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Biology subjects

Aronson, H.

Publications and source records attributed to Aronson, H..

3 recordsLinked to original sources

Evidence of thermal selection from experimental evolution in the arboviral vector Aedes albopictus

The extent to which phenotypic plasticity and adaptation are coupled during ectotherm thermal evolution is poorly understood. We carried out thermal experimental evolution for 20 generations in the arboviral vector Aedes albopictus, an efficient invasive species that has newly conquered climatically diverse regions in the past few decades. During acclimation (one generation of evolution) we saw accelerated development and increased reproduction that traded off against survival. After only another 10 generations, we saw adaptation in the form of major changes in mosquito fitness, metabolism and gene expression, revealing the consolidation of a temperature-dependent trade-off between reproduction and longevity. These shifts demonstrate that Ae. albopictuscan adapt at the pace of warming. When selection was relaxed, most of the thermally shifted phenotypes reverted to control levels, revealing the importance of plasticity after prolonged evolution. Furthermore, 250 warm evolution-altered genes did not return to control levels. These genes exhibited significant negative correlation between mean and variance in warm-evolved mosquitoes, but a two-fold variance reduction without mean change in relaxed-selection mosquitoes. Both signals are consistent with the action of selection operating on a polygenic trait architecture. Ecological modelling identified egg-to-adult viability as the primary driver of thermal reproductive success, highlighting juvenile stages as a crucial control target under continued warming.

evolutionary biology↗

Lithosyntrophy: Obligate syntrophy in a phosphite-oxidizing, methanogenic culture

The anaerobic conversion of organic matter to methane and carbon dioxide typically relies on obligate syntrophic interactions between bacteria and methanogenic archaea, where interspecies hydrogen (H2) transfer enables thermodynamically constrained reactions to proceed near equilibrium. Syntrophs couple the oxidation of fermentation products such as fatty acids and alcohols to the reduction of protons to form H2. These reactions can only proceed if low H2 concentrations are maintained by H2-consuming syntrophic partners. Here, we describe "lithosyntrophy," a novel mode of syntrophic interaction in which electrons that drive hydrogenotrophic methanogenesis originate from an inorganic compound rather than from the canonical organic substrates. Candidatus Phosphitivorax anaerolimi strain Phox-21 oxidizes phosphite (HPO32-, oxidation state +3) to phosphate coupled to hydrogenogenesis in an obligate energetic dependency on a hydrogenotrophic methanogen, Methanoculleus sp. Physiology experiments, thermodynamic calculations, genomic annotation, and metaproteomics analysis collectively revealed a mechanism for syntrophic phosphite oxidation in Phox-21, which requires phosphite, acetate, and CO2 as co-substrates. In this pathway, electrons derived from phosphite drive H2 production via an electron-confurcating hydrogenase. Unlike previously characterized acetogenic phosphite oxidizers that grow without exogenous acetate, Phox-21 requires acetate to regenerate AMP, a cofactor required by the phosphite dehydrogenase, PtdF. Lithosyntrophic phosphite oxidizers may play important roles both in transferring reducing equivalents as well as biologically available phosphorus to other members of their surrounding microbial communities. We infer that lithosyntrophic DPO emerged before acetoclastic methanogenesis and was a major sink for acetate in the Archaean when phosphite was more abundant. Significance statementDissimilatory phosphite-oxidizing microorganisms (DPOM) use phosphite as an energy source, producing phosphate. While the two previously isolated DPOM couple phosphite oxidation to carbon fixation via the Wood-Ljungdahl pathway, Candidatus Phosphitivorax anaerolimi strain Phox-21 instead performs lithosyntrophic metabolism, coupling DPO to proton reduction in obligate partnership with a hydrogenotrophic methanogen. This establishes a novel link between phosphorus and carbon redox cycles: like organosyntrophy, DPO can fuel methanogenesis. Lithosyntrophy expands our understanding of syntrophic interactions and suggests similar processes may occur with other inorganic substrates in anoxic ecosystems. We propose lithosyntrophic DPO predates acetoclastic methanogenesis, serving as an early acetate sink during the Archaean. Following Earths oxygenation, phosphite depletion likely reduced competition for acetate, enabling the later evolution of acetoclastic methanogenesis.

microbiology↗

Thiovibrio frasassiensis gen. nov., sp. nov., an autotrophic, elemental sulfur disproportionating bacterium isolated from sulfidic karst sediment, and proposal of Thiovibrionaceae fam. nov.

A novel, autotrophic, mesophilic bacterium, strain RS19-109T, was isolated from sulfidic stream sediments in the Frasassi Caves, Italy. The cells of this strain grew chemolithoautotrophically under anaerobic conditions while disproportionating elemental sulfur (S0) and thiosulfate, but not sulfite with bicarbonate/CO2 as a carbon source. Autotrophic growth was also observed with molecular hydrogen as an electron donor, and S0, sulfate, thiosulfate, nitrate, and ferric iron as electron acceptors. Oxygen was not used as an electron acceptor and sulfide was not used as an electron donor. Weak growth was observed with sulfate as an electron acceptor and organic carbon as electron donors and carbon sources. The strain also showed weak growth by fermentation of tryptone. Strain RS19-109T was found to be phylogenetically distinct based on 16S rRNA gene sequence similarity (89.2%) to its closest relative, Desulfurivibrio alkaliphilus AHT2T. The draft genome sequence for strain RS19-109T had average nucleotide identity, average amino acid identity, and in silico DNA-DNA hybridization values of 72.2%, 63.0%, and 18.3%, respectively, compared with the genome sequence of D. alkaliphilus AHT2T. On the basis of its physiological and genomic properties, strain RS19-109T is proposed as the type strain of a novel species of a novel genus, Thiovibrio frasassiensis gen. nov., sp. nov. A novel family, Thiovibrionaceae fam. nov., is proposed to accommodate Thiovibrio within the order Desulfobulbales.

microbiology↗