Recommended Citation
Preprint version. Journal of Geophysical Research, Volume 103, Issue B12, January 1, 1998, pages 30601-30604.
The definitive version is available at https://doi.org/10.1029/97JB03512.
Abstract
Magnetotactic bacteria construct an internal, permanent magnetic dipole based on single magnetic domain particles of magnetite or greigite. The organisms exert a high degree of control over the size and morphology of the particles. This may be relevant in distinguishing biogenic from nonbiogenic iron mineral particles.
Disciplines
Physics
Copyright
Publisher statement
An edited version of this paper was published by AGU. Further reproduction or electronic distribution is not permitted.
URL: https://digitalcommons.calpoly.edu/phy_fac/295