Ferromagnetic resonance and low-temperature magnetic tests for biogenic magnetite

By B. Weiss, S. Kim, J. Kirschvink, Robert E Kopp, M. Sankaran, A. Kobayashi, A. Komeili. 2004

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Detection of noninteracting single domain particles using first‐order reversal curve diagrams (2010, methodology): “This property has been exploited by coercivity analysis [Egli, 2003, 2004a] and ferromagnetic resonance (FMR) spectroscopy [Weiss et al., 2004; Kopp et al., 2006].”
Searching for single domain magnetite in the “pseudo‐single‐domain” sedimentary haystack: Implications of biogenic magnetite preservation for sediment magnetism and relative paleointensity determinations (2012, background): “…and the fact that they are shifted to lower fields compared to non-biogenic magnetite makes them distinctive of intact magnetite magnetosome chains [Weiss et al., 2004;Kopp et al., 2006; Fischer et al., 2008; Charilaou et al., 2011; Kind et al., 2011; Gehring et al., 2011; Chang et al., 2012].”
Magnetite as a prokaryotic biomarker: A review (2010, methodology): “…type of magnetic determination is through ferromagnetic resonance spectroscopy (FMR) which can be used to measure the effective magnetic field within a sample and includes contributions from both magnetic anisotropy and magnetostatic interactions [Weiss et al., 2004a, 2004b; Kopp et al., 2006].”