Biology subjects

Orsi, W. D.

Publications and source records attributed to Orsi, W. D..

12 recordsLinked to original sources

bioRxiv2026

Seafloor topography structures subseafloor microbial communities in the Puerto Rico Trench

The influence of seafloor topography on subseafloor microbial communities is poorly understood. In this study, we systematically sampled subseafloor sedimentary microbial communities and pore-water geochemistry at bathyal, abyssal, and hadal water depths of the Puerto Rico Trench. The Puerto Rico Trench exhibits vertical relief of over 8 km with seafloor topography shaped by active plate tectonics and characterized by a very steep southern wall and active mass wasting. Sampling across these features, we find that subseafloor microbial communities are influenced by topography in the following two ways. First, subseafloor sediment in the deepest part of the trench is anoxic, enriched in organic matter due to mass transport of sediment from shallower water depths, and contains an anaerobic subseafloor community that is quite distinct from the anaerobic subseafloor community in anoxic sediment at bathyal depths. The difference between these bathyal and hadal subseafloor anaerobic communities is consistent with influence of water-depth-related physical properties on subseafloor community composition. Second, subseafloor sediment remains oxygenated for meters below seafloor on steep slopes within the bathyal zone, an abyssal topographic high within the trench, and the abyssal plain seaward of the trench subseafloor, likely due to limited sediment accumulation, which selects for the presence of aerobic microbial communities. The difference between these bathyal and abyssal aerobic subseafloor communities and the anaerobic communities at bathyal and hadal depths reflects the role of seafloor topography in structuring subseafloor availability of redox reactants, which in turn drives the activities and composition of subseafloor microbial communities.

microbiology↗

bioRxiv2026

Piezophilic activity dominates the Puerto Rico Trench deep subseafloor biosphere

Hydrostatic pressure is a defining feature of the deep ocean, yet how it structures microbial activity across the subseafloor biosphere is poorly understood. Here, we assess pressure effects on anabolic activity in seafloor and subseafloor communities across a margin-to-hadal-to-abyssal transect of the Puerto Rico Trench region (493-8,385 m water depth). Community-level responses to pressure reverse with burial, revealing a previously unrecognized shift toward piezophily in resident subseafloor communities down to 20 meters below seafloor (mbsf). In pressure-incubation experiments, atmospheric pressure yielded higher proportions of active cells in surficial sediments, whereas in situ pressure yielded higher proportions in the subseafloor. Pressure also structured active-community composition; in trench-axis sediments extending to 8.35 mbsf, JS1/Atribacterota populations belonging to geographically widespread hadal lineages exhibited a physiological response to in situ pressure, indicative of subseafloor piezophily. These findings suggest that hydrostatic pressure acts as an ecological filter after burial, favoring piezophilic traits that may support microbial persistence in the deep subseafloor biosphere.

microbiology↗

bioRxiv2026

Protist quantitative stable isotope probing identifies diverse active grazers in natural freshwater communities

Bacterivorous protists are central to aquatic food webs, mediating the transfer of carbon and nutrients to higher trophic levels through the microbial loop. In natural communities, a major challenge remains in linking protist grazing activity to environmental sequences and identifying which taxa are actively feeding at the community level. Here, we present the first application of quantitative stable isotope probing (qSIP) in a grazing experiment. By combining qSIP with 18S rRNA gene amplicon sequencing, we linked prey assimilation to the identity of active protist predators at the operational taxonomic unit (OTU) level. In a replicated 36-h bottle-experiment, live 13C, 15N-labeled Limnohabitans planktonicus cells were added to natural samples from a lake pelagic site and its main inlet stream. Although hydrologically connected, protist richness was higher in the inlet than in the lake, yet a similar number of taxa incorporated prey biomass, comprising 108 OTUs in the inlet and 107 OTUs in the lake, including both rare and abundant taxa. Of these, 26 OTUs were labeled at both sites. The most strongly labeled protist in the inlet was a putative phago-mixotrophic prasinophyte, whereas in the lake it was an uncultured chrysophyte. Across sites, prey incorporation occurred in a broad range of taxa, including heterotrophs (e.g., choanoflagellates, cercozoans, ciliates, centrohelids), putative mixotrophs (e.g., cryptophytes, chrysophytes, dictyochophytes), parasitic protists and fungi. These results demonstrate the potential of qSIP to resolve trophic interactions at fine taxonomic resolution in natural communities and highlight new opportunities to study complex microbial food webs across environmental systems.

