Biology subjects

Templeton, A.

Publications and source records attributed to Templeton, A..

3 recordsLinked to original sources

bioRxiv2025

Dissolved inorganic carbon supports robust anabolism and methanogenesis in actively serpentinizing rocks

Serpentinites, hydrated ultramafic rocks that produce [hyper]alkaline, reducing, H2-rich groundwaters, host subsurface microbial ecosystems. Though in the presence of enormous reducing power, life in serpentinizing systems is limited by oxidant and carbon availability. The forms of carbon that support the serpentinite-hosted microbiome, and their rates of biological assimilation, remain poorly understood. In this work, we quantify the habitability of subsurface environments shaped by serpentinization and examine the forms of carbon that support their microbial constituents, focusing specifically on dissolved inorganic carbon, acetate, and formate. We access reacted groundwater from Earths largest terrestrial serpentinizing body and measure carbon assimilation at the single-cell level. Across all conditions, we consistently observe robust assimilation of dissolved inorganic carbon into microbial biomass. Notably, we find that dissolved inorganic carbon supports the majority of methanogenic activity in the system, even at hyperalkaline conditions (pH > 11). Inferred bioenergetic fluxes suggest that rates of biological hydrogen-consumption and methanogenesis are relevant at the landscape scale. We identify a strong potential for the microbiome to be stimulated by increases in H2 and CO2, a finding with implications for the search for life on other planetary bodies and for the growing deployment of fluid injection technologies in ultramafic rocks, such as geological hydrogen production or carbon mineralization. Significance StatementWhen iron-rich rocks interact with water, they undergo a "serpentinization" reaction that results in the production of H2 and [hyper]alkaline fluids. This abiotic process does not operate alone but rather supports and interacts with microbial life. However, it remains unknown to what extent the stressors of subsurface life under [hyper]alkaline conditions may limit microbial activity. In this work, we quantify the rates at which microorganisms transform different carbon sources across a range of serpentinizing conditions. We find that serpentinizing rocks host a remarkably robust microbiome, a finding that motivates the targeting of serpentinizing systems for life detection efforts in our solar system, as well as further analysis of efforts to leverage serpentinites for industrial-scale geological H2 and carbon drawdown projects.

microbiology↗

bioRxiv2023

Quantitative measurement of microbial growth rate with Raman microspectroscopy

Rates of microbial activity and growth are fundamental to understanding environmental geochemistry and ecology. However, measuring the heterogeneity of microbial activity at the single-cell level, especially within complex populations and environmental matrices, remains a forefront challenge. Stable Isotope Probing (SIP) is a standard method for assessing microbial activity and involves measuring the incorporation of an isotopically labeled compound into microbial biomass. Here, we assess the utility of Raman microspectroscopy as a SIP technique, specifically focusing on the measurement of deuterium (2H), a tracer of microbial biomass production. We generate calibrations of microbial biomass 2H values and find that Raman microspectroscopy reliably quantifies 2H incorporation ranging between 0 and 40 at. %. Applying the results of this calibration to a SIP model, we explicitly parameterize the factors controlling microbial growth quantification, demonstrating how Raman-SIP can measure the growth of microorganisms with doubling times ranging from hours to years. Furthermore, we correlatively compare our Raman-derived measurements with those of nanoscale secondary ion mass spectrometry (nanoSIMS) to compare the relative strengths of nanoSIMS- and Raman-based SIP approaches. We find that Raman microspectroscopy is a robust, accessible methodology that can readily differentiate and quantify the growth of individual microbial cells in complex samples. ImportanceGrowth rate, the rate at which organisms grow and reproduce, is a key metric with which to evaluate microbial physiology and contributions to system-level processes. The heterogeneity of microbial growth across space, time, and populations is often difficult to capture with bulk-scale techniques. Single-cell methods hold promise for measuring the heterogeneity of microbial growth rates and responses to changing conditions in situ, without the need for cultivation of microbial isolates. In this study, we evaluated the ability of Raman microspectroscopy, a non-destructive and rapid technique, to measure the assimilation of isotopically labeled water into individual microbial cells and thereby calculate their rates of growth. We explicitly parameterize the factors controlling the quantification of microbial growth rate and compare this technique to standard methods. The framework we report allows researchers to couple single-cell and aggregate rate measurements to functional or system-level properties, a forefront challenge in microbiology.

microbiology↗

bioRxiv2020

Metagenomic Insights into Microbial Metabolisms of a Sulfur-Influenced Glacial Ecosystem

Biological sulfur cycling in polar, low-temperature ecosystems is an understudied phenomenon in part due to difficulty of access and the ephemeral nature of such environments. One such environment where sulfur cycling plays an important role in microbial metabolisms is located at Borup Fiord Pass (BFP) in the Canadian High Arctic. Here, transient springs emerge from the toe of a glacier creating a large proglacial aufeis (spring-derived ices) that are often covered in bright yellow/white sulfur, sulfate, and carbonate mineral precipitates that are accompanied by a strong odor of hydrogen sulfide. Metagenomic sequencing from multiple sample types at sites across the BFP glacial system produced 31 highly complete metagenome assembled genomes (MAGs) that were queried for sulfur-, nitrogen- and carbon-cycling/metabolism genes. Sulfur cycling, especially within the Sox complex of enzymes, was widespread across the isolated MAGs and taxonomically associated with the bacterial classes Alpha-, Beta-, Gamma-, and Epsilon- Proteobacteria. While this does agree with previous research from BFP implicating organisms within the Gamma- and Epsilon- Proteobacteria as the primary classes responsible for sulfur oxidation, our new data suggests putative sulfur oxidation by organisms within Alpha- and Beta- Proteobacterial classes which was not predicted. These findings indicate that in a low-temperature, ephemeral sulfur-based environment such as this, functional redundancy may be a key mechanism that microorganisms use to co-exist whenever energy is limited and/or focused by redox chemistry. ImportanceBorup Fiord Pass is a unique environment characterized by a sulfur-enriched glacial ecosystem, in the low-temperature environment of the Canadian High Arctic. This unique combination makes BFP one of the best analog sites for studying icy, sulfur-rich worlds outside of our own, such as Europa and Mars. The site also allows investigation of sulfur-based microbial metabolisms in cold environments here on Earth. Herein, we report whole genome sequencing data that suggests sulfur cycling metabolisms at BFP are more widely used across bacterial taxa than predicted. From our data, the metabolic capability of sulfur oxidation among multiple community members appears likely due to functional redundancy within their genomes. Functional redundancy, with respect to sulfur-oxidation at BFP, may indicate that this dynamic ecosystem hosts microorganisms that are able to use multiple sulfur electron donors alongside other important metabolic pathways, including those for carbon and nitrogen.

microbiology↗