In deep-sea benthic ecosystems, chemotrophic organisms derive energy from inorganic chemical reactions rather than sunlight. While hydrothermal vent fauna predominantly rely on thiotrophic (sulfur-oxidizing) endosymbionts fueled by hydrogen sulfide emitted from volcanic fissures, organisms inhabiting cold seeps often exploit both thiotrophic and methanotrophic (methane-oxidizing) bacteria. Methanotrophy requires molecular oxygen to convert methane into organic carbon. Consequently, while sulfur oxidation can persist across broader micro-aerobic gradients in anoxic sediments, seep organisms harboring obligate methanotrophs are strictly restricted to benthic zones where oxygenated bottom water directly interfaces with ascending methane plumes. Furthermore, dual-symbiont seep mussels (Bathymodiolinae) modulate the relative biomass of their sulfur- and methane-oxidizing bacterial populations in response to fluctuating localized chemical concentrations, a physiological plasticity entirely absent in vent taxa specialized exclusively in mono-symbiotic sulfur oxidation.
Based on the passage, which of the following statements are logically supported by the text? (Select all that apply)
- Organisms relying exclusively on methanotrophic endosymbionts cannot survive in deep-sea benthic microenvironments that lack dissolved molecular oxygen.Answer
- A localized decrease in ambient methane concentration relative to hydrogen sulfide would induce Bathymodiolinae mussels to adjust their internal symbiont ratio in favor of sulfur-oxidizing bacteria.Answer
- CMono-symbiotic hydrothermal vent organisms possess greater overall metabolic flexibility in response to shifting geochemical ratios than dual-symbiont cold seep mussels.
- DMethane emissions at deep-sea cold seeps remain chemically stable for substantially longer geological durations than volcanic vents.
- ESulfur oxidation generates significantly less organic carbon per unit of substrate consumed than methanotrophic metabolic pathways.