Until recently, marine biologists assumed that deep-sea hydrothermal vent communities relied exclusively on chemosynthetic bacteria utilizing hydrogen sulfide emitted directly from vent chimneys. However, recent sediment analysis near dormant vent fields revealed trace deposits of organic carbon isotope ratios that match those produced by methane-oxidizing archaea rather than sulfur-oxidizing bacteria. Because these isotopic signatures were found in sediment layers deposited thousands of years after vent fluid discharge had ceased, researchers hypothesize that microbial ecosystems can persist around extinct hydrothermal structures far longer than previously thought. The persistence of these communities depends not on active thermal plumes, but on the slow diffusion of trapped subsurface methane through porous volcanic rock. Consequently, estimates of total biological productivity in the abyssal zone may need to be revised upward, as non-eruptive vent sites cover vast expanses of the ocean floor previously regarded as biological deserts.
Which of the following can be inferred from the passage regarding non-eruptive hydrothermal vent sites?
- They are capable of sustaining specific microbial communities even after active fluid discharge from vent chimneys has stopped.Answer
- BThey produce greater