Abstract
MamA is a highly conserved protein found in magnetotactic bacteria (MTB), a diverse group of prokaryotes capable of navigating according to magnetic fields – an ability known as magnetotaxis. Questions surround the acquisition of this magnetic navigation ability; namely, whether it arose through horizontal or vertical gene transfer. Though its exact function is unknown, MamA surrounds the magnetosome, the magnetic organelle embedding a biomineralised nanoparticle and responsible for magnetotaxis. Several structures for MamA from a variety of species have been determined and show a high degree of structural similarity. By determining the structure of MamA from Desulfovibrio magneticus RS-1 using X-ray crystallography, we have opened up the structure-sequence landscape. As such, this allows us to perform structural- and phylogenetic-based analyses using a variety of previously determined MamA from a diverse range of MTB species across various phylogenetic groups. We found that MamA has remained remarkably constant throughout evolution with minimal change between different taxa despite sequence variations. These findings, coupled with the generation of phylogenetic trees using both amino acid sequences and 16S rRNA, indicate that magnetotaxis likely did not spread via horizontal gene transfer and instead has a significantly earlier, primordial origin.
Highlights
Magnetotactic bacteria (MTB) are a diverse group of prokaryotes capable of movement according to magnetic fields–an ability known as magnetotaxis
Size-exclusion chromatography revealed that MamAΔ41RS-1 elutes at a volume that corresponds to an octamer, whilst MamAΔ41 proteins from different species were found as either trimers or monomers (S1 Fig)
The size-exclusion chromatography elution profile of ARSTM displayed some differences in reference to MamAΔ41RS-1, as the mutated protein eluted at three distinct volumes
Summary
Magnetotactic bacteria (MTB) are a diverse group of prokaryotes capable of movement according to magnetic fields–an ability known as magnetotaxis. This characteristic is believed to have developed to enable these aerobic or anaerobic, aquatic, Gram negative bacteria to optimally find the oxic-anoxic boundary [1]. This is achieved via the internal biomineralisation of magnetic nanoparticles of either magnetite (Fe3O4) or greigite (Fe3S4) by a specific organelle, the PLOS ONE | DOI:10.1371/journal.pone.0130394. Desulfovibrio magneticus RS-1, which shares 98.7% similarity of its 16S rRNA gene sequence with Desulfovibrio burkinensis, is a magnetite-containing microorganism related to dissimilatory sulphate-reducing bacteria [10]
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