Biology subjects

Steen, A. D.

Publications and source records attributed to Steen, A. D..

14 recordsLinked to original sources

bioRxiv2026

Tracing the evolution of microbial alkaline phosphatases and their role in phosphorus recycling through time

Phosphorus (P) recycling in seawater is critical for maintaining nutrient availability and marine primary productivity. This process is catalyzed by alkaline phosphatases enzymes, which hydrolyze dissolved organic phosphorus (DOP) compounds, releasing inorganic P for cellular assimilation. Here, we reconstructed the evolutionary history of three major alkaline phosphatase families through deep time using phylogenetic reconciliation across the tree of life. We further quantified their distribution and cellular localization across major metabolic groups using extant genomes to assess how the oceans capacity for P regeneration has changed through time. Our results demonstrate that alkaline phosphatases emerged early in the Archaean, indicating that DOP has sustained marine ecosystems for most of Earths history. A pronounced expansion and diversification of alkaline phosphatases occurred during the Neoproterozoic, coinciding with the rise and ecological diversification of algae. Across metabolic groups, extracellular alkaline phosphatases are particularly concentrated in ferric iron reducers, fermenters, and aerobic heterotrophs, but are comparatively rare in other metabolisms. This distribution suggests that the efficiency of marine P recycling has been strongly influenced by prevailing metabolic strategies and environmental redox conditions. Overall, our results provide new insights into the enzymatic drivers of marine P cycling and the mechanisms that maintained marine productivity as Earths surface became progressively oxygenated and biologically complex.

microbiology↗

bioRxiv2025

Microbial exoenzymes catalyzed the transition to an oxygenated Earth

Microbial exoenzymes--extracellular enzymes secreted to degrade complex organic polymers-- are essential for recycling carbon and nutrients, thus sustaining primary productivity in todays oceans1. Yet, their evolutionary history and role in shaping Earths early biosphere remain entirely unexplored. Here, we trace the origins of microbial exoenzymes and reveal their previously unrecognized role in driving planetary oxygenation. Our results show that exoenzymes are more common in microorganisms utilizing high-energy metabolisms, likely reflecting the energetic costs of enzyme biosynthesis and secretion. They are especially advantageous in environments rich in particulate organic matter (POM). A refined carbon cycle model indicates that early Archean oceans offered few such habitats, as low productivity and intense UV radiation rapidly photodegraded POM. However, with a Paleoproterozoic rise of atmospheric oxygen2, increased oxidative weathering boosted marine primary productivity and POM accumulation3, creating conditions favoring exoenzyme evolution. Molecular clock analyses further indicate that alkaline phosphatase, a key phosphorus-releasing exoenzyme, had likely emerged with the permanent rise of oxygen, enabling more efficient phosphorus recycling. We propose that exoenzymes initiated a positive feedback loop: by accelerating nutrient regeneration, they fueled cyanobacterial productivity and oxygen release, which in turn favored greater exoenzyme capacity, reinforcing long-term oxygenation of the planet.

microbiology↗

bioRxiv2025

Functional genomic signatures predict microbial culturability across the tree of life

Most microbial taxa on Earth remain uncultivated, limiting our ability to study their physiology, ecology, and roles in environmental processes. Although metagenome-assembled genomes (MAGs) have expanded access to uncultured phylogenetic diversity, the functional basis for culturability remains poorly understood. Here, we analyze the 52,515 MAGs from the Genomes from Earths Microbiomes (GEM) catalog to test two hypotheses: 1) genomes from uncultured microbes encode more functionally novel genes than those from cultured taxa, and 2) specific genomic features are systematically associated with culturability across phyla. To assess functional novelty, we aligned predicted proteins to SwissProt and measured sequence dissimilarity to the nearest curated homolog. We find that uncultured MAGs, particularly among Archaea, harbor substantially more divergent proteins. To identify genomic traits predictive of culturability, we combined pathway-level enrichment with LASSO regression and permutation-based feature importance. Cultured MAGs were consistently enriched in Clusters of Orthologous Groups (COG) pathways related to vitamin and cofactor biosynthesis (e.g., thiamine, folate, B12), energy metabolism (e.g., TCA cycle), and CRISPR-Cas systems--functions often depleted in uncultured counterparts. LASSO models identified a subset of these pathways as strong predictors of cultured status even in poorly sampled phyla, suggesting conserved genomic signatures of culturability. In contrast, pathways such as purine biosynthesis and NADH dehydrogenase were associated with uncultured lineages, highlighting potential barriers to cultivation. These results 1) demonstrate the great functional novelty of uncultured microbes, potentially offering unprecedented opportunities for discoveries of novel function, and 2) identify metabolic traits associated with culturability to inform future cultivation strategies. ImportanceThe vast majority of microbes are uncultured, which means they have never been characterized under laboratory conditions. We showed that genomic sequences of uncultured microbes have less similarity to characterized proteins compared to cultured microbes, revealing that there may be fundamental biological reasons why they are not cultured. We also showed that certain metabolic pathways, such as those related to vitamin and cofactor biosynthesis, can predict the ability of microbes to grow under laboratory conditions, and these pathways are abundant in highly cultured phyla, indicating how metabolic pathways can influence cultivation strategies.

