Biology subjects

Lavy, A.

Publications and source records attributed to Lavy, A..

10 recordsLinked to original sources

bioRxiv2024

Scalable cell-free production of active T7 RNA polymerase

The SARS-CoV-2 pandemic highlighted the urgent need for biomanufacturing paradigms that are robust and fast. Here, we demonstrate the rapid process development and scalable cell-free production of T7 RNA polymerase, a critical component in mRNA vaccine synthesis. We carry out a one-liter cell-free gene expression (CFE) reaction that achieves over 80% purity, low endotoxin levels, and enhanced activity relative to commercial T7 RNA polymerase. To achieve this demonstration, we implement rolling circle amplification to circumvent difficulties in DNA template generation, and tune cell-free reaction conditions, such as temperature, additives, purification tags and agitation to boost yields. We achieve production of a similar quality and titer of T7 RNA polymerase over more than 4 orders of magnitude reaction volume. This proof of principle positions CFE as a viable solution for decentralized biotherapeutic manufacturing, enhancing preparedness for future public health crises or emergent threats.

synthetic biology↗

bioRxiv2024

Characterization of sediment and granite hosted deep underground research laboratories reveals diverse microbiome functions, limited temporal variation and substantial genomic conservation

Underground research laboratories (URLs) provide a window on the deep biosphere and enable investigation of potential microbial impacts on nuclear waste, CO2 and H2 stored in the subsurface. We carried out the first multi-year study of groundwater microbiomes sampled from defined intervals between 140 and 400 m below the surface of the Horonobe and Mizunami URLs, Japan. We reconstructed draft genomes for >90% of all organisms detected over a four year period. The Horonobe and Mizunami microbiomes are dissimilar, likely because the Mizunami URL is hosted in granitic rock and the Horonobe URL in sedimentary rock. Despite this, hydrogen metabolism, rubisco-based CO2 fixation, reduction of nitrogen compounds and sulfate reduction are well represented functions in microbiomes from both URLs, although methane metabolism is more prevalent at the organic- and CO2-rich Horonobe URL. High fluid flow zones and proximity to subsurface tunnels select for candidate phyla radiation bacteria in the Mizunami URL. We detected near-identical genotypes for approximately one third of all genomically defined organisms at multiple depths within the Horonobe URL. This cannot be explained by inactivity, as in situ growth was detected for some bacteria, albeit at slow rates. Given the current low hydraulic conductivity and groundwater compositional heterogeneity, ongoing inter-site strain dispersal seems unlikely. Alternatively, the Horonobe URL microbiome homogeneity may be explained by higher groundwater mobility during the last glacial period. Genotypically-defined species closely related to those detected in the URLs were identified in three other subsurface environments in the USA. Thus, dispersal rates between widely separated underground sites may be fast enough relative to mutation rates to have precluded substantial divergence in species composition. Species overlaps between subsurface locations on different continents constrain expectations regarding the scale of global subsurface biodiversity. Overall, microbiome and geochemical stability over the study period has important implications for underground storage applications.

microbiology↗

bioRxiv2021

The Chloroflexi supergroup is metabolically diverse and representatives have novel genes for non-photosynthesis based CO2 fixation

The Chloroflexi superphylum have been investigated primarily from the perspective of reductive dehalogenation of toxic compounds, anaerobic photosynthesis and wastewater treatment, but remain relatively little studied compared to their close relatives within the larger Terrabacteria group, including Cyanobacteria, Actinobacteria, and Firmicutes. Here, we conducted a detailed phylogenetic analysis of the phylum Chloroflexota, the phylogenetically proximal candidate phylum Dormibacteraeota, and a newly defined sibling phylum proposed in the current study, Eulabeiota. These groups routinely root together in phylogenomic analyses, and constitute the Chloroflexi supergroup. Chemoautotrophy is widespread in Chloroflexi. Two Form I Rubisco ancestral subtypes that both lack the small subunit are prevalent in ca. Eulabeiota and Chloroflexota, suggesting that the predominant modern pathway for CO2 fixation evolved in these groups. The single subunit Form I Rubiscos are inferred to have evolved prior to oxygenation of the Earths atmosphere and now predominantly occur in anaerobes. Prevalent in both Chloroflexota and ca. Eulabeiota are capacities related to aerobic oxidation of gases, especially CO and H2. In fact, aerobic and anaerobic CO dehydrogenases are widespread throughout every class-level lineage, whereas traits such as denitrification and reductive dehalogenation are heterogeneously distributed across the supergroup. Interestingly, some Chloroflexota have a novel clade of group 3 NiFe hydrogenases that is phylogenetically distinct from previously reported groups. Overall, the analyses underline the very high level of metabolic diversity in the Chloroflexi supergroup, suggesting the ancestral metabolic platform for this group enabled highly varied adaptation to ecosystems that appeared in the aerobic world.

