Pende, N. | Search bioRxiv

bioRxiv2021

An ancient divide in outer membrane tethering systems in Bacteria

Recent data support the hypothesis that Gram-positive bacteria (monoderms) arose from Gram-negatives (diderms) through loss of the outer membrane (OM). However how this happened remains unknown. Considering that tethering of the OM is essential for cell envelope stability in diderm bacteria we hypothesize that its destabilization may have been involved in OM loss. Here, we present an in-depth analysis of the four main OM tethering systems across all Bacteria. We show that their distribution strikingly follows the bacterial phylogeny with a bimodal distribution matching the deepest phylogenetic cleavage between Terrabacteria (a clade encompassing Cyanobacteria, Deinococcus/Thermus, Firmicutes, etc.) and Gracilicutes (a clade encompassing Proteobacteria, Bacteroidetes, Spirochaetes, etc.). Diderm Terrabacteria display as the main system OmpM, a porin that attaches non-covalently to modified peptidoglycan or to secondary cell wall polymers. In contrast, the lipoprotein Pal is restricted to the Gracilicutes along with a more sporadic occurrence of OmpA. While Brauns lipoprotein Lpp is largely considered as the textbook example of OM attachment, it is actually present only in a subclade of Gammaproteobacteria. We propose an evolutionary scenario whereby the last common bacterial ancestor used a system based on OmpM, which was later replaced by one based on the lipoprotein Pal concomitantly to the emergence of the Lol machinery to address lipoproteins to the OM, with OmpA as a possible transition state. We speculate that the existence of only one main OM tethering system in the Terrabacteria would have allowed the multiple emergences of the monoderm phenotype specifically observed in this clade through OmpM perturbation. We test this hypothesis by inactivating all four ompM gene copies in the genetically tractable diderm Firmicute Veillonella parvula. The resulting mutant is severely affected in growth and displays high sensitivity to OM stress. High resolution imaging and tomogram reconstructions reveal a dramatic - yet non-lethal - phenotype, in which vast portions of the OM detach, producing large vesicles surrounding multiple monoderm-like cells sharing a common periplasm. Complementation by a single OmpM rescues the phenotype to a normal cell envelope. Together, our results highlight an ancient shift in bacterial evolution involving OM tethering systems. They suggest a possible mechanism for OM loss and a high flexibility of the cell envelope in diderm Firmicutes, making them ideal models to further refine our understanding of the mechanisms involved in bacterial OM stability, and opening the way to recapitulate the monoderm/diderm transition in the laboratory.

microbiology↗

bioRxiv2020

SepF is the FtsZ-anchor in Archaea: implications for cell division in the Last Universal Common Ancestor

The Archaea present profound differences compared to Bacteria in fundamental molecular and cellular processes. While most Archaea divide by binary fission using an FtsZ-based system similar to Bacteria, they lack the majority of the components forming the complex bacterial divisome. Moreover, how FtsZ precisely functions and interacts with other proteins to assemble the archaeal division machinery remains largely unknown. Notably, among the multiple bacterial factors that tether FtsZ to the membrane during cell constriction, Archaea only possess SepF-like homologues, but their function has not been demonstrated. Here, we combine structural, cellular, and evolutionary approaches to demonstrate that SepF is the FtsZ anchor in the human-associated archaeon Methanobrevibacter smithii. 3D super-resolution microscopy of immunolabeled cells shows that M. smithii SepF co-localizes with FtsZ at the division plane. We also show that M. smithii SepF binds both to membranes and FtsZ, inducing filament bundling. High-resolution crystal structures of archaeal SepF alone and in complex with FtsZCTD reveal that SepF forms a dimer with a specific homodimerization interface. This drives a strikingly different binding mode from what is observed in Bacteria. Finally, analysis of the distribution and phylogeny of SepF and FtsZ indicates that these proteins date back to the Last Universal Common Ancestor (LUCA) and that Archaea may have retained features of an ancestral minimal cell division system, while Bacteria likely diverged to accommodate the emergence of the complex machinery required to coordinate cytokinesis with the rigid peptidoglycan cell wall and the appearance of additional FtsZ tethers. Our results contribute key insights into the largely understudied mechanisms of archaeal cell division, and pave the way for a better understanding of the processes underlying the divide between the two prokaryotic domains.

microbiology↗