microbiology↗

bioRxiv2025

Thermophilic traits correlate with slow growth in permafrost soils

Permafrost soil is characterized by prolonged freezing conditions. Thermophilic microbes have been discovered in various permanently cold environments, including permafrost, where they can persist for extended periods. The reason for this apparent mismatch between microbial adaptations and environmental conditions is unclear. Here, we test the hypothesis that thermophilic traits provide selective advantage to extremely slow-growing microbes, even in cold temperatures. We used a computational approach to predict optimal growth rates and several measures of thermophilicity in metagenome-assembled genomes (MAGs) from permafrost and active layer soils in diverse cold regions. We find that in permafrost, where available energy is always low, measures of thermophilicity correlate positively with minimum doubling time, indicating that slow growers in permafrost have more thermophilic traits. This trend is reversed in microbes in active layer soil, in which seasonal thawing, temperature changes, and episodic rain events allow periodic fast growth. Similar trends were observed in the relationship between optimal growth rates and the optimal temperature of nucleoside diphosphate kinase (NDPK), an enzyme whose temperature optimum is known to be correlated to optimal growth temperatures of the host organism. Thermophilic traits within slow growers appear to be environmentally rather than phylogenetically constrained, and thermophilic slow growers share few horizontal gene transfers with other permafrost microbes. These findings suggest that the presence of thermophilic traits in slow-growers appears to be an adaptation to extreme slow growth in a persistently low-energy environment. ImportancePermanently cold environments, including permafrost soils, contain an active microbial community, which appears to include thermophilic, or heat-loving, microorganisms. This appears to be a paradox - how (and why) do microbes adapted to high temperatures live in permanently cold environments? We provide a potential answer: that the well-understood adaptations which allow microorganisms to survive high temperatures are similar to the poorly understood adaptations that allow microbes to persist over long timescales in very low-energy environments, including permafrost and the Earths deep subsurface. The latter environments represent 88% of the all biomass of bacteria and archaea on Earth, but the adaptations of deep subsurface microorganisms are poorly understood. This work is a step towards understanding how microorganisms persist in two different, challenging environments.

microbiology↗

bioRxiv2024

A global atlas of subsurface microbiomes reveals phylogenetic novelty, large scale biodiversity gradients, and a marine-terrestrial divide

Subsurface environments constitute one of Earths largest habitats for microbial life, yet differences between surface and subsurface microbiomes and between marine and terrestrial microbiomes remain unclear. We analyzed 478 archaeal and 1054 bacterial amplicon sequence datasets and 147 metagenomes from diverse and globally distributed surface and subsurface environments. Taxonomic analyses show that archaeal and bacterial diversity is similar in marine and terrestrial microbiomes at local to global scales. However, community composition greatly differs between marine and terrestrial microbiomes, suggesting a horizontal phylogenetic divide between sea and land that mirrors patterns in plant and animal diversity. In contrast, community composition overlapped from surface to subsurface environments indicating vertical diversity continua rather than a discrete subsurface biosphere. Diversity of terrestrial microbiomes decreases from surface to subsurface environments. Marine subsurface diversity and phylogenetic novelty rivaled (bacteria) or even exceeded (archaea) that of surface environments, suggesting that the marine subsurface holds a considerable and underestimated fraction of Earths archaeal and bacterial diversity. TeaserSubsurface ecosystems within Earths crust and seafloor harbor diverse and distinct microbiomes featuring many unknown lineages.