ecology↗

bioRxiv2026

Non-enzymatic assimilation of organosulfur compounds at the interface of geochemistry and biochemistry

Dimethyl sulfide (DMS) and dimethyl sulfoxide (DMSO) have important microbial-driven roles in global nutrient cycling, chemotaxis and/or climate regulation. Microbial DMSO and DMS assimilation were thought to require their enzymatic reduction to methanethiol. However, reactive oxygen species were recently shown to mediate methane production from DMS and DMSO. Here, we show that this oxidative mechanism can sustain microbial growth without the need for enzymes to directly reduce DMS or oxidize DMSO. Both, light and heat were effective geochemical drivers of this mechanism that yielded methanesulfonic acid and sulfite, and which mimicked the stepwise oxidation of DMSO by monooxygenases that only enzymatically enhance this oxidation reaction. Furthermore, we demonstrated intracellular DMSO degradation, in which sulfur and the simultaneously released carbon were both utilized by microbes. This study emphasizes that metabolic pathways are not necessarily enzyme-driven, with putatively ancient, non-enzymatic reaction networks taking place at a transition between geochemistry and biochemistry.

biochemistry↗

bioRxiv2022

Body-plan reorganization in a sponge correlates with microbiome change

Mounting evidence suggests that animals and their associated bacteria interact via intricate molecular mechanisms, and it is hypothesized that disturbances to the microbiome can influence animal development. Sponges diverged from other animals more than 750 MYA and represent one of the earliest branching animal phyla that exhibit symbiotic relationships with diverse bacteria. Over 41 microbial phyla have been found in association with sponges, forming a holobiont that is integral to aquatic ecosystems worldwide. Sponge-associated microbes contain an enriched set of proteins bearing eukaryotic-like domains, and their metabolism supports the host with nutrients. This indicates strong physiological interconnections in the holobiont, which are thought to be modulated by sponge immunity and pattern-recognition proteins. Despite the hypothesized tight physiological integration and ancient origin of the sponge holobiont, the effect of changes in the symbiotic community on the sponge metabolism and morphogenesis remains poorly understood. Here, we show that the loss of a key microbial sponge symbiont correlates with a stark body plan reorganization of the sponge host. This reorganization is coupled with broad transcriptomic changes and includes the modulation of signaling pathways known to be involved in morphogenesis and innate immune response in sponges and other animals. This study provides a combined genetic, physiological, and morphological assessment of the effect of changes in the microbiome on sponge post-embryonic development and homeostasis. The drastic microbiome reorganization and the correlated response observed in the sponge host provide evidence for a coupling between sponge transcriptomic state and the state of its microbiome. Our results suggest that sponges use molecular mechanisms to respond to changes in their microbiome and that the ability to sense and respond to microbiome perturbations has deep evolutionary origins among animals.

genomics↗

bioRxiv2020

Genome evolution in bacteria isolated from million-year-old subseafloor sediments

