Biology subjects

Gillett, D. L.

Publications and source records attributed to Gillett, D. L..

4 recordsLinked to original sources

bioRxiv2024

Quinone extraction drives atmospheric carbon monoxide oxidation in bacteria

Diverse bacteria and archaea use atmospheric carbon monoxide (CO) as an energy source during long-term survival. This process enhances the biodiversity of soil and marine ecosystems globally and removes 250 million tonnes of a toxic, climate-relevant pollutant from the atmosphere each year. Bacteria use [MoCu]-carbon monoxide dehydrogenases (Mo-CODH) to convert CO to carbon dioxide, then transfer the liberated high-energy electrons to the aerobic respiratory chain. However, given no high-affinity Mo-CODH has been purified, it is unknown how these enzymes oxidise CO at low concentrations and interact with the respiratory chain. Here we resolve these knowledge gaps by analysing Mo-CODH (CoxSML) and its hypothetical partner CoxG from Mycobacterium smegmatis. Kinetic and electrochemical analyses show purified Mo-CODH is a highly active high-affinity enzyme (Km = 139 nM, kcat = 54.2 s-1). Based on its 1.85 [A] resolution cryoEM structure, Mo-CODH forms a CoxSML homodimer similar to characterised low-affinity homologs, but has distinct active site coordination and narrower gas channels that may modulate affinity. We provide structural, biochemical, and genetic evidence that Mo-CODH transfers CO-derived electrons to the aerobic respiratory chain via the membrane-bound menaquinone-binding protein CoxG. Consistently, CoxG is required for CO-driven respiration, extracts menaquinone from mycobacterial membranes, and binds quinones in a hydrophobic pocket. Finally, we show that Mo-CODH and CoxG genetically and structurally associate in diverse bacteria and archaea. These findings reveal the basis of a biogeochemically and ecologically important process, while demonstrating that the newly discovered process of long-range quinone transport is a general mechanism of energy conservation, which convergently evolved on multiple occasions.

biochemistry↗

bioRxiv2023

An obligate aerobe adapts to hypoxia by hybridising fermentation with carbon storage

In soil ecosystems, obligately aerobic bacteria survive oxygen deprivation (hypoxia) by entering non-replicative persistent states. Little is known about how these bacteria rewire their metabolism to stay viable in these states. The model obligate aerobe Mycobacterium smegmatis maintains redox homeostasis during hypoxia by mediating fermentative hydrogen production. However, the fate of organic carbon during fermentation, and the associated remodeling of carbon metabolism, is unresolved. Here we systematically profiled the metabolism of M. smegmatis during aerobic growth, hypoxic persistence, and the transition between these states. Using differential isotope labelling, and paired metabolomics and proteomics, we observed rerouting of central carbon metabolism through the pentose phosphate pathway and Entner-Doudoroff pathway during hypoxia. We show that M. smegmatis excretes high levels of hydrogen concurrently with upregulating triacylglyceride synthases and accumulating glycerides as carbon stores. Using electron cryotomography (cryo-ET), we observed the presence of large spheroid structures consistent with the appearance of lipid droplets. Thus, in contrast to obligately and facultative anaerobic fermentative bacteria, M. smegmatis stores rather than excretes organic carbon during hypoxia. This novel hybrid metabolism likely provides a competitive advantage in resource-variable environments by allowing M. smegmatis to simultaneously dispose excess reductant during hypoxia and maintain carbon stores to rapidly resume growth upon reoxygenation.

microbiology↗

bioRxiv2021

A nitrite-oxidizing bacterium constitutively consumes atmospheric hydrogen

Chemolithoautotrophic nitrite-oxidizing bacteria (NOB) of the genus Nitrospira contribute to nitrification in diverse natural environments and engineered systems. Nitrospira are thought to be well-adapted to substrate limitation owing to their high affinity for nitrite and capacity to use alternative energy sources. Here, we demonstrate that the canonical nitrite oxidizer Nitrospira moscoviensis oxidizes hydrogen (H2) below atmospheric levels using a high-affinity group 2a nickel-iron hydrogenase [Km(app) = 32 nM]. Atmospheric H2 oxidation occurred under both nitrite-replete and nitrite-deplete conditions, suggesting low-potential electrons derived from H2 oxidation promote nitrite-dependent growth and enable survival during nitrite limitation. Proteomic analyses confirmed the hydrogenase was abundant under both conditions and indicated extensive metabolic changes occur to reduce energy expenditure and growth under nitrite-deplete conditions. Respirometry analysis indicates the hydrogenase and nitrite oxidoreductase are bona fide components of the aerobic respiratory chain of N. moscoviensis, though they transfer electrons to distinct electron carriers in accord with the contrasting redox potentials of their substrates. Collectively, this study suggests atmospheric H2 oxidation enhances the growth and survival of NOB in amid variability of nitrite supply. These findings also extend the phenomenon of atmospheric H2 oxidation to a seventh phylum (Nitrospirota) and reveal unexpected new links between the global hydrogen and nitrogen cycles.

microbiology↗

bioRxiv2020

Cellular and structural basis of synthesis of the unique intermediate dehydro-F420-0 in mycobacteria

F420 is a low-potential redox cofactor used by diverse bacteria and archaea. In mycobacteria, this cofactor has multiple roles, including adaptation to redox stress, cell wall biosynthesis, and activation of the clinical antitubercular prodrugs pretomanid and delamanid. A recent biochemical study proposed a revised biosynthesis pathway for F420 in mycobacteria; it was suggested that phosphoenolpyruvate served as a metabolic precursor for this pathway, rather than 2-phospholactate as long proposed, but these findings were subsequently challenged. In this work, we combined metabolomic, genetic, and structural analyses to resolve these discrepancies and determine the basis of F420 biosynthesis in mycobacterial cells. We show that, in whole cells of Mycobacterium smegmatis, phosphoenolpyruvate rather than 2-phospholactate stimulates F420 biosynthesis. Analysis of F420 biosynthesis intermediates present in M. smegmatis cells harboring genetic deletions at each step of the biosynthetic pathway confirmed that phosphoenolpyruvate is then used to produce the novel precursor compound dehydro-F420-0. To determine the structural basis of dehydro-F420-0 production, we solved high-resolution crystal structures of the enzyme responsible (FbiA) in apo, substrate, and product bound forms. These data show the essential role of a single divalent cation in coordinating the catalytic pre-complex of this enzyme and demonstrate that dehydro-F420-0 synthesis occurs through a direct substrate transfer mechanism. Together, these findings resolve the biosynthetic pathway of F420 in mycobacteria and have significant implications for understanding the emergence of antitubercular prodrug resistance.

biochemistry↗