microbiology↗

bioRxiv2023

Complex organic matter degradation by secondary consumers in chemolithoautotrophy-based subsurface geothermal ecosystems

Microbial communities in terrestrial geothermal systems often contain chemolithoautotrophs with well-characterized distributions and metabolic capabilities. However, the extent to which organic matter produced by these chemolithoautotrophs supports heterotrophs remains largely unknown. Here we compared the abundance and activity of peptidases and carbohydrate active enzymes (CAZymes) that are predicted to be extracellular identified in metagenomic assemblies from 63 springs in the Central American and the Andean convergent margin (Argentinian backarc of the Central Volcanic Zone), as well as the plume-influenced spreading center in Iceland. All assemblies contain two orders of magnitude more peptidases than CAZymes, suggesting that the microorganisms more often use proteins for their carbon and/or nitrogen acquisition instead of complex sugars. The CAZy families in highest abundance are GH23 and CBM50, and the most abundant peptidase families are M23 and C26, all four of which degrade peptidoglycan found in bacterial cells. This implies that the heterotrophic community relies on autochthonous dead cell biomass, rather than allochthonous plant matter, for organic material. Enzymes involved in the degradation of cyanobacterial- and algal-derived compounds are in lower abundance at every site, with volcanic sites having more enzymes degrading cyanobacterial compounds and non-volcanic sites having more enzymes degrading algal compounds. Activity assays showed that many of these enzyme classes are active in these samples. High temperature sites (> 80{degrees}C) had similar extracellular carbon-degrading enzymes regardless of their province, suggesting a less well-developed population of secondary consumers at these sites, possibly connected with the limited extent of the subsurface biosphere in these high temperature sites. We conclude that in < 80{degrees}C springs, chemolithoautotrophic production supports heterotrophs capable of degrading a wide range of organic compounds that do not vary by geological province, even though the taxonomic and respiratory repertoire of chemolithoautotrophs and heterotrophs differ greatly across these regions.

biochemistry↗

bioRxiv2021

Functional Redundancy in Ocean Microbiomes Controls Trait Stability

Theory predicts that functional redundancy in microbial communities increases trait stability, meaning that traits or functions are less likely to be lost from the community when species go extinct. However, few experiments have empirically tested this prediction, especially in the context of microbial communities and at the landscape scale. In part, the lack of metrics for functional redundancy in microbial ecosystems has prevented addressing this question. In a companion manuscript we proposed a quantitative metric for functional redundancy called Contribution Evenness (CE) that is optimized to reflect trait stability. Here, we use CE to predict the stability of marine microbial functions to species and transcription loss. Using transcriptomes deposited in the Ocean Microbial Reference Gene Catalog (OM-RGC.v2), a catalog of genes and transcripts sequenced by the TARA Ocean expedition, we quantified the functional redundancy for 4,314 KEGG Orthologs (KOs) across 124 marine sites. Functional redundancy was highly correlated with a latent variable consisting of four ocean physiochemical parameters: oxygen and chlorophyll a concentrations, depth, and salinity. Functional redundancy was higher at the poles than in non-polar regions. Simultaneously, regional {beta}-diversity for individual functions was higher for functions with higher functional redundancy. These observations provide evidence that higher functional redundancy indicates increased stability of microbial ecosystem functions on spatiotemporal scales consistent with surface ocean mixing. We suggest that future changes in ocean physiochemistry could likely influence this stability for functions with lower functional redundancy. ImportanceFunctional redundancy describes the state of multiple species performing the same function. Theory suggests functional redundancy stabilizes microbial community functions from disturbances leading to species loss or other changes to the microbiome. Previous work suggests that functional redundancy is common in ocean microbiomes which implies traits should be more stable among metacommunities. Some laboratory experiments demonstrate this idea, but it is difficult to test in the natural world. In a companion manuscript, we proposed a functional redundancy metric sensitive to trait stability. Here, we used this metric to show that functional redundancy varied substantially among ocean microbiomes and that regions with higher functional redundancy had higher regional trait stability. Last, we noted that variations in functional redundancy strongly correlated to ocean physiochemistry. Thus, changes in ocean physiochemistry via climate change may alter community traits to become more or less resistant to disturbance relative to contemporary conditions.

