobiology. 2009 Dec;7(5):577-91. doi: 10.1111/j.1472-4669.2009.00221.x. Epub 2009 Oct 26.

DOI:10.1111/j.1472-4669.2009.00221.x
PMID:19863594
Abstract

Quantitative three-dimensional (3D) chemical mapping using angle-scan spectro-tomography in a scanning transmission (soft) X-ray microscope (STXM) has been used for the first time to characterize the early stages of CaCO(3) biomineral nucleation on the surface of planktonic freshwater cyanobacterial cells of the strain Synechococcus leopoliensis PCC 7942. The apparatus for STXM angle-scan tomography is described. Aspects of sample preparation, sample mounting and data acquisition and quantitative analysis and interpretation are discussed in detail. Angle-scan tomography and chemically selective 3D imaging at multiple photon energies has been combined with a complete 2D spectromicroscopic characterization of the biochemical and mineralogical composition. This has provided detailed insights into the mechanisms of mineral nucleation, leading to development of a detailed model of CaCO(3) nucleation by the cyanobacterial strain S. leopoliensis PCC 7942. It shows that Ca is absorbed by the extracellular polymeric substances (EPS) of the cyanobacteria and that CaCO(3) with aragonite-like short-range order is precipitated rather homogeneously within the EPS. The precipitation of the thermodynamically more stable calcite polymorph then starts at Ca-rich hot spots within the EPS and close to the cyanobacteria.

摘要

首次使用扫描透射(软)X 射线显微镜(STXM)中的角度扫描光谱层析术对淡水浮游蓝藻细胞Synechococcus leopoliensis PCC 7942 表面上碳酸钙(CaCO3)生物矿化成核的早期阶段进行了定量三维(3D)化学绘图。描述了用于 STXM 角度扫描层析的设备。详细讨论了样品制备、样品安装、数据采集和定量分析以及解释的各个方面。角度扫描层析和多光子能量下的化学选择性 3D 成像与生化和矿物成分的完整 2D 光谱微成像相结合,深入了解了成核机制,从而提出了蓝藻菌株 S. leopoliensis PCC 7942 中 CaCO3 成核的详细模型。它表明 Ca 被蓝藻的细胞外聚合物(EPS)吸收,并且具有文石样短程有序的 CaCO3 相当均匀地沉淀在 EPS 内。然后,在 EPS 内的富 Ca 热点处和靠近蓝藻处开始沉淀热力学上更稳定的方解石多晶型物。

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