Abstract / Description of output
Focused ion beam (FIB) sample preparation in combination with subsequent transmission electron microscopy (TEM) analysis are powerful tools for nanometre-scale examination of the cell-mineral interface in bio-geological samples. In this study, we used FIB-TEM to investigate the interaction between a cyanobacterium (Hassallia byssoidea) and a common sheet silicate mineral (biotite) following a laboratory-based bioweathering, incubation experiment. We discuss the FIB preparation of cross-sections of the cell mineral interface for TEM investigation. We also establish an electron fluence threshold (at 200 key) in biotite for the transition from scanning (S)TEM electron beam induced contamination build up on the surface of biotite thin sections to mass loss, or hole-drilling within the sections. Working below this threshold fluence nanometre-scale structural and elemental information has been obtained from biotite directly underneath cyanobacterial cells incubated on the biotite for 3 months. No physical alteration of the biotite was detected by TEM imaging and diffraction with little or no elemental alteration detected by STEM-energy dispersive X-ray (EDX) elemental line-scanning or by energy filtered TEM (EF-TEM) jump ratio elemental mapping. As such we present evidence that the cyanobacterial strain of H. byssoidea did not cause any measurable alteration of biotite, within the resolution limits of the analysis techniques used, after 3 months of incubation on its surface. (C) 2013 Elsevier Ltd. All rights reserved.
Original language | English |
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Pages (from-to) | 10-17 |
Number of pages | 8 |
Journal | Micron |
Volume | 47 |
DOIs | |
Publication status | Published - Apr 2013 |
Keywords / Materials (for Non-textual outputs)
- FIB
- TEM
- Cyanobacteria
- Weathering
- Cell-mineral interface
- Biotite
- FOCUSED ION-BEAM
- TRANSMISSION ELECTRON-MICROSCOPE
- SAMPLE PREPARATION
- PLANETARY MATERIALS
- DISSOLUTION
- BIOTITE
- ROCKS
- PHYLLOSILICATES
- MICROSTRUCTURE
- TRANSFORMATION