microbiology↗

bioRxiv2021

Sustained ability of a natural microbial community to remove nitrate from groundwater

Microbial-mediated nitrate removal from groundwater is widely recognized as the predominant mechanism for nitrate attenuation in contaminated aquifers and is largely dependent on the presence of a carbon-bearing electron donor. The repeated exposure of a natural microbial community to an electron donor can result in the sustained ability of the community to remove nitrate; this phenomenon has been clearly demonstrated at the laboratory scale. However, in situ demonstrations of this ability are lacking. For this study, ethanol (electron donor) was repeatedly injected into a groundwater well (treatment) for six consecutive weeks to establish the sustained ability of a microbial community to remove nitrate. A second well (control) located up-gradient was not injected with ethanol during this time. The treatment well demonstrated strong evidence of sustained ability as evident by concomitant ethanol and nitrate removal and subsequent sulfate removal upon consecutive exposures. Both wells were then monitored for six additional weeks under natural (no injection) conditions. During the final week, ethanol was injected into both treatment and control wells. The treatment well demonstrated sustained ability as evident by concomitant ethanol and nitrate removal whereas the control did not. Surprisingly, the treatment well did not indicate a sustained and selective enrichment of a microbial community. These results suggested that the predominant mechanism(s) of sustained ability likely exist at the enzymatic- and/or genetic-levels. The results of this study demonstrated that the in situ ability of a microbial community to remove nitrate can be sustained in the prolonged absence of an electron donor. Moreover, these results implied that the electron-donor exposure history of nitrate-contaminated groundwater can play an important role nitrate attenuation. Article Impact StatementGroundwater microbes sustain ability to remove nitrate in absence of carbon and energy source.

ecology↗

bioRxiv2020

A quantitative measure of functional redundancy in microbial ecosystems

The concept of functional redundancy has received considerable attention in both the macroecology and microbial ecology literature. As a result, multiple metrics of functional redundancy have been proposed. These vary in how they weight trait levels, species abundance, functional richness, and species richness. Here we present a new functional redundancy metric tailored for community-aggregated traits, which are traits that are quantified at the community level and can be quantitatively partitioned among species. We call this metric Contribution Evenness (CE) because it measures how evenly species contribute to a community-aggregated trait. As CE is an evenness measurement, it ranges from 0 and 1, where 0 corresponds to a single species contributing to a community-aggregated trait and 1 corresponds to all species contributing equally. Using in silico simulations of species extinctions, we demonstrate that CE reflects the stability of an ecosystem function to species extinction, a hypothesized ecological consequence of functional redundancy. As a positive control and to illustrate how CE can be used with sequence data, we analyzed the functional redundancy of eight nitrogen-transforming pathways using 2,631 metagenome-assembled genomes from 47 marine sites. CE for marine nitrogen cycle marker genes was consistent with our qualitative understanding of which nitrogen pathways are most functionally redundant in the ocean. We found that, on average, the NH4+ assimilation pathway was the most functionally redundant (0.44 {+/-} 0.08) while dissimilatory nitrate reduction was the least redundant (0.005 {+/-} 0.005). As demonstrated here, CE provides a promising framework for measuring trait stability in microbiomes.

microbiology↗

bioRxiv2019

Characterization of the interactive effects of labile and recalcitrant organic matter on microbial growth and metabolism

Geochemical models typically represent organic matter (OM) as consisting of multiple, independent pools of compounds, each accessed by microorganisms at different rates. However, recent findings indicate that organic compounds can interact within microbial metabolisms. The relevance of interactive effects within marine systems is debated and a mechanistic understanding of its complexities, including microbe-substrate relationships, is lacking. As a first step toward uncovering mediating processes, the interactive effects of distinct pools of OM on the growth and respiration of marine bacteria, individual strains and a simple, constructed community of Roseobacter lineage members were tested. Isolates were provided with natural organic matter (NOM) and different concentrations (1, 4, 40, 400 M-C) and forms of labile organic matter (acetate, casamino acids, tryptone, coumarate). The microbial response to the mixed substrate regimes was assessed using viable counts and respiration in two separate experiments. Two marine bacteria and a six-member constructed community were assayed with these experiments. Both synergistic and antagonistic growth responses were evident for all strains, but all were transient. The specific substrate conditions promoting a response, and the direction of that response, varied amongst species. These findings indicate that the substrate conditions that result in OM interactive effects are both transient and species-specific and thus influenced by both the composition and metabolic potential of a microbial community.