Beneath the seafloor, microbial life subsists in isolation from the surface world under persistent energy limitation. The nature and extent of genomic evolution in subseafloor microbes has been unknown. Here we show that the genomes of Thalassospira bacterial populations cultured from million-year-old subseafloor sediments evolve by point mutation, with a relatively low rate of homologous recombination and a high frequency of pseudogenes. Ratios of synonymous to non-synonymous mutation rates correlate with the accumulation of pseudogenes, consistent with a dominant role for genetic drift in the subseafloor strains, but not in type strains of Thalassospira isolated from the surface world. Our findings demonstrate that the long term physical isolation of these bacteria, in the absence of recombination, has resulted in clonal populations that evolve consistent with Mullers Ratchet, whereby reduced access to novel genetic material from neighbors has resulted in fixation of new mutations that accumulate in genomes over millions of years. Significance statementThe nature and extent of genomic evolution in subseafloor microbial populations subsisting for millions of years below the seafloor is unknown. Subseafloor populations have ultra-slow metabolic rates that are hypothesized to restrict reproduction and, consequently, the spread of new traits. Our findings demonstrate that genomes of cultivated bacterial strains from the genus Thalassospira isolated from million-year-old abyssal sediment exhibit greatly reduced levels of homologous recombination, elevated numbers of pseudogenes, and genome-wide evidence of relaxed purifying selection. These substitutions and pseudogenes are fixed into the population, suggesting the genome evolution of these bacteria has been dominated by genetic drift, whereby under long-term physical isolation in small population sizes, and in the absence of homologous recombination, newly acquired mutations accumulate in the genomes of clonal populations over millions of years.

microbiology↗

bioRxiv2020

Chloroflexi persisting for millions of years in oxic and anoxic deep-sea clay

Chloroflexi are widespread in energy-limited subseafloor sediments, but how Chloroflexi respond to subseafloor energy limitation under oxic and anoxic conditions is poorly understood. Here, we characterize the diversity, abundance, activity, and metabolic potential of Chloroflexi in oxic and anoxic abyssal clay from three deep-sea cores covering up to 15 million years of sediment deposition, where Chloroflexi are a major component of the community throughout the entire cored sequence at all sites. In oxic red clay at two different sites, Chloroflexi communities exhibit net death over both 10-15 million year cored sequences, and gene expression was below detection despite the availability of oxygen as a high energy electron acceptor, indicating a reduced level of activity. In contrast at the anoxic site, Chloroflexi abundance and gene expression increase below the seafloor and peak in 2 to 3 million year old sediment. The anaerobic subseafloor Chloroflexi exhibited a homoacetogenic metabolism and potential for energetically efficient intracellular H2 recycling that have been proposed to confer a fitness advantage in energy-limited subseafloor habitats. Our findings indicate that the expression of this energy efficient metabolism in Chloroflexi coincides with net growth over million year timescales in deep-sea anoxic clay. Significance statementChloroflexi are widespread in energy-limited subseafloor sediments, both in oxic subseafloor sediments that are energetically limited by the availability of electron donors (organic matter) and in anoxic sediments that are energetically limited by the availability of high energy terminal electron acceptors. How Chloroflexi respond to these different forms of energy limitation over long time scales is poorly understood. We present new data that demonstrates how key differences in metabolism are manifested in different communities of aerobic and anaerobic Chloroflexi subsisting over millions of years in oxic and anoxic deep-sea clay. These data provide new insights into how certain Chloroflexi respond to different types of long-term energy limitation.

microbiology↗

bioRxiv2020

Contesting the evidence for gene expression in lower oceanic crust

Li et al [Nature 579, 250-255 (2020)] report microbial gene expression in deep ocean crust, from microbial communities that have concentrations as low as 100 cell per cubic cm. This would be incredible, since that would be the lowest biomass sample ever analyzed for gene expression for a deep biosphere sample by several orders of magnitude. However, I have reanalyzed the data and show that the authors data are derived from contamination via seawater, humans, human skin associated bacteria, drilling fluid, and molecular reagent kits. The method that the authors used to produce their gene expression data is highly sensitive to DNA contamination, which is the case here. The authors claim that Pseudomonas, a known widespread contaminant in molecular reagent kits, is one of the most active groups in their lower crust samples and base their metabolic analysis on this contaminating organism. Here, I show that the gene expression data are derived from contaminating Pseudomonas (as well as other groups), and I show that the groups claimed as being active in the rock samples are also present in the negative controls at similar or higher relative abundance. For example, methane production in long term incubations was reported but gene expression from methanogens was 10 times higher in the drill fluid negative controls compared to the rock samples, demonstrating that the methane measured is likely derived from methanogen contaminants introduced from the drill fluid. There are no signs of active life here, but lipid biomarkers were found preserved in the rocks. Thus, the authors have sampled a fossilized biosphere, not a living one.

