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Eukaryotes may experience oxygen deprivation under both physiological and pathological conditions. Because oxygen shortage leads to a reduction in cellular energy production, all eukaryotes studied so far conserve energy by suppressing their metabolism. However, the molecular physiology of animals that naturally and repeatedly experience anoxia is underexplored. One such animal is the marine nematode Laxus oneistus. It thrives, invariably coated by its sulfur-oxidizing symbiont Candidatus Thiosymbion oneisti, in anoxic sulfidic or hypoxic sand. Here, transcriptomics and proteomics showed that, whether in anoxia or not, L. oneistus mostly expressed genes involved in ubiquitination, energy generation, oxidative stress response, immune response, development, and translation. Importantly, ubiquitination genes were also highly expressed when the nematode was subjected to anoxic sulfidic conditions, together with genes involved in autophagy, detoxification and ribosome biogenesis. We hypothesize that these degradation pathways were induced to recycle damaged cellular components (mitochondria) and misfolded proteins into nutrients. Remarkably, when L. oneistus was subjected to anoxic sulfidic conditions, lectin and mucin genes were also upregulated, potentially to promote the attachment of its thiotrophic symbiont. Furthermore, the nematode appeared to survive oxygen deprivation by using an alternative electron carrier (rhodoquinone) and acceptor (fumarate), to rewire the electron transfer chain. On the other hand, under hypoxia, genes involved in costly processes (e.g., amino acid biosynthesis, development, feeding, mating) were upregulated, together with the worm's Toll-like innate immunity pathway and several immune effectors (e.g., bactericidal/permeability-increasing proteins, fungicides). In conclusion, we hypothesize that, in anoxic sulfidic sand, L. oneistus upregulates degradation processes, rewires the oxidative phosphorylation and reinforces its coat of bacterial sulfur-oxidizers. In upper sand layers, instead, it appears to produce broad-range antimicrobials and to exploit oxygen for biosynthesis and development.
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http://dx.doi.org/10.1038/s41598-022-13235-9 | DOI Listing |
Nature
August 2025
Division of Microbial Ecology, Centre for Microbiology and Environmental Systems, University of Vienna, Vienna, Austria.
Microorganisms have driven Earth's sulfur cycle since the emergence of life, yet the sulfur-cycling capacities of microorganisms and their integration with other element cycles remain incompletely understood. One such uncharacterized metabolism is the coupling of sulfide oxidation with iron(III) oxide reduction, a ubiquitous environmental process hitherto considered to be strictly abiotic. Here we present a comprehensive genomic analysis of sulfur metabolism across prokaryotes, and reveal bacteria that are capable of oxidizing sulfide using extracellular solid phase iron(III).
View Article and Find Full Text PDFFront Microbiol
August 2025
Department of Biology, Indiana Wesleyan University, Marion, IN, United States.
Despite their potential for harboring novel microorganisms exhibiting beneficial metabolisms or that produce useful products for biotechnology and industry, alkaline lakes and soils are among the least studied extreme environments. With its high productivity and meromictic water column, haloalkaline Soap Lake (Washington, USA) is among the most intriguing soda lakes in the world. We sampled the water column of Soap Lake and used both culture-based and culture-independent (16S rRNA amplicon-based) methods to analyze the microbial diversity of both its oxic and anoxic waters.
View Article and Find Full Text PDFJ Hazard Mater
July 2025
Department of Civil and Mineral Engineering, University of Toronto, 35 St. George Street, Toronto, Ontario M5S 1A4, Canada. Electronic address:
Acidification and dissolved oxygen (DO) depletion in mining-affected water bodies are global environmental challenges associated with the oxidation of reduced S species (S), including sulfide and sulfur oxidation intermediate compounds (SOI). The recent detection of diverse SOI species in tailings impoundments and pit lakes highlights overlooked risks from microbial S cycling, that are difficult to geochemically quantify due to rapid S turnover. This study characterizes sulfur-reducing bacteria (SRB; capable of sulfate and/or SOI reduction), in Base Mine Lake (BML), the first oil sands tailings reclamation end pit lake.
View Article and Find Full Text PDFACS Omega
July 2025
Key Laboratory of Unconventional Natural Gas Evaluation and Development in Complex Tectonic Areas, Ministry of Natural Resources of the People's Republic of China, Guiyang 550004, China.
The purpose of this research was to examine the paleoenvironment, hydrothermal activity, and restriction water condition of the Lower Cambrian Niutitang Formation shale gas reservoir in northern Guizhou and analyze the controlling factors for organic matter enrichment. This investigation is based on the geochemical analyses of the total organic carbon (TOC) and major and trace elements from drill core samples of YF1 Well in Fenggang Area, Northern Guizhou. TOC of the Niutitang Formation is mainly distributed between 0.
View Article and Find Full Text PDFEnviron Microbiol
August 2025
Department of Microbiology, Radboud Institute for Biological and Environmental Sciences, Faculty of Science, Radboud University, Nijmegen, the Netherlands.
Hydrogen (H) and methane (CH) are produced in the anoxic layers of wetlands and sediments. In the overlaying oxygenated surface layers, these gases become available for oxidation by aerobic hydrogenotrophic and methanotrophic microorganisms. While H oxidation by verrucomicrobial methane-oxidising bacteria (MOB) is extensively studied, less is known about this metabolism in MOB from the class Alphaproteobacteria, which frequently inhabit wetlands.
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