microbiology↗

bioRxiv2019

Partitioning of microbial function among taxonomic ranks across the tree of life

Widely used microbial taxonomies, such as the NCBI taxonomy, are based on a combination of sequence homology among conserved genes and historically accepted taxonomies, which were developed based on observable traits such as morphology and physiology. A recently-proposed alternative taxonomy, the Genome Taxonomy Database (GTDB), incorporates only sequence homology of conserved genes and attempts to partition taxonomic ranks such that each rank implies the same amount of evolutionary distance, regardless of its position on the phylogenetic tree. This provides the first opportunity to completely separate taxonomy from traits, and therefore to quantify how taxonomic rank corresponds to traits across the microbial tree of life. We quantified the enrichment of clusters of orthologous gene functional categories (COG-FCs) as a proxy for traits within the lineages of 13,735 cultured and uncultured microbial lineages from a custom-curated genome database. On average, 41.4% of the variation in COG-FC enrichment is explained by taxonomic rank, with domain, phylum, class, order, family, and genus explaining, on average, 3.2%, 14.6%, 4.1%, 9.2%, 4.8%, and 5.5% of the variance, respectively (p<0.001 for all). To our knowledge, this is the first work to quantify the variance in metabolic potential contributed by individual taxonomic ranks. A qualitative comparison between the COG-FC enrichments and genus-level phylogenies, generated from published concatenated protein sequence alignments, further supports the idea that metabolic potential is taxonomically coherent at higher taxonomic ranks. The quantitative analyses presented here constrain the integral relationship between diversification of microbial lineages and the metabolisms which they host.\n\nImportanceRecently there has been great progress in defining a complete taxonomy of bacteria and archaea, which has been enabled by improvements in DNA sequencing technology and new bioinformatic techniques. A new, algorithmically-defined microbial tree of life describes those linkages relying solely on genetic data, which raises the question of how microbial traits relate to taxonomy. Here, we adopted cluster of orthologous group functional categories as a scheme to describe the genomic contents of microbes, which can be applied to any microbial lineage for which genomes are available. This simple approach allows quantitative comparisons between microbial genomes with different gene composition from across the microbial tree of life. Our observations demonstrate statistically significant patterns in cluster of orthologous group functional categories at the taxonomic levels spanning from domain to genus.

microbiology↗

bioRxiv2018

Simulation-based approaches to characterize the effect of sequencing depth on the quantity and quality of metagenome-assembled genomes

We applied simulation-based approaches to characterize how microbial community structure influences the amount of sequencing effort to reconstruct metagenomes that are assembled from short read sequences. An initial analysis evaluated the quantity, completion, and contamination of complete-metagenome-assembled genome (complete-MAG) equivalents, a bioinformatic-pipeline normalized metric for MAG quantity, as a function of sequencing effort, on four preexisting sequence read datasets taken from a maize soil, an estuarine sediment, the surface ocean, and the human gut. These datasets were subsampled to varying degrees of completeness in order to simulate the effect of sequencing effort on MAG retrieval. Modeling suggested that sequencing efforts beyond what is typical in published experiments (1 to 10 Gbp) would generate diminishing returns in terms of MAG binning. A second analysis explored the theoretical relationship between sequencing effort and the proportion of available metagenomic DNA sequenced during a sequencing experiment as a function of community richness, evenness, and genome size. Simulations from this analysis demonstrated that while community richness and evenness influenced the amount of sequencing required to sequence a community metagenome to exhaustion, the effort necessary to sequence an individual genome to a target fraction of exhaustion was only dependent on the relative abundance of the corresponding organism and its genome size. A software tool, GRASE, was created to assist investigators further explore this relationship. Re-evaluation of the relationship between sequencing effort and binning success in the context of the relative abundance of genomes, as opposed to base pairs, provides a framework to design sequencing experiments based on the relative abundance of microbes in an environment rather than arbitrary levels of sequencing effort.

