Biology subjects

Cobban, A.

Publications and source records attributed to Cobban, A..

4 recordsLinked to original sources

bioRxiv2024

The clumped isotope signatures of multiple methanogenesis metabolisms

Methane is a potent greenhouse gas, an important energy source, and a potential biosignature on extraterrestrial planetary bodies. The relative abundances of doubly substituted ("clumped") methane isotopologues (13CH3D and 12CH2D2) offer important information on the sources and sinks of methane. However, the clumped isotope signatures of microbially produced methane from different methanogenic pathways lack a systematic investigation. In this study, we provide a dataset encompassing the relative isotopologue abundances produced by hydrogenotrophic, methylotrophic, acetoclastic, and methoxydotrophic methanogenesis. We find that a statistical "combinatorial effect" generates significant differences in 12CH2D2 compositions between hydrogenotrophic methanogenesis and other pathways. The thermodynamic drive of methanogenic reactions and phylogenetic affiliation may also influence the isotope compositions of methane. Our study provides new experimental constraints on the isotope signatures of different microbial methanogenic pathways, and evidence of the mechanisms responsible for the observed differences. TeaserA novel stable isotope tool to track and differentiate sources of biological methane.

microbiology↗

bioRxiv2024

Lipid hydrogen isotope compositions primarily reflect growth water in the model archaeon Sulfolobus acidocaldarius

The stable hydrogen isotope composition ({delta}2H) of lipid biomarkers can track environmental processes and remain stable over geologically relevant time scales, enabling studies of past climate, hydrology, and ecology. Most research has focused on lipids from the domain Eukarya (e.g., plant waxes, long-chain alkanes), and the potential of prokaryotic lipid biomarkers from the domain Archaea to offer unique insights into environments not captured by eukaryotic lipids remains unclear. Here, we investigate the H-isotope composition of biphytanes in Sulfolobus acidocaldarius, a model thermoacidophile and obligate heterotroph. We conducted a series of experiments that varied temperature, pH, shaking rate, electron acceptor availability, or electron donor flux. From these experiments, we quantified the lipid/water H-isotope fractionation (2{varepsilon}L/W) values for core biphytane chains derived from tetraether lipids. The 2{varepsilon}L/W values are consistently negative (-230 to - 180 {per thousand}) and are relatively invariant across all experiments despite a 20-fold change in doubling times and 2-fold change in lipid cyclization. The magnitude and relative invariance of 2{varepsilon}L/W values are consistent with studies on other heterotrophic archaea and suggests archaeal lipids may be faithful recorders of the {delta}2H composition of growth water. Our study highlights the potential of archaeal lipid {delta}2H as a hydrological proxy, offering new insights into environments where traditional proxies, such as plant-derived lipids, are not available, including extreme environments and extraterrestrial settings. ImportanceReconstructing past climates is crucial for understanding Earths environmental history and its responses to changing conditions. This study examines Sulfolobus acidocaldarius, a thermoacidophilic archaeon that thrives in extreme environments like hot springs. These microorganisms incorporate hydrogen water in the growth environment into membrane lipids, creating hydrogen isotope signatures that can reflect hydroclimate conditions. Our findings show that these hydrogen isotope ratios remain consistent even under varying temperature, pH, oxygen levels, and electron donor fluxes, indicating a stable fractionation between lipids and water. This invariance suggests that S. acidocaldarius lipids could serve as a robust proxy for reconstructing ancient water H-isotope values, especially in extreme environments where traditional proxies, such as plant waxes, are absent. This research has broader implications for planetary-scale reconstructions, including potential applications in studying past climates on other planets, such as Mars, where similar microorganisms may have existed in hydrothermal conditions.

microbiology↗

bioRxiv2020

Multiple environmental parameters impact core lipid cyclization in Sulfolobus acidocaldarius

Environmental reconstructions based on microbial lipids require understanding the coupling between environmental conditions and membrane physiology. The paleotemperature proxy TEX86 is built on the observation that archaea alter the number of five- and six-membered rings in the hydrophobic core of their glycerol dibiphytanyl glycerol tetraether (GDGT) membrane lipids when growing at different temperatures. However, recent work with these archaea also highlights a role for other factors, such as pH or energy availability in determining the degree of core lipid cyclization. To better understand the role of these variables we cultivated a model Crenarchaeon, Sulfolobus acidocaldarius, over a range in temperature, pH, oxygen flux, or agitation speed, and quantified the changes in growth rate, biomass yield, and core lipid compositions. The average degree of cyclization in core lipids correlated with growth rate under most conditions. When considered alongside other experimental findings from both the thermoacidophilic and mesoneutrophilic archaea, the results suggest the cyclization of archaeal lipids records a universal response to energy availability at the cellular level. Although we isolated the effects of individual parameters, there remains a need for multi-factor experiments (e.g., pH + temperature + redox) to establish a robust framework to interpret biomarker records of environmental change.

microbiology↗

bioRxiv2019

Energy flux controls tetraether lipid cyclization in Sulfolobus acidocaldarius

Microorganisms regulate the composition of their membranes in response to environmental cues. Many archaea maintain the fluidity and permeability of their membranes by adjusting the number of cyclic moieties within the cores of their glycerol dibiphytanyl glycerol tetraether (GDGT) lipids. Cyclized GDGTs increase membrane packing and stability, which has been shown to help cells survive shifts in temperature and pH. However, the extent of this cyclization also varies with growth phase and electron acceptor or donor limitation. These observations indicate a relationship between energy metabolism and membrane composition. Here we show that the average degree of GDGT cyclization increases with doubling time in continuous cultures of the thermoacidophile Sulfolobus acidocaldarius (DSM 639). This is consistent with the behavior of a mesoneutrophile, Nitrosopumilus maritimus SCM1. Together, these results demonstrate that archaeal GDGT distributions can shift in response to electron donor flux and energy availability, independent of pH or temperature. Paleoenvironmental reconstructions based on GDGTs thus capture the energy available to microbes, which encompasses fluctuations in temperature and pH, as well as electron donor and acceptor availability. The ability of Archaea to adjust membrane composition and packing may be an important strategy that enables survival during episodes of energy stress.\n\nSignificance StatementMicrobial lipid membranes protect and isolate a cell from its environment while regulating the flow of energy and nutrients to metabolic reaction centers within. We demonstrate that membrane lipids change as a function of energy flux using a well-studied archaeon that thrives in acidic hot springs and observe an increase in membrane packing as energy becomes more limited. These observations are consistent with chemostat experiments utilizing a low temperature, neutral pH, marine archaeon. This strategy appears to regulate membrane homeostasis is common across GDGT-producing lineages, demonstrating that diverse taxa adjust membrane composition in response to chronic energy stress.

microbiology↗