Biology subjects

Rogers, T. J.

Publications and source records attributed to Rogers, T. J..

4 recordsLinked to original sources

bioRxiv2025

Virus-mediated recycling of chemoautotrophic biomass

Aquatic environments absorb [~]2.5 gigatonnes of atmospheric carbon each year1, more than the carbon stored in the atmosphere, soils, and all biomass combined. Primary producers transform this dissolved inorganic carbon into biomass that can subsequently flow into other trophic levels, or be released back into the environment through viral lysis. While there is substantial knowledge about the diversity and activity of viruses infecting photoautotrophic primary producers, little is known about viruses infecting chemoautotrophs, representing a gap in our understanding of key microbial processes driving global carbon cycles. Here, we combine metagenomics with 12/13C stable isotopic probing mesocosm experiments in a marine-derived meromictic pond to quantify lineage-specific carbon cycling activity to identify key microbial populations driving carbon cycling. We then tracked the flow of carbon from active chemoautotrophs to their viruses and found evidence supporting virus-mediated recycling of chemoautotrophic biomass through the production of viral particles. In particular, active populations of hydrogen/sulfur-oxidizing chemoautotrophs (Thiomicrorhabdus, Hydrogenovibrio, Sulfurimonas, Sulfurovum) were targeted by viruses. Considering the widespread distribution of chemoautotrophs on Earth, we postulate that this previously overlooked component of the microbial carbon cycle is a globally relevant process that has implications for our planets carbon cycle. This work provides the foundation for revealing the role of viral lysis in chemoautotrophic primary production and builds toward biogeochemical models that incorporate viral recycling of chemoautotrophic biomass. Summary statementThe diversity, mechanisms, and processes governing microbial primary production and the recycling of autotrophic biomass are fundamental to our planets carbon cycle. These processes have implications for carbon sequestration, ocean biogeochemistry, and the overall balance of carbon dioxide in the atmosphere. Beneath the Earths sunlit layer, primary production is driven by microbial chemoautotrophs that derive energy from the oxidation of reduced compounds, such as hydrogen and sulfur, to form the base of the food web. Growing evidence suggests that aquatic ecosystems fueled by chemoautotrophy are widely distributed on Earth, ranging from beneath ice shelves to coastal upwelling regions to oxygen minimum zones, deep-sea hydrothermal vents and cold seeps, groundwater, and meromictic ponds and lakes2-7. Studying microbial processes regulating chemoautotrophic primary production and the recycling of chemoautotrophic biomass is fundamental to our understanding of global carbon cycles. While the diversity, function, and activity of viruses targeting photoautotrophs have been well-described across aquatic ecosystems8, we have little understanding of viruses involved in the recycling of chemoautotrophic biomass. Viruses are a major source of cellular mortality and carbon cycling in aquatic environments9-11. Viral lysis is estimated to transform [~]150 gigatonnes of carbon annually from biomass back into the environment, equivalent to [~]25 times that of the oceans biological carbon pump12,13. Despite recognition of the important role of viruses in aquatic habitats, there is a large gap in our understanding of the impact of viruses on globally distributed chemoautotrophs2,4,5,14-18. In this study, we show that viruses are not merely passive players but active agents recycling carbon fixed by productive chemoautotrophs, fundamentally reshaping how we view carbon and nutrient cycling in redox-active ecosystems.

microbiology↗

bioRxiv2024

An alternative route for β-hydroxybutyrate metabolism supports fatty acid synthesis in cancer cells

Cancer cells are exposed to diverse metabolites in the tumor microenvironment that are used to support the synthesis of nucleotides, amino acids, and lipids needed for rapid cell proliferation1-3. Recent work has shown that ketone bodies such as {beta}-hydroxybutyrate ({beta}-OHB), which are elevated in circulation under fasting conditions or low glycemic diets, can serve as an alternative fuel that is metabolized in the mitochondria to provide acetyl-CoA for the tricarboxylic acid (TCA) cycle in some tumors4-7. Here, we discover a non-canonical route for {beta}-OHB metabolism, in which {beta}-OHB can bypass the TCA cycle to generate cytosolic acetyl-CoA for de novo fatty acid synthesis in cancer cells. We show that {beta}-OHB-derived acetoacetate in the mitochondria can be shunted into the cytosol, where acetoacetyl-CoA synthetase (AACS) and thiolase convert it into acetyl-CoA for fatty acid synthesis. This alternative metabolic routing of {beta}-OHB allows it to avoid oxidation in the mitochondria and net contribute to anabolic biosynthetic processes. In cancer cells, {beta}-OHB is used for fatty acid synthesis to support cell proliferation under lipid-limited conditions in vitro and contributes to tumor growth under lipid-limited conditions induced by a calorie-restricted diet in vivo. Together, these data demonstrate that {beta}-OHB is preferentially used for fatty acid synthesis in cancer cells to support tumor growth.

cancer biology↗

bioRxiv2024

Lipid availability influences ferroptosis sensitivity in cancer cells by regulating polyunsaturated fatty acid trafficking

Ferroptosis is a form of cell death caused by lipid peroxidation that is emerging as a target for cancer therapy, highlighting the need to identify factors that govern ferroptosis susceptibility. Lipid peroxidation occurs primarily on phospholipids containing polyunsaturated fatty acids (PUFAs). Here, we show that even though extracellular lipid limitation reduces cellular PUFA levels, lipid-starved cancer cells are paradoxically more sensitive to ferroptosis. Using mass spectrometry-based lipidomics with stable isotope fatty acid labeling, we show that lipid limitation induces a fatty acid trafficking pathway in which PUFAs are liberated from triglycerides to synthesize highly unsaturated PUFAs such as arachidonic acid and adrenic acid. These PUFAs then accumulate in phospholipids, particularly ether phospholipids, to promote ferroptosis sensitivity. Therefore, PUFA levels within cancer cells do not necessarily correlate with ferroptosis susceptibility. Rather, how cancer cells respond to extracellular lipid levels by trafficking PUFAs into proper phospholipid pools dictates their sensitivity to ferroptosis.

cancer biology↗

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↗