bioinformatics↗

bioRxiv2018

Phylogenetically novel uncultured microbial cells dominate Earth microbiomes

To unequivocally determine a microbes physiology, including its metabolism, environmental roles, and growth characteristics, it must be grown in a laboratory culture. Unfortunately, many phylogenetically-novel groups have never been cultured, so their physiologies have only been inferred from genomics and environmental characteristics. Although the diversity, or number of different taxonomic groups, of uncultured clades has been well-studied, their global abundances, or number of cells in any given environment, have not been assessed. We quantified the degree of similarity of 16S rRNA gene sequences from diverse environments in publicly-available metagenome and metatranscriptome databases, which we show are largely free of the culture-bias present in primer-amplified 16S rRNA gene surveys, to their nearest cultured relatives. Whether normalized to scaffold read depths or not, the highest abundance of metagenomic 16S rRNA gene sequences belong to phylogenetically novel uncultured groups in seawater, freshwater, terrestrial subsurface, soil, hypersaline environments, marine sediment, hot springs, hydrothermal vents, non-human hosts, snow and bioreactors (22-87% uncultured genera to classes and 0-64% uncultured phyla). The exceptions were human and human-associated environments which were dominated by cultured genera (45-97%). We estimate that uncultured genera and phyla could comprise 7.3 x 1029 (81%) and 2.2 x 1029 (25%) microbial cells, respectively. Uncultured phyla were over-represented in meta transcript omes relative to metagenomes (46-84% of sequences in a given environment), suggesting that they are viable, and possibly more active than cultured clades. Therefore, uncultured microbes, often from deeply phylogenetically divergent groups, dominate non-human environments on Earth, and their undiscovered physiologies may matter for Earth systems.

microbiology↗

bioRxiv2016

Extracellular peptidases in subsurface sediments of the White Oak River estuary, NC, suggest microbial community adaptation to oxidize degraded organic matter

Anoxic subsurface sediments contain communities of heterotrophic microorganisms that metabolize organic carbon at extraordinarily slow rates. In order to assess the mechanisms by which subsurface microorganisms access detrital sedimentary organic matter, we measured kinetics of a range of extracellular peptidases in anoxic sediments of the White Oak River estuary, NC. Nine distinct peptidase substrates were enzymatically hydrolyzed at all depths. Potential peptidase activities (Vmax) decreased with increasing sediment depth, although Vmax expressed on a per cell basis was approximately the same at all depths. Half-saturation constants (Km) decreased with depth, indicating peptidases that functioned more efficiently at low substrate concentrations. Potential activities of extracellular peptidases acting on molecules that are enriched in degraded organic matter (D-phenylalanine and L-ornithine) increased relative to enzymes that act on L-phenylalanine, further suggesting microbial community adaptation to access degraded organic matter. Nineteen classes of predicted, exported peptidases were identified in genomic data from the same site, of which genes for class C25 (gingipain-like) peptidases represented more than 40% at each depth. Methionine aminopeptidases, zinc carboxypeptidases, and class S24-like peptidases, which are involved in single-stranded DNA repair, were also abundant. These results suggest a subsurface heterotrophic microbial community that primarily accesses low-quality detrital organic matter via a diverse suite of well-adapted extracellular enzymes.\n\nIO_SCPLOWMPORTANCEC_SCPLOWBurial of organic carbon in marine and estuarine sediments represents a long-term sink for atmospheric carbon dioxide. Globally, [~]40% of organic carbon burial occurs in anoxic estuaries and deltaic systems. However, the ultimate controls on the amount of organic matter that is buried in sediments, versus oxidized into CO2, are poorly constrained. Here we used a combination of enzyme assays and metagenomic analysis to identify how subsurface microbial communities catalyze the first step of proteinaceous organic carbon degradation. Our results show that microbial communities in deeper sediments are adapted to access molecules characteristic of degraded organic matter, suggesting that those heterotrophs are adapted to life in the subsurface.

ecology↗