Biology subjects

McFarlin, J.

Publications and source records attributed to McFarlin, J..

3 recordsLinked to original sources

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↗

bioRxiv2023

The hydrogen isotope signatures of autotrophy versus heterotrophy recorded in archaeal tetraether lipids

The stable hydrogen isotope composition of archaeal lipids is emerging as a potential paleoenvironmental proxy, adding to the well-established application of plant leaf wax-derived n-alkanes in paleohydrological reconstruction. A handful of studies reported relatively invariant and depleted hydrogen isotope compositions for archaeal lipids despite the range of different organisms and growth conditions explored. However, how modes of metabolism and physiological state (growth phase) affect the hydrogen isotope signatures of archaeal lipids remains poorly understood, limiting our ability to interpret archaeal lipid biomarker records from the environment. Here we conducted water isotope label experiments with a metabolically flexible and well-studied model archaeon Archaeoglobus fulgidus and quantified the hydrogen isotope fractionation between lipids and water in response to different carbon substrates and electron donor-acceptor pairs. The 2H/1H fractionation between lipids and water ({varepsilon}L/W) was overall negative, ranging from -280 to -226 {per thousand}, and overlapped with the ranges observed for other archaea in previous studies. Isotope flux-balance model results suggest that [≥]80 % and [≥]50 % of lipid-bound H in A. fulgidus cultures directly reflect water isotope compositions (i.e., not via organic substrate or H2) during autotrophy and heterotrophy, respectively. The model results also suggest the final saturation during isoprenoid lipid biosynthesis catalyzed by a flavoenzyme geranylgeranyl reductase likely contributes to the large 2H/1H fractionation observed in this study, consistent with previous isotope flux-balance model results for a different archaeon. Finally, we synthesized available data to compare {varepsilon}L/W patterns across all three domains of life: Bacteria, Archaea and Eukarya. Emerging patterns between archaeal and eukaryotic lipids are consistent with the notion of highly fractionating geranylgeranyl reductase, and the patterns between archaeal and bacterial lipids suggest that the general state of energy limitation may also contribute to large, negative values of {varepsilon}L/W observed in prokaryotic lipids. Altogether, these findings lend further support for the potential of archaeal lipid {varepsilon}L/W as a paleohydrological proxy and provide a broader insight into the 2H/1H fractionation mechanisms potentially shared among prokaryotic and eukaryotic lipid biomarkers.

microbiology↗

bioRxiv2022

Hydrogen stable isotope probing of lipids demonstrates slow rates of microbial growth in soil

The rate at which microorganisms grow and reproduce is fundamental to our understanding of microbial physiology and ecology. While soil microbiologists routinely quantify soil microbial biomass levels and the growth rates of individual taxa in culture, there is a limited understanding of how quickly microbes actually grow in soil. For this work, we posed the simple question: what are the growth rates of soil microorganisms? In this study, we measure these rates in three distinct soil environments using hydrogen stable isotope probing of lipids with 2H-enriched water. This technique provides a taxa-agnostic quantification of in situ microbial growth from the degree of 2H enrichment of intact polar lipid compounds ascribed to bacteria and fungi. We find that average apparent generation times in soil are quite slow (20 to 64 days) but also highly variable at the compound-specific level (6 to 1137 days), suggesting differential growth rates between community subsets. We observe that low-biomass communities can exhibit more rapid growth rates than high-biomass communities, highlighting that biomass quantity alone does not predict microbial productivity in soil. Furthermore, within a given soil, the rates at which specific lipids are being synthesized do not relate to their quantity, suggesting a general decoupling of microbial abundance and growth in soil microbiomes. More generally, we demonstrate the utility of lipid stable isotope probing for measuring microbial growth rates in soil and highlight the importance of measuring growth rates to complement more standard analyses of soil microbial communities. SignificanceGeneration times, how quickly organisms grow and reproduce, are a key feature of biology. However, there are few measurements of microbial generation times in soil, despite the crucial importance of soil microbes to terrestrial ecosystems. By measuring the rate at which isotopically labeled water is incorporated into microbial membranes, we find that the generation times of soil microorganisms are far longer than those typically observed in culture. Surprisingly, we observe that lower-biomass soils exhibited faster growth rates than high-biomass soils. More abundant microorganisms are not necessarily the fastest growing and most soil microorganisms are slow growers. Our results underscore the importance of considering slow and variable growth rates when studying microbial communities and their contributions to ecosystem processes.

microbiology↗