Biology subjects

Onstott, T. C.

Publications and source records attributed to Onstott, T. C..

5 recordsLinked to original sources

bioRxiv2025

Diverse but temporally stable virome in a 1.2 km deep karst aquifer accessed via Moab Khotsong mine, South Africa

Despite their ubiquity, viruses remain understudied in many of Earths environments. The deep subsurface contains a large portion of Earths biomass and can be expected to hold a rich store of viruses as well. We investigated the viral community in a 1.2-kilometer-deep dolomitic aquifer accessed in the Moab Khotsong gold mine in South Africa by microscopically quantifying virus-like particles (VLP) and cells and conducting a metagenomic survey of viruses and their associations with the microbial community. VLP:cell ratios were consistently lower ([~]1:1) than those found in most shallower aquifers. Viral sequences were recovered from both the <0.2 {micro}m fraction, presumably representing free virions, and the >0.2 {micro}m fraction that also included microbial cells. Viruses were diverse and 78% were novel, and the viral communities were relatively unchanged at four sampling dates spanning five years. Host prediction indicated viral infection of the dominant microbes, including Thiomicrospiraceae and Rhodocyclaceae, with temperate phages. Viral genomes include auxiliary metabolic genes (AMGs), with most of them being Type II, which favor host persistence. Taken together, VLP:cell ratios, type II AMGs, and temporally stable viromes point to dominance of lysogeny and piggyback-the-persistent viral-host interactions in the deep aquifer. The many novel viruses observed here suggest that the terrestrial subsurface is an untapped reservoir of viral diversity.

microbiology↗

bioRxiv2020

Ancestral absence of electron transport chains in Patescibacteria and DPANN

Recent discoveries suggest that the candidate superphyla Patescibacteria and DPANN constitute a large fraction of the phylogenetic diversity of Bacteria and Archaea. Their small genomes and limited coding potential have been hypothesized to be ancestral adaptations to obligate symbiotic lifestyles. To test this hypothesis, we performed cell-cell association, genomic, and phylogenetic analyses on 4,829 individual cells of Bacteria and Archaea from 46 globally distributed surface and subsurface field samples. This confirmed the ubiquity and abundance of Patescibacteria and DPANN in subsurface environments, the small size of their genomes and cells, and the divergence of their gene content from other Bacteria and Archaea. Our analyses suggest that most Patescibacteria and DPANN in the studied subsurface environments do not form specific physical associations with other microorganisms. These data also suggest that their unusual genomic features and prevalent auxotrophies may be a result of minimal cellular energy transduction mechanisms that potentially precede the evolution of respiration, thus relying solely on fermentation for energy conservation.

evolutionary biology↗

bioRxiv2019

The genome of a subterrestrial nematode reveals an evolutionary strategy for adaptation to heat

The nematode Halicephalobus mephisto was originally discovered inhabiting a deep terrestrial aquifer 1.3 km underground. H. mephisto can thrive under conditions of abiotic stress including heat and minimal oxygen, where it feeds on a community of both chemolithotrophic and heterotrophic prokaryotes in an unusual ecosystem isolated from the surface biosphere. Here we report the comprehensive genome and transcriptome of this organism, identifying a signature of adaptation: an expanded repertoire of 70 kilodalton heat-shock proteins (Hsp70) and avrRpt2 induced gene 1 (AIG1) proteins. We find that positive selection has driven the expansion of Hsp70 genes, which are also transcriptionally induced upon growth under heat stress. We further show that AIG1 may have been acquired by horizontal gene transfer (HGT) from a rhizobial fungus. Over one-third of the genes of H. mephisto are novel, highlighting the divergence of this nematode from other sequenced organisms. This work sheds light on the genomic strategies of adaptation to heat in the first complete subterrestrial eukaryotic genome.

genomics↗

bioRxiv2018

Life Inside A Dinosaur Bone: A Thriving Microbiome

Fossils were long thought to lack original organic material, but the discovery of organic molecules in fossils and sub-fossils, thousands to millions of years old, has demonstrated the potential of fossil organics to provide radical new insights into the fossil record. How long different organics can persist remains unclear, however. Non-avian dinosaur bone has been hypothesised to preserve endogenous organics including collagen, osteocytes, and blood vessels, but proteins and labile lipids are unstable during diagenesis or over long periods of time. Furthermore, bone is porous and an open system, allowing microbial and organic flux. Some of these organics within fossil bone have therefore been identified as either contamination or microbial biofilm, rather than original organics. Here, we use biological and chemical analyses of Late Cretaceous dinosaur bones and sediment matrix to show that dinosaur bone hosts a diverse microbiome. Fossils and matrix were freshly-excavated, aseptically-acquired, and then analysed using microscopy, spectroscopy, chromatography, spectrometry, DNA extraction, and 16S rRNA amplicon sequencing. The fossil organics differ from modern bone collagen chemically and structurally. A key finding is that 16S rRNA amplicon sequencing reveals that the subterranean fossil bones host a unique, living microbiome distinct from that of the surrounding sediment. Even in the subsurface, dinosaur bone is biologically active and behaves as an open system, attracting microbes that might alter original organics or complicate the identification of original organics. These results suggest caution regarding claims of dinosaur bone soft tissue preservation and illustrate a potential role for microbial communities in post-burial taphonomy.

paleontology↗

bioRxiv2017

Labeling of prokaryotic mRNA in live cells using fluorescent in situ hybridization of transcript-annealing molecular beacons (FISH-TAMB)

High-throughput sequencing and cellular imaging have expanded our knowledge of microbial diversity and expression of cellular activity. However, it remains challenging to characterize low-abundance, slow-growing microorganisms that play key roles in biogeochemical cycling. With the goal of isolating transcriptionally active cells of these microorganisms from environmental samples, we developed fluorescent in situ hybridization of transcript-annealing molecular beacons (FISH-TAMB) to label living prokaryotic cells. FISH-TAMB utilizes polyarginine cell-penetrating peptides to deliver molecular beacons across cell walls and membranes. Target cells are fluorescently labeled via hybridization between molecular beacons and messenger RNA of targeted functional genes. FISH-TAMBs target specificity and deliverance into both bacterial and archaeal cells were demonstrated by labeling intracellular methyl-coenzyme M reductase A (mcrA) transcripts expressed by Escherichia coli mcrA+, Methanosarcina barkeri, and a methanogenic enrichment of deep continental fracture fluid. Growth curve analysis supported sustained cellular viability following FISH-TAMB treatment. Flow cytometry and confocal microscopy detected labeled single cells and single cells in aggregates with unlabeled cells. As FISH-TAMB is amenable to target any functional gene of interest, when coupled with cell sorting, imaging, and sequencing techniques, FISH-TAMB will enable characterization of key uncharacterized rare biosphere microorganisms and of the syntrophically activated metabolic pathways between physically associated microorganisms.

microbiology↗