Search bioRxiv⌕ Search

Biology subjects

Gutierrez-Preciado, A.

Publications and source records attributed to Gutierrez-Preciado, A..

8 recordsLinked to original sources

Redox distribution of Asgard archaea and co-occurring taxa in microbial mats from an early Proterozoic ecosystem analog

Increasing evidence supports that eukaryotes originated from the symbiosis of an Asgard archaeon, the alphaproteobacterial ancestor of mitochondria, and possibly additional bacterial contributions. Eukaryogenesis likely occurred in redox-transition environments such as microbial mats or shallow sediments [~]2 billion years ago, when atmospheric oxygen was far lower than today, and oceans were euxinic. We investigated Asgardarchaeota-enriched microbial mats from the low-oxygen, sulfidic Catherine volcano lake (Afar region, Ethiopia), mimicking early Proterozoic conditions. 16S rRNA gene metabarcoding, metagenomics, and metagenome-assembled genome (MAG) analyses across redox-stratified layers of in situ and mesocosm-maintained mats revealed that Asgardarchaeota thrived in the sulfate-reduction zone, mainly co-occurring with Desulfurobacterota and Myxococcota, among others. Lokiarchaeia and Thorarchaeia were more abundant in deeper, anoxic layers. Within Heimdallarchaeia, Heimdallarchaeales were enriched in upper layers, correlating with oxygen-tolerant hydrogenase and sulfate-reduction genes, whereas Hodarchaeales were more relatively abundant in anoxic layers, correlating with methanogenesis. Although reactive-oxygen-species defense mechanisms were widespread in Asgardarchaeota MAGs, they lacked genes for aerobic respiration. These results support the hypothesis that Asgard archaea engaged primarily in syntrophic interactions with sulfate-reducers under conditions prevailing on the early Earth at the onset of eukaryogenesis.

microbiology↗

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↗

Nested parasitism in hypersaline environments: viruses and virus satellites of haloarchaea and their nanosized cellular symbionts

It is increasingly recognized that hyperparasitism, whereby a parasite exploits a host which itself is a parasite, is a common phenomenon across ecosystems and domains of life. Here, to explore hyperparasitism in Archaea, we focused on ultra-small archaea of the phylum Nanohaloarchaeota, a distinct lineage within the DPANN superphylum, which establish obligate symbiotic interactions with extreme halophiles of the class Halobacteria. We assembled five metagenomes originating from geothermally influenced salt lakes in the Danakil Depression, Ethiopia, and reconstructed the viromes associated with both haloarchaea and nanohaloarchaea. Both archaeal lineages were associated with viruses from four distinct groups, including head-tailed viruses (class Caudoviricetes), tailless icosahedral viruses, pleomorphic viruses and spindle-shaped viruses, which represent 12 previously undescribed families. The haloarchaeal viruses (HVs) and nanohaloarchaeal viruses (NHVs) are only distantly related, suggesting that viruses from the four groups co-evolved with their respective hosts for an extended period, likely since the divergence of the two archaeal lineages from their last common ancestor. Consistently, our results show that HVs and NHVs are well-adapted to replicate in their respective hosts and to thrive in hypersaline environments. No evidence of host switching between haloarchaea and nanohaloarchaea was obtained, but multiple horizontal transfers of genes implicated in virion structure and morphogenesis between HVs and NHVs were detected. We also identified several NHVs-encoded auxiliary metabolic genes implicated in nucleotide and amino acid metabolisms, which could enhance the metabolic capabilities of the nanohaloarchaeal hosts that have highly reduced genomes. Finally, in addition to HVs and NHVs, we describe plasmid-derived virus satellites that appear to have originated convergently to parasitize spindle-shaped viruses of both haloarchaea and nanohaloarchaea, uncovering an additional layer of parasitism. Collectively, our findings fill the knowledge gap on the diversity of HVs and NHVs, highlight the complexity of virus-host and virus-virus interactions in hypersaline environments, and open doors for further mining of the virosphere of the globally distributed DPANN archaea.

microbiology↗

Extremely acidic proteomes and metabolic flexibility in bacteria and highly diversified archaea thriving in geothermal chaotropic brines

