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The observation of large magnetite (Fe3O4) crystals from magnetotactic bacteria by electron and atomic force microscopy

 

作者: MARCOS FARINA,   BECHARA KACHAR,   ULYSSES LINS,   RAYMOND BRODERICK,   HENRIQUE LINS BARROS,  

 

期刊: Journal of Microscopy  (WILEY Available online 1994)
卷期: Volume 173, issue 1  

页码: 1-8

 

ISSN:0022-2720

 

年代: 1994

 

DOI:10.1111/j.1365-2818.1994.tb03423.x

 

出版商: Blackwell Publishing Ltd

 

关键词: Magnetotactic bacteria;atomic force microscopy;electron microscopy;crystalline habits;magnetic single domains;biomineralization

 

数据来源: WILEY

 

摘要:

SUMMARYMagnetite crystals inside coccoid magnetotactic bacteria found in lagoons near Rio de Janeiro city were examined by electron microscopy (EM) and atomic force microscopy (AFM). For AFM, ultrathin sections of bacteria embedded in Epon resin were etched with an ethanolic NaOH solution and observed both in the height and in the force modes. Comparative electron microscope images were useful for identifying crystalline reliefs in the etched sections. Different situations representing particular arrangements of crystal chains were observed by AFM. The majority of the bacteria examined presented unusually large magnetite crystals which remained strongly attached in linear chains even after the laboratory procedures for their isolation. This behaviour is different from all other biogenic magnetite crystals isolated so far. It is suggested that this attachment is due to the strong field between individual crystals as well as to the contact areas, which are the largest observed until now. The correct identification of a particular topography by AFM as a crystal relief may be critical when crystals are not aligned in chains; in these cases the linear dimensions and the presence of well‐defined edges and faces are important features to be taken into account. Characterization of the crystal faces is important for the study of magnetotactic micro‐organisms since the crystalline habits seem to be species‐specific. Observation of etched sections proved to be a helpful approach for crystal relief observation, especially when small amounts of bacteria were avai

 

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