microbiology↗

bioRxiv2021

Soils and sediments host novel archaea with divergent monooxygenases implicated in ammonia oxidation

Copper membrane monooxygenases (CuMMOs) play critical roles in the global carbon and nitrogen cycles. Organisms harboring these enzymes perform the first, and rate limiting, step in aerobic oxidation of ammonia, methane, or other simple hydrocarbons. Within archaea, only organisms in the order Nitrososphaerales (Thaumarchaeota) encode CuMMOs, which function exclusively as ammonia monooxygenases. From grassland and hillslope soils and aquifer sediments, we identified 20 genomes from distinct archaeal species encoding divergent CuMMO sequences. These archaea are phylogenetically clustered in a previously unnamed Thermoplasmatota order, herein named the Ca. Angelarcheales. The CuMMO proteins in Ca. Angelarcheales are more similar in structure to those in ammonia-oxidizing archaea than those of bacteria, and they contain all functional residues required for activity. Similarly to the Nitrososphaerales, Ca. Angelarcheales genomes are significantly enriched in blue copper proteins (BCPs) relative to sibling lineages, including plastocyanin-like electron carriers and divergent nitrite reductase-like (nirK) 2-domain cupredoxin proteins co-located with electron transport machinery. Angelarcheales do not have identifiable genes for methanol oxidation or carbon fixation, encode significant capacity for peptide/amino acid uptake and degradation, and share numerous electron transport mechanisms with the Nitrososphaerales. In the studied soils and sediments Ca. Angelarcheales were at least as abundant as ammonia-oxidizing Nitrososphaerales. Thus, we predict that Angelarcheales live a mixotrophic lifestyle based on oxidation of ammonia liberated from peptide and amino acid degradation. This work expands the known diversity of Thermoplasmatota and of CuMMO enzymes in archaea and suggests that these organisms are important and previously unaccounted for contributors to nitrogen cycling.

microbiology↗

bioRxiv2020

Meanders as a scaling motif for understanding of floodplain soil microbiome and biogeochemical potential at the watershed scale

Biogeochemical exports of C, N, S and H2 from watersheds are modulated by the activity of microorganisms that function over micron scales. This disparity of scales presents a substantial challenge for development of predictive models describing watershed function. Here, we tested the hypothesis that meander-bound regions exhibit patterns of microbial metabolic potential that are broadly predictive of biogeochemical processes in floodplain soils along a river corridor. We intensively sampled floodplain soils located in the upper, middle, and lower reaches of the East River in Colorado and reconstructed 248 draft quality genomes representative at a sub-species level. Approximately one third of the representative genomes were detected across all three locations with similar levels of abundance, and despite the very high microbial diversity and complexity of the soils, ~15% of species were detected in two consecutive years. A core floodplain microbiome was enriched in bacterial capacities for aerobic respiration, aerobic CO oxidation, and thiosulfate oxidation with the formation of elemental sulfur. We did not detect systematic patterns of gene abundance based on sampling position relative to the river. However, at the watershed scale meander-bound floodplains appear to serve as scaling motifs that predict aggregate capacities for biogeochemical transformations in floodplain soils. Given this, we conducted a transcriptomic analysis of the middle site. Overall, the most highly transcribed genes were amoCAB and nxrAB (for nitrification) followed by genes involved in methanol and formate oxidation, and nitrogen and CO2 fixation. Low soil organic carbon correlated with high activity of genes involved in methanol, formate, sulfide, hydrogen, and ammonia oxidation, nitrite oxidoreduction, and nitrate and nitrite reduction. Thus, widely represented genetic capacities did not predict in situ activity at one time point, but rather they define a reservoir of biogeochemical potential available as conditions change.