Few described archaeal, and fewer bacterial, lineages thrive at salt-saturating conditions, such as solar saltern crystallizers (salinity above 30%-w/v). They accumulate molar K+ cytoplasmic concentrations to maintain osmotic balance ( salt-in strategy), and have proteins adaptively enriched in negatively charged, acidic amino acids. Here, we analyzed metagenomes and metagenome-assembled genomes (MAGs) from geothermally influenced hypersaline ecosystems with increasing chaotropicity in the Danakil Depression. Normalized abundances of universal single-copy genes confirmed that haloarchaea and Nanohaloarchaeota encompass 99% of microbial communities in the near life-limiting conditions of the Western-Canyon Lakes (WCLs). Danakil metagenome- and MAG-inferred proteomes, compared to those of freshwater, seawater and solar saltern ponds up to saturation (6-14-32% salinity), showed that WCL archaea encode the most acidic proteomes ever observed (median protein isoelectric points [≤]4.4). We identified previously undescribed Halobacteria families as well as an Aenigmatarchaeota family and a bacterial phylum independently adapted to extreme halophily. Despite phylum-level diversity decreasing with increasing salinity-chaotropicity, and unlike in solar salterns, adapted archaea exceedingly diversified in Danakil ecosystems, challenging the notion of decreasing diversity under extreme conditions. Metabolic flexibility to utilize multiple energy and carbon resources generated by local hydrothermalism along feast-and-famine strategies seemingly shape microbial diversity in these ecosystems near life limits.

microbiology↗

Culture- and genome-based characterization of a tripartite interaction between patescibacterial epibionts, methylotrophic proteobacteria, and a jumbo phage in freshwater ecosystems

Patescibacteria form a very diverse and widely distributed phylum of small bacteria inferred to have an episymbiotic lifestyle. However, the prevalence of this lifestyle within the phylum and their host specificity remain poorly known due to the scarcity of cultured representatives. Here, we describe a complex system consisting of a patescibacterium, its gammaproteobacterial hosts, and their respective phages based on enrichment cultures and metagenomic data from two shallow, geographically close, freshwater ecosystems. The patescibacterium, Strigamonas methylophilicida sp. nov., defines a new genus within the family Absconditicoccaceae. It grows as epibiont on cells of methanotrophic species of the gammaproteobacterial family Methylophilaceae. Strigamonas cells grow tightly attached to the host, sometimes forming stacks that connect two host cells. Despite a surprisingly large genome (1.9 Mb) compared to many other Patescibacteria, S. methylophilicida lacks many essential biosynthetic pathways, including the complete biosynthesis of phospholipids, amino acids, and nucleic acids, implying a dependence on the host to obtain these molecules. We also identified and assembled the complete genomes of one patescibacterial phage that might represent a new virus family within the class Caudoviricetes, and two Methylophilaceae phages predicted to have head-tailed and filamentous virions, respectively. The patesciphage uses a modified genetic code similar to that of its host and encodes four tRNA genes, including the suppressor tRNA gene for the UGA stop codon, which is reassigned to glycine in many Patescibacteria. Our results confirm a prevalent episymbiotic lifestyle in Absconditicoccaceae and further suggest a clade-specific adaptation of this patescibacterial family for gammaproteobacterial hosts. IMPORTANCEPatescibacteria are ultra-small bacteria with reduced genomes that rely on symbiotic interactions with other prokaryotes, yet their host specificity and associated viral parasites remain poorly characterized due to limited cultured representatives. Here, we describe Strigamonas methylophilicida, a new patescibacterial species of the family Absconditicoccaceae that grows as an epibiont on various methylotrophic Gammaproteobacteria. This expands the host range for this family beyond previously documented photosynthetic partners. Using enrichment cultures and metagenomics, we retrieved complete genomes of novel phages infecting S. methylophilicida and its hosts, including one phage that uses a modified genetic code matching that of the patescibacterium. These findings reveal a previously unrecognized patescibacteria- methylotroph-phage tripartite interaction in freshwater environments, highlight the adaptations of patescibacterial phages, and shed light on the complex ecology and evolution of host-parasite-phage dynamics in understudied bacterial lineages.