microbiology↗

bioRxiv2020

Anaerobic metabolism of Foraminifera thriving below the seafloor

Foraminifera are single-celled eukaryotes (protists) of large ecological importance, as well as environmental and paleoenvironmental indicators and biostratigraphic tools. In addition, they are capable of surviving in anoxic marine environments where they represent a major component of the benthic community. However, the cellular adaptations of Foraminifera to the anoxic environment remain poorly constrained. We sampled an oxic-anoxic transition zone in marine sediments from the Namibian shelf, where the genera Bolivina and Stainforthia dominated the Foraminifera community, and use metatranscriptomics to characterize Foraminifera metabolism across the different geochemical conditions. The relative abundance of Foraminifera gene expression in anoxic sediment depths increased an order of magnitude, which was confirmed in a ten-day incubation experiment where the development of anoxia coincided with a 27-fold increase in the relative abundance of Foraminifera protein encoding transcripts. This indicates that many Foraminifera were not only surviving, but thriving under the anoxic conditions. The anaerobic energy metabolism of these active Foraminifera was characterized by fermentation of sugars and amino acids, dissimilatory nitrate reduction, fumarate reduction, and dephosphorylation of creatine phosphate. This was co-expressed alongside genes involved in production of reticulopodia, phagocytosis, calcification, and clathrin-mediated-endocytosis (CME). Thus, Foraminifera may use CME under anoxic conditions to utilize dissolved organic matter as a carbon and energy source, in addition to ingestion of prey cells via phagocytosis. These mechanisms help explain how some Foraminifera can thrive under anoxia, which would help to explain their ecological success documented in the fossil record since the Cambrian period more than 500 million years ago.

microbiology↗

bioRxiv2020

Textile waste and microplastic induce activity and development of unique hydrocarbon-degrading marine bacterial communities

Biofilm-forming microbial communities on plastics and textile fibers are of growing interest since they have potential to contribute to disease outbreaks and material biodegradability in the environment. Knowledge on microbial colonization of pollutants in the marine realm is expanding, but metabolic responses during substrate colonization remains poorly understood. Here, we assess the metabolic response in marine microbial communities to three different micropollutants, virgin high-density polyethylene (HDPE) microbeads, polysorbate-20 (Tween), and textile fibers. Intertidal textile fibers, mainly cotton, virgin HDPE, and Tween induced variable levels of microbial growth, respiration, and community assembly in controlled microcosm experiments. RAMAN characterization of the chemical composition of the textile waste fibers and high-throughput DNA sequencing data shows how the increased metabolic stimulation and biodegradation is translated into selection processes ultimately manifested in different communities colonizing the different micropollutant substrates. The composition of the bacterial communities colonizing the substrates were significantly altered by micropollutant substrate type and light conditions. Bacterial taxa, closely related to the well-known hydrocarbonoclastic bacteria Kordiimonas spp. and Alcanivorax spp., were enriched in the presence of textile-waste. The findings demonstrate an increased metabolic response by marine hydrocarbon-degrading bacterial taxa in the presence of microplastics and textile waste, highlighting their biodegradation potential. The metabolic stimulation by the micropollutants was increased in the presence of light, possibly due to photochemical dissolution of the plastic into smaller bioavailable compounds. Our results suggest that the development and increased activity of these unique microbial communities likely play a role in the bioremediation of the relatively long lived textile and microplastic pollutants in marine habitats. Graphical Abstract O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=104 SRC="FIGDIR/small/939876v1_ufig1.gif" ALT="Figure 1"> View larger version (40K): org.highwire.dtl.DTLVardef@19322f3org.highwire.dtl.DTLVardef@dbae7dorg.highwire.dtl.DTLVardef@9c9d4aorg.highwire.dtl.DTLVardef@1aa636_HPS_FORMAT_FIGEXP M_FIG C_FIG

