Biology subjects

Duprat, E.

Publications and source records attributed to Duprat, E..

4 recordsLinked to original sources

bioRxiv2025

Intracellular amorphous calcium carbonate biomineralization in methanotrophic gammaproteobacteria was acquired by horizontal gene transfer from cyanobacteria

Some bacteria genetically control the biomineralization of intracellular amorphous calcium carbonates (iACC) with potential implications for microbial physiology, evolution, bioremediation and biogeochemical cycling. Until now, this capacity has been documented in Cyanobacteria, the giant gammaproteobacterium Achromatium and a few magnetotactic Pseudomonadota and Nitrospirota. Here, we report the discovery of iACC biomineralization in members of the Methylococcaceae, a family of aerobic methanotrophic Gammaproteobacteria. A homolog of the ccyA gene, previously considered a diagnostic marker for iACC formation in Cyanobacteria, was identified in several Methylococcaceae genomes, based on a search of the conserved C-terminal (GlyZip)3 domain of the encoded calcyanin protein, with a sequence coverage higher than 60% and an E-value lower than 1e-20. Moreover, two cultivated strains, Methylococcus geothermalis and Methylococcus mesophilus, whose genomes contained the ccyA gene, were consistently shown to form iACC granules. The ccyA genes of Methylococcaceae and Microcystis share higher sequence similarity (47%) than with other Cyanobacteria (around 30%) within their common (GlyZip)3 domain, suggesting horizontal gene transfer (HGT) from an ancestral Microcystis-like cyanobacterium to Methylococcaceae. This finding extends the known taxonomic distribution of ccyA and suggests that the capability to biomineralize iACC was acquired by HGT, possibly in environments such as those close to the oxyclines of lakes, where Cyanobacteria and Methylococcaceae commonly co-exist. The discovery of iACC in methane-oxidizing Methylococcaceae highlights a previously unrecognized coupling between calcium carbonate biomineralization and methane cycling in aquatic environments, suggesting that iACC formation may play an overlooked role in microbial carbon storage and local geochemical regulation.

microbiology↗

bioRxiv2024

Diel changes in the expression of a marker gene and candidate genes for intracellular amorphous CaCO3 biomineralization in Microcystis

Phylogenetically diverse cyanobacteria biomineralize intracellular amorphous calcium carbonate (iACC) inclusions. This includes several genotypes of the Microcystis genus, a potentially toxic, bloom-forming cyanobacterium found worldwide in freshwater ecosystems. While we ignore the biological function of iACC and the molecular mechanisms driving their formation, this process may impact local geochemical cycles and/or be used for bioremediation strategies. Recently, a marker gene of this biomineralization pathway, named ccyA, was discovered. However, the function of the calcyanin protein encoded by ccyA remains unknown. Here, based on an RNA- Seq approach, we assess the expression of the ccyA gene in Microcystis aeruginosa PCC 7806 during a 24 h day/night cycle. The ccyA gene shows a clear day/night expression pattern with maximum transcript abundances during the second half of the night. This is consistent with the assumption that iACC biomineralization is related with photosynthesis and may therefore follow a day/night cycle as well. Moreover, several genes directly co-localized upstream and downstream of ccyA, on the same DNA strand show a similar expression pattern, including a cax gene encoding a calcium/proton exchanger and a gene encoding a protein with a domain also present in the N-terminal region of calcyanins in many iACC-forming cyanobacteria. This suggests that they all could be part of an operon, and may play a concerted role in iACC formation. Last, several other genes involved in carbon concentrating mechanisms and calcium transport show an expression pattern similar to that of ccyA. Overall, this study provides a list of candidate genes that may be involved in the biomineralization of iACC by cyanobacteria and whose role could be, in the future, analyzed by biochemistry and genetics approaches.

microbiology↗

bioRxiv2021

A new gene family diagnostic for intracellular biomineralization of amorphous Ca-carbonates by cyanobacteria

Cyanobacteria have massively contributed to carbonate deposit formation over the geological history. They are traditionally thought to biomineralize CaCO3 extracellularly as an indirect byproduct of photosynthesis. However, the recent discovery of freshwater cyanobacteria forming intracellular amorphous calcium carbonates (iACC) challenges this view. Despite the geochemical interest of such a biomineralization process, its molecular mechanisms and evolutionary history remain elusive. Here, using comparative genomics, we identify a new gene (ccyA) and protein (calcyanin) family specifically associated with cyanobacterial iACC biomineralization. Calcyanin is composed of a conserved C-terminal domain, which likely adopts an original fold, and a variable N-terminal domain whose structure allows differentiating 4 major types among the 35 known calcyanin homologues. Calcyanin lacks detectable full-length homologs with known function. Yet, genetic and comparative genomic analyses suggest a possible involvement in Ca homeostasis, making this gene family a particularly interesting target for future functional studies. Whatever its function, this new gene family appears as a gene diagnostic of intracellular calcification in cyanobacteria. By searching for ccyA in publicly available genomes, we identified 13 additional cyanobacterial strains forming iACC. This significantly extends our knowledge about the phylogenetic and environmental distribution of cyanobacterial iACC biomineralization, especially with the detection of multicellular genera as well as a marine species. Phylogenetic analyses indicate that iACC biomineralization is ancient, with independent losses in various lineages and some HGT cases that resulted in the broad but patchy distribution of calcyanin across modern cyanobacteria. Overall, iACC biomineralization emerges as a new case of genetically controlled biomineralization in bacteria. Significance statementFew freshwater species of Cyanobacteria have been known to mineralize amorphous CaCO3 (ACC) intracellularly. Despite the geochemical interest of this biomineralization, its evolutionary history and molecular mechanism remain poorly known. Here, we report the discovery of a new gene family that has no homolog with known function, which proves to be a good diagnostic marker of this process. It allowed to find cyanobacteria in several phyla and environments such as seawater, where ACC biomineralization had not been reported before. Moreover, this gene is ancient and was independently lost in various lineages with some later horizontal transfers, resulting in a broad and patchy phylogenetic distribution in modern cyanobacteria.

evolutionary biology↗

bioRxiv2018

Novel Mechanism for Surface Layer Shedding and Regenerating in Bacteria Exposed to Metal-Contaminated Conditions

Surface layers (S-layers) are self-assembling, ordered structures composed of repeating protein subunits found as components of the cell walls throughout the Bacteria and the Archaea. S-layers act as an interface between prokaryotic cells and their surrounding environment, and provide protection for microorganisms against diverse environmental stresses including heavy metal stress. We have previously characterized the process by which S-layers serve as a nucleation site for metal mineralization in the presence of high concentration of metals. Here, we test the hypothesis originally proposed in cyanobacteria that a \"shedding\" mechanism exists in prokaryotes for replacing S-layers that have become mineral-encrusted. We used a metallotolerant gram-positive bacterium bearing an S-layer, Lysinibacillus sp. TchIII 20n38, as a model organism. We characterize for the first time a mechanism for resistance to metals through S-layer shedding and regeneration. S-layers nucleate the formation of Fe-mineral on the cell surface, leading to the encrustation of the S-layer. Using a combination of scanning electron microscopy (SEM) and nanoSIMS, we show that mineral-encrusted S-layers are shed by the bacterial cells, and the emerging cells regenerate new S-layers as part of their cell wall structure. This novel mechanism for the survival of prokaryotes in metal-contaminated environments may also provide elements necessary for the development of renewable systems for metal bioremediation.

microbiology↗