microbiology↗

Several independent adaptations of archaea to hypersaline environments

Several archaeal lineages thrive in high, saturating salt concentrations. These extremely halophilic archaea, including Halobacteria, Nanohaloarchaeota, Methanonatronarchaeia, and Haloplasmatales, must maintain osmotic equilibrium with their environment. For this, they use a salt-in strategy, which involves pumping molar concentrations of potassium into the cells, which, in turn, has led to extensive proteome-wide modifications to prevent protein aggregation. However, the evolutionary history underlying these adaptations remains poorly understood. In particular, the number of times that these dramatic proteome-sweeping changes occurred is unclear due to the conflicting phylogenetic positions found for several of these lineages. Here, we present a resolved phylogeny of extremely halophilic archaea obtained using improved taxon sampling and state-of-the-art phylogenetic approaches designed to cope with the strong compositional biases of their proteomes. We describe two new uncultured lineages, Afararchaeaceae and Asboarchaeaceae, which break the long branches at the base of Haloarchaea and Nanohaloarchaeota, respectively. Our extensive phylogenomic analyses show that at least four independent adaptations to extreme halophily occurred during archaeal evolution. Finally, gene-tree/species-tree reconciliation suggests that gene duplication and horizontal gene transfer played an important role in this process, for example, by spreading key genes (such as those encoding potassium transporters) across the various extremely halophilic lineages.

evolutionary biology↗

Description of Gloeomargarita ahousahtiae sp. nov., a thermophilic member of the order Gloeomargaritales with intracellular carbonate inclusions

A unicellular cyanobacterium, strain VI4D9, was isolated from thermophilic microbial mats thriving in a hot spring of the Ahousaht territory of Vancouver Island, Canada. The cells were elongated rods (5.1 m in length and 1.2 m in width on average). Their UV-visible absorption spectra revealed that they contain chlorophyll a, phycocyanin, and carotenoids. Transmission electron microscopy showed the presence of thylakoids concentrated on one side of the cells. The strain grew within a temperature range of 37-50{degrees}C, with an optimum at 45{degrees}C. Its genome had a size of 3,049,282 bp and a DNA G+C content of 51.8 mol%. The cells contained numerous intracellular spherical granules easily visible under scanning electron microscopy. Energy-dispersive x-ray spectroscopy revealed that these granules were made of Ca-, Ba- and Sr-containing carbonates. A phylogenetic 16S rRNA gene tree robustly placed this strain as sister to several environmental sequences and the described species Gloeomargarita lithophora, also characterized by the possession of intracellular carbonate inclusions. We consider strain VI4D9 to represent a new Gloeomargarita species based on its marked phenotypic differences with G. lithophora, notably, its thermophilic nature and different thylakoid organization. We propose the name Gloeomargarita ahousahtiae sp. nov. for this newly isolated thermophilic cyanobacterium. The type strain is VI4D9 (Culture Collection of Algae and Protozoa strain 1472/1; Laboratorio de Algas Continentales Mexico strain LAC 140). G. ahousahtiae is the second species described within the recently discovered order Gloeomargaritales.

microbiology↗

Viral and parasitic cell ratios per free-living microbe across ecosystems

It is generally assumed that viruses outnumber cells on Earth by at least tenfold. Virus-to-microbe ratios (VMR) are largely based on counts of fluorescently labelled virus-like particles. However, these exclude intracellular viruses and potentially include false positives (DNA-containing vesicles, gene-transfer agents, unspecifically stained inert particles). Here, we develop a metagenome-based VMR estimate (mVRM) that accounts for DNA viruses across all stages of their replication cycles (virion, intracellular lytic and lysogenic) by using normalised RPKM (reads per kilobase of gene sequence per million of mapped metagenome reads) counts of the major capsid protein (MCP) genes and cellular universal single-copy genes (USCGs) as proxies for virus and cell counts, respectively. After benchmarking this strategy using mock metagenomes with increasing VMR, we inferred mVMR across different biomes. To properly estimate mVMR in aquatic ecosystems, we generated metagenomes from co-occurring cellular and viral fractions (>50 kDa-200 {micro}m size-range) in freshwater, seawater and solar saltern ponds (10 metagenomes, 2 control metaviromes). Viruses outnumbered cells in freshwater by [~]13 fold and in plankton from marine and saline waters by [~]2-4 fold. However, across an additional set of 121 diverse non-aquatic metagenomes including microbial mats, microbialites, soils, freshwater and marine sediments and metazoan-associated microbiomes, viruses, on average, outnumbered cells by barely two-fold. Although viruses likely are the most diverse biological entities on Earth, their global numbers might be closer to those of cells than previously estimated.

microbiology↗