microbiology↗

bioRxiv2019

Taxonomically and metabolically distinct microbial communities with depth and across a hillslope to riparian zone transect

Watersheds are important for supplying fresh water, the quality of which depends on complex interplay involving physical, chemical and biological processes. As water percolates through the soil and underlying weathering rock en route to the river corridor, microorganisms mediate key geochemical transformations, yet the distribution and functional capacities of subsurface microbial communities remain little understood. We have studied metabolic capacities of microbial communities along a meadow to floodplain hillslope transect within the East-River watershed, Colorado, using genome resolved metagenomics and carbon and hydrogen stable isotopes. Very limited strain/species overlap was found at different depths below the ground surface and at different distances along the hillslope, possibly due to restricted hydraulic connectivity after early stages of snowmelt. Functions such as carbon fixation and selenate reduction were prevalent at multiple sites, although the lineages of organisms responsible tend to be location-specific. Based on its abundance, sulfur is significantly more important for microbial metabolism at the floodplain compared to on the hillslope. Nitrification and methylamine oxidation are likely only occurring within the floodplain, with nitrification capacity in shallow soil, and methylamine oxidation in deeper unsaturated sediment. Biogenic methane was detected in deep surface samples, but methanogenic organisms were not identified. Originality-Significance StatementIn a previous study within a hillslope to riparian zone transect of a sub-alpine watershed, the community structure was explored using ribosomal protein S3 genes, and the metabolic potential was hypothesized based on the presence of metabolism related genes. However, tying specific strains and species to metabolic functioning was not discussed as resolved genomes were not available. In the current study, we use genome-resolved metagenomics along with carbon and hydrogen stable isotopes to explore the spatial distribution of biogeochemical processes. By linking taxonomy and function, using multiple functional genes indicative of full metabolic pathways, we detect heterogeneity in the distribution of metabolic potential and the organisms involved with depth and landscape position. Thus, we infer how microbiome genomic variation impacts biogeochemical cycling across the watershed. We found very limited strain/species overlap at different depths below the surface and along the hillslope, possibly due to the restricted site to site hydraulic connectivity, and show that communities are largely distinct in their metabolic capacities. Both proximity to the river and the underlying Mancos shale apparently control species distribution and metabolic potential. Functions such as carbon fixation and selenate reduction were prevalent at multiple sites, although the lineages of organisms responsible tend to be location-specific. Arsenate detoxification was found to be prevalent in the riparian zone whereas selenate reduction was detected within weathered Mancos shale. We conclude that important ecosystem functions are strongly associated with the riparian zone, some of which may have crucial implications as to water quality and human health.

bioinformatics↗

bioRxiv2019

Consistent metagenome-derived metrics verify and define bacterial species boundaries

Longstanding questions relate to the existence of naturally distinct bacterial species and genetic approaches to distinguish them. Bacterial genomes in public databases form distinct groups, but these databases are subject to isolation and deposition biases. We compared 5,203 bacterial genomes from 1,457 environmental metagenomic samples to test for distinct clouds of diversity, and evaluated metrics that could be used to define the species boundary. Bacterial genomes from the human gut, soil, and the ocean all exhibited gaps in whole-genome average nucleotide identities (ANI) near the previously suggested species threshold of 95% ANI. While genome-wide ratios of non-synonymous and synonymous nucleotide differences (dN/dS) decrease until ANI values approach [~]98%, estimates for homologous recombination approached zero at [~]95% ANI, supporting breakdown of recombination due to sequence divergence as a species-forming force. We evaluated 107 genome-based metrics for their ability to distinguish species when full genomes are not recovered. Full length 16S rRNA genes were least useful because they were under-recovered from metagenomes, but many ribosomal proteins displayed both high metagenomic recoverability and species-discrimination power. Taken together, our results verify the existence of sequence-discrete microbial species in metagenome-derived genomes and highlight the usefulness of ribosomal genes for gene-level species discrimination.

