Abstract
A series of controlled abiotic syntheses of magnetite nanocrystals were carried out to explore the possibility of using morphological criteria, crystal size distributions, and shape ratio as tools for identifying nanocrystals that would be specifically produced by magnetotactic bacteria. High-quality magnetite crystals synthesized with various controlled total iron concentrations were shown to have cubo-octahedral shapes and sizes varying from 4 to 24 nm. The mean particle size of the population was found to be 10.5 ± 0.7 nm and no significant effect of the total iron concentration on the particle size was observed. Systematical analyses of size and morphology also allowed for the determination of crystal size and shape ratio distributions. Crystal sizes were observed to follow log-normal distributions. Shape factors are bounded by one, with maxima between 0.80 to 1.00. Their distributions are asymmetric, with a cut off toward the high values. Crystal morphologies and shape factors appear not to be a powerful diagnostic tool for the differentiation of abiotic vs. biotic particles. However, crystal size distributions of abiotic crystals are significantly different from those of biotic populations. Indeed, opposite asymmetry of the size distributions from biogenic and non biogenic crystals was observed, with cut off toward larger sizes for biogenic nanocrystals and with cut off toward smaller sizes for abiogenic nanocrystals. This therefore constitutes a potential diagnostic tool for deciphering magnetite origin.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
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- Structure of framboidal pyrite: An electron backscatter diffraction study
- The mineralogical microstructure of shells: PART 2.1 The iridescence colors of abalone shells
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- Experimental study on diamond dissolution in kimberlitic and lamproitic melts at 1300-1420 °C and 1 GPa with controlled oxygen partial pressure
- Validation of LA-ICP-MS fluid inclusion analysis with synthetic fluid inclusions
- Etch pit coalescence, surface area, and overall mineral dissolution rates
- Crystal chemistry of the elbaite-schorl series
- Morphology of nanomagnetite crystals: Implications for formation conditions
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- Kinetics of Fe2+-Mg order-disorder in P21/c pigeonite
- First-principles studies on the elastic constants of a 1:1 layered kaolinite mineral
- Quantum mechanical calculations of trans-vacant and cis-vacant polymorphism in dioctahedral 2:1 phyllosilicates
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- Letter. Direct observations of pseudomorphism: compositional and textural evolution at a fluid- solid interface
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- Comment on Melluso et al. (2003) Reported data and interpretation of some wollastonite- and melilite-bearing rocks from the Central Apennines of Italy
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- Reply to Capitanio 2005. Mineralogic and bulk rock composition of Italian wollastonite- and melilite-bearing paralava and clinker: Further evidence of their pyrometamorphic nature