microbiology↗

bioRxiv2019

Lokiarchaeon exhibits homoacetogenesis

The proposed Asgard superphylum of Archaea comprises the closest archaeal relatives of eukaryotes, whose genomes hold clues pertaining to the nature host cell that acquired the mitochondrion at the origin of eukaryotes1-4. Genomes of the Asgard candidate Phylum Candidatus Lokiarchaeota [Lokiarchaeon] suggest an acetogenic H2 -dependent lifestyle5 and mixotrophic capabilities6. However, data on the activity of Lokiarchaeon are currently lacking, and the ecology of the host cell that acquired the mitochondrion is debated4,7. Here, we show that in anoxic marine sediments underlying highly productive waters on the Namibian continental shelf Lokiarchaeon gene expression increases with depth below the seafloor, and was significantly different across a redox gradient spanning hypoxic to sulfidic conditions. Notably, Lokiarchaeon increased expression of genes involved in growth, carbohydrate metabolism, and the H2-dependent Wood-Ljungdahl (WLP) carbon fixation pathway under the most reducing (sulfidic) conditions. Quantitative stable isotope probing experiments revealed multiple populations of Lokiarchaeota utilizing both CO2 and diatomaceous extracellular polymeric substances (dEPS) as carbon sources over a 10-day incubation under anoxic conditions. This apparent anaerobic mixotrophic metabolism was consistent with the expression of Lokiarchaeon genes involved in transport and fermentation of sugars and amino acids. Remarkably, several Asgard populations were more enriched with 13C-dEPS compared to the community average, indicating a preference for dEPS as a growth substrate. The qSIP and gene expression data indicate a metabolism of \"Candidatus Lokiarchaeota\" similar to that of sugar fermenting homoacetogenic bacteria8, namely that Lokiarchaeon can couple fermentative H2 production from organic substrates with electron bifurcation and the autotrophic and H2-dependent WLP. Homoacetogenesis allows to access a wide range of substrates and relatively high ATP gain during acetogenic sugar fermentation8 thereby providing an ecological advantage for Lokiarchaeon in anoxic, energy limited settings.

microbiology↗

bioRxiv2017

A 16S rRNA gene sequencing and analysis protocol for the Illumina MiniSeq platform

High-throughput sequencing of the 16S rRNA gene is widely used in microbial ecology, with Illumina platforms being widely used in recent studies. The MiniSeq, Illuminas latest benchtop sequencer, enables more cost-efficient DNA sequencing relative to larger sequencing platforms (e.g. MiSeq). Here we used a modified custom primer sequencing approach to test the fidelity of the MiniSeq for high-throughput sequencing of the V4 hypervariable region of 16S rRNA genes from complex communities in environmental samples. To this end, we designed an additional sequencing primer that enabled application of a dual-index barcoding method on the MiniSeq. A mock community was sequenced alongside the environmental samples as a quality control benchmark. After careful filtering procedures, we were able to recapture a realistic richness of the mock community, and identify meaningful differences in alpha and beta diversity in the environmental samples. These results show that the MiniSeq can produce similar quantities of high quality V4 reads compared to the MiSeq, yet is a cost-effective option for any laboratory interested in performing high-throughput 16S rRNA gene sequencing.\n\nIMPORTANCEWe modified a custom sequencing approach and used a mock community to test the fidelity of high-throughput sequencing on the Illumina MiniSeq platform. Our results show that the MiniSeq can produce similar quantities of high quality V4 reads compared to the MiSeq. In addition, our protocol increases feasibility for small laboratories to perform their own high-throughput sequencing of the 16S rRNA marker gene.

microbiology↗