microbiology↗

bioRxiv2019

Clades of huge phage from across Earth’s ecosystems

Phage typically have small genomes and depend on their bacterial hosts for replication. DNA sequenced from many diverse ecosystems revealed hundreds of huge phage genomes, between 200 kbp and 716 kbp in length. Thirty-four genomes were manually curated to completion, including the largest phage genomes yet reported. Expanded genetic repertoires include diverse and new CRISPR-Cas systems, tRNAs, tRNA synthetases, tRNA modification enzymes, translation initiation and elongation factors, and ribosomal proteins. Phage CRISPR-Cas systems have the capacity to silence host transcription factors and translational genes, potentially as part of a larger interaction network that intercepts translation to redirect biosynthesis to phage-encoded functions. In addition, some phage may repurpose bacterial CRISPR-Cas systems to eliminate competing phage. We phylogenetically define major clades of huge phage from human and other animal microbiomes, oceans, lakes, sediments, soils and the built environment. We conclude that their large gene inventories reflect a conserved biological strategy, observed over a broad bacterial host range and across Earths ecosystems.

microbiology↗

bioRxiv2018

Microbial communities across a hillslope-riparian transect shaped by proximity to the stream, groundwater table, and weathered bedrock

Watersheds are important suppliers of freshwater for human societies. Within mountainous watersheds, microbial communities impact water chemistry and element fluxes as water from precipitation events discharges through soils and underlying weathered rock, yet there is limited information regarding the structure and function of these communities. Within the East River, CO watershed, we conducted a depth-resolved, hillslope to riparian zone transect study to identify factors that control how microorganisms are distributed and their functions. Metagenomic and geochemical analyses indicate that distance from the East River and proximity to groundwater and underlying weathered shale strongly impact microbial community structure and metabolic potential. Riparian zone microbial communities are compositionally distinct from all hillslope communities. Bacteria from phyla lacking isolated representatives consistently increase in abundance with increasing depth, but only in the riparian zone saturated sediments did we find Candidate Phyla Radiation bacteria. Riparian zone microbial communities are functionally differentiated from hillslope communities based on their capacities for carbon and nitrogen fixation and sulfate reduction. Selenium reduction is prominent at depth in weathered shale and saturated riparian zone sediments. We anticipate that the drivers of community composition and metabolic potential identified throughout the studied transect will predict patterns across the larger watershed hillslope system.

microbiology↗

bioRxiv2017

Dramatic expansion of microbial groups that shape the global sulfur cycle

The biogeochemical cycle of sulfur on Earth is driven by microbial sulfate reduction, yet organisms from relatively few lineages have been implicated in this process. Recent studies using functional marker genes have detected abundant, novel dissimilatory sulfite reductases that confer the capacity for microbial sulfate reduction and could do not be affiliated with known organisms. Thus, the identity of a significant fraction of sulfate reducing microbes has remained elusive. Here we report the discovery of the capacity for sulfate reduction in the genomes of organisms from twelve bacterial and archaeal phyla, thereby doubling the number of microbial phyla associated with this process. Eight of the twelve newly identified groups are candidate phyla that lack isolated representatives, a finding only possible given genomes from metagenomes. Two candidate phyla, Candidatus Rokubacteria and Candidatus Hydrothermarchaeota contain the earliest evolved genes. The capacity for sulfate reduction has been laterally transferred in multiple events within some phyla, and a key gene potentially capable of switching sulfur oxidation to sulfate reduction in associated cells has been acquired by putatively symbiotic bacteria. We conclude that functional predictions based on phylogeny will significantly underestimate the extent of sulfate reduction across Earths ecosystems. Understanding the prevalence of this capacity is integral to interpreting the carbon cycle because sulfate reduction is often coupled to turnover of buried organic carbon. Our findings expand the diversity of microbial groups associated with sulfur transformations in the environment and motivate revision of biogeochemical process models based on microbial community composition.

microbiology↗