Item talk:Q255753
From geokb
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"abstract": "Chemosynthetic environments support distinct\u00a0benthic communities\u00a0capable of utilizing reduced chemical compounds for nutrition. Hundreds of\u00a0methane\u00a0seeps have been documented along the U.S. Atlantic margin (USAM), and detailed investigations at a few seeps have revealed distinct environments containing\u00a0mussels,\u00a0microbial mats, authigenic carbonates, and soft\u00a0sediments. The dominant mussel,\u00a0Bathymodiolus childressi, contains methanotrophic\u00a0endosymbionts\u00a0but is also capable of\u00a0filter feeding, and\u00a0stable isotope\u00a0analysis (SIA) of mussel-shell periostracum suggests that these mussels are mixotrophic, assimilating multiple food resources. However, it is unknown whether\u00a0mixotrophy\u00a0is widespread or varies spatially and temporally. We used SIA (\u03b413C, \u03b415N, and \u03b434S) and an\u00a0isotope\u00a0mixing model (MixSIAR) to estimate resource contribution to\u00a0B. childressi\u00a0and characterize\u00a0food webs\u00a0at two seep sites (Baltimore Seep; 400\u202fm and Norfolk Seep; 1500\u202fm depths) along the USAM, and applied a linear mixed-effects model to explore the role of mussel\u00a0population density\u00a0and tissue type in influencing SIA variance. After controlling for location and temporal variation, isotopic variability was a function of proportion of live mussels present and tissue type. Isotopic differences were also spatially discrete, possibly reflecting variations in the underlying carbon source at the two sites. Low mussel \u03b413C values (\u223c\u221263\u2030) are consistent with a dependence on microbial methane. However, MixSIAR results revealed mixotrophy for mussels at both sites, implying a reliance on a mixture of methane and phytoplankton-derived\u00a0particulate\u00a0organic material. The mixing model results also reveal population density-driven patterns, suggesting that resource use is a function of live mussel abundance. Mussel isotopes differed by tissue type, with\u00a0gill\u00a0having the lowest \u03b415N values relative to muscle and mantle tissues. Based on mass balance equations, up to 79% of the dissolved\u00a0inorganic carbon\u00a0(DIC) of the pore fluids within the anaerobic\u00a0oxidation\u00a0of the methane zone is derived from methane and available to fuel upper slope deep-sea communities, such as fishes (Dysommina rugosa\u00a0and\u00a0Symphurus nebulosus),\u00a0echinoderms\u00a0(Odontaster robustus,\u00a0Echinus\u00a0wallisi, and\u00a0Gracilechinus affinis), and shrimp, (Alvinocaris markensis). The presence of these seeps thereby increases the overall trophic and community diversity of the USAM\u00a0continental slope. Given the presence of hundreds of seeps within the\u00a0region,\u00a0primary production\u00a0at seeps may serve as an important, yet unquantified, energy source to the USAM deep-sea environment.",
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