Methane hydrates stored in cold seeps are an important source of energy and carbon for both the endemic chemosynthetic community and humanity. However, the methane fluids may cease and even stop naturally or anthropogenically, calling for a thorough evaluation of its potential impact on the endemic species and local chemosynthetic ecosystems. As one dominant megafauna in cold seeps, some of the deep-sea mussels rely on methanotrophic endosymbionts for nutrition and therefore could serve as a promising model in monitoring the dynamic changes of methane hydrate. However, knowledge on the long-term responses of deep-sea mussels to environmental stresses induced by methane reduction and deprivation, is still lacking. Here, we set up a laboratory system and cultivated methanotrophic deep-sea mussel Gigantidas platifrons without methane supply to survey the phenotypic changes after methane deprivation. While the mussels managed to survive for >10 months after the methane deprivation, drastic changes in the metabolism, function, and development of gill tissue, and in the association with methanotrophic symbionts were observed. In detail, the mussel digested all methanotrophic endosymbionts shortly after methane deprivation for nutrition and remodeled the global metabolism of gill to conserve energy. As the methane deprivation continued, the mussel replaced its bacteriocytes with ciliated cells to support filter-feeding, which is an atavistic trait in non-symbiotic mussels. During the long-term methane deprivation assay, the mussel also retained the generation of new cells to support the phenotypic changes of gill and even promoted the activity after being transplanted back to deep-sea, showing the potential resilience after long-term methane deprivation. Evidences further highlighted the participation of symbiont sterol metabolism in regulating these processes. These results collectively show the phenotypic plasticity of deep-sea mussels and their dynamic responses to methane deprivation, providing essential information in assessing the long-term influence of methane hydrate extinction.
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http://dx.doi.org/10.1016/j.scitotenv.2024.178048 | DOI Listing |
Sci Total Environ
December 2024
Center of Deep Sea Research, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China; Laoshan Laboratory, Qingdao 266071, China. Electronic address:
Methane hydrates stored in cold seeps are an important source of energy and carbon for both the endemic chemosynthetic community and humanity. However, the methane fluids may cease and even stop naturally or anthropogenically, calling for a thorough evaluation of its potential impact on the endemic species and local chemosynthetic ecosystems. As one dominant megafauna in cold seeps, some of the deep-sea mussels rely on methanotrophic endosymbionts for nutrition and therefore could serve as a promising model in monitoring the dynamic changes of methane hydrate.
View Article and Find Full Text PDFMethane mitigation is regarded as a critical strategy to combat the scale of global warming. Currently, about 40% of methane emissions originate from microbial sources, which is causing strategies to suppress methanogens, either through direct toxic effects or by diverting their substrates and energy, to gain traction. Problematically, current microbial methane mitigation knowledge derives from rumen studies and lacks detailed microbiome-centered insights, limiting translation across ecosystems.
View Article and Find Full Text PDFBioresour Technol
December 2024
University of Gdańsk, Department of Oceanography and Geography al. Marszałka Piłsudskiego 46, 81-378 Gdynia, Poland.
ISME J
January 2024
Department of Civil and Environmental Engineering, University of Tennessee, Knoxville, TN 37996, United States.
Isolate studies have been a cornerstone for unraveling metabolic pathways and phenotypical (functional) features. Biogeochemical processes in natural and engineered ecosystems are generally performed by more than a single microbe and often rely on mutualistic interactions. We demonstrate the rational bottom-up design of synthetic, interdependent co-cultures to achieve concomitant utilization of chlorinated methanes as electron donors and organohalogens as electron acceptors.
View Article and Find Full Text PDFChemosphere
May 2024
Institute of Sustainable Processes, Valladolid University, Dr. Mergelina s/n, Spain; Department of Chemical Engineering and Environmental Technology, Valladolid University, Prado de la Magdalena 5, Valladolid, Spain. Electronic address:
Climate change and plastic pollution are likely the most relevant challenges for the environment in the 21st century. Developing cost-effective technologies for the bioconversion of methane (CH) into polyhydroxyalkanoates (PHAs) could simultaneously mitigate CH emissions and boost the commercialization of biodegradable polymers. Despite the fact that the role of temperature, nitrogen deprivation, CH:O ratio or micronutrients availability on the PHA accumulation capacity of methanotrophs has been carefully explored, there is still a need for optimization of the CH-to-PHA bioconversion process prior to becoming a feasible platform in future biorefineries.
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