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where −1 indicates the inversion operation of a matrix.
This sudden change in viscosity indicates the inversion point from oil-in-water emulsion to water-in-oil emulsion which coincides with 70.5% oil content at 30 °C and 245 s−1 using 3 wt% Triton X-100.
** one gene inversion indicates the inversion event of one gene.
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Table 3 illustrates that only the CDC 684 isolate possessed the inverted genotype from among 17 genomes examined, indicating the inversion is not common in B. anthracis.
A viscosity reduction of around 100% was obtained up to a critical oil content between 66 and 70%, which indicates the phase inversion of the emulsions from O/W to W/O emulsions.
A map summarizing genetic changes among K1207, S0108 and FAM18 genomes is shown in Figure 3, where the blue chiasma indicates the same inversion present in S0108 with respect to FAM18.
The arrow indicates the location of the inversion in Sp. A few landmark loci are shown.
The fact that there is not a long stretch of SNPs along the ∼3.8 Mb region that is flanked by the SDs that involve this polymorphic inversion, and only a region of about 170 kb on both sides showing homozygosity for the SNPs, indicates that the inversion has likely been generated many generations ago, leading to many recombination events within the region.
Molecular characterization of the breakpoints indicates that the inversion is a result of intra-chromosomal homologous recombination, originating almost exclusively in male germ cells.
The retention of the rRNA genes on the minor strand in other available evaniomoph mt genomes indicates that the inversion occurred after the divergence of the Megalyroidea.
The genetic variation pattern within the region indicates that the inversion first appeared before dispersal out of Africa, and that there has been little or no recombination between the haplotypes.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com