Biology subjects

Maloney, A. E.

Publications and source records attributed to Maloney, A. E..

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↗

bioRxiv2025

Microbial Resuscitation and Growth Rates in Deep Permafrost: Lipid Stable Isotope Probing Results from the Permafrost Research Tunnel in Fox, Alaska

Permafrost is at increasing risk of thaw as cold regions in the Northern Hemisphere continue to warm. Of particular concern is ice-rich, organic-rich, syngenetic "yedoma" type permafrost. The lability of organic carbon in permafrost post-thaw largely depends on the rate at which microorganisms resuscitate and proliferate after thousands of years in below-freezing, dark, anaerobic conditions. However, the resuscitation and growth rates of microorganisms in deep permafrost are unknown. To quantify these rates, we conducted lipid stable isotope probing (lipid-SIP) on permafrost cores collected from four locations within the Permafrost Tunnel near Fairbanks, Alaska. We compare rates of microbial growth, marker gene sequences, and greenhouse gas (CO2, CH4) emissions across cores held anaerobically at ambient and elevated temperatures. In deep, ancient permafrost, microbial biomass turnover is exceedingly slow, often undetectable, within the first month following thaw. Our results indicate microbial growth in response to anaerobic thaw has a notable lag period, where only 0.001 - 0.01% of cells turn over per day. This suggests a slow reawakening that could provide some buffer between anomalous warmth and C degradation if permafrost refreezes seasonally. However, within six months, microbial communities undergo dramatic restructuring and succession, producing communities that are distinct from both the emplaced ancient and overlying surface communities. These results have critical implications for predictions of microbial biogeochemical contributions in a warming arctic, especially as thaw proceeds into deeper and more ancient permafrost horizons. Plain Language SummaryPermafrost, earth material like soil, rock, or ice continually frozen for more than two years, contains more organic carbon than is currently in the atmosphere as CO2. As the Arctic warms and permafrost thaws, ancient microbes can reactivate, allowing the degradation of organic carbon that has accumulated in permafrost over millenia, resulting in the release of greenhouse gases. In this work, we measured the rates at which permafrost microorganisms resuscitate during thaw and related these growth rates to changes in microbial community composition and greenhouse gas emissions. Key PointsO_LIMicrobial growth is extremely slow within the first 30 days of thaw. Temperature may drive which taxa are active, but not growth rates. C_LIO_LISubsurface microbes show a preference for glycolipids over phospholipids, suggesting a possible cryotolerance adaptation. C_LIO_LIAncient, entrapped gases may be the primary source of emissions in early thaw stages. C_LI

microbiology↗

bioRxiv2021

Diverse arsenic-containing lipids in the surface ocean

Arsenic is present at nanomolar levels throughout the surface ocean, and microbes assimilate this toxic element due to its similarity to inorganic phosphorus. Although the concentration and characterization of dissolved arsenic has been a focus of ocean studies, the size of the particulate arsenic pool and its partitioning into organic molecules within the microbial community is not known. We measured the particulate pool of arsenic in five surface samples from the open ocean and determined the contribution of arsenic-containing lipids to this pool. Here we show that the accumulation of arsenic into lipids is a widespread phenomenon in the surface ocean. Particulate arsenic concentrations were 15 to 42 pmol L-1 with 7-20% of the particulate arsenic pool in the form of arsenolipids. We characterized these arsenolipids and found that arsenosugar phospholipids dominated the arsenolipid pools in our samples with a minor component of arsenohydrocarbons and other unidentified lipids. A significant portion of the arsenosugar phospholipids (up to 35%) were present as previously undescribed mixed acyl ether lipids, suggesting a bacterial source. Scientific significance statementMarine microbes experience constant exposure to the toxic element arsenic. However, there are no baseline measurements of how much arsenic accumulates in microbial communities nor do we know the full spectrum of arsenic containing biomolecules produced in marine systems. In culture-based studies there is strong evidence that phytoplankton synthesize arsenic-containing lipids, but these lipids have not been observed in natural communities of marine microbes. Here we make measurements of bulk particulate arsenic at five sites in the surface open ocean and show that a significant portion of this particulate arsenic is present as complex arsenic-containing lipids. We characterize this arsenolipid pool chemically and quantitatively to show a variety of chemically distinct and quantitatively significant lipids that expand our understanding of marine arsenic biogeochemistry. Data availability statementMass spectrometry data and its associated metadata will be available on Dryad with publication. Scripts for data processing and figure generation found on github at https://github.com/kheal/particulate_As_data_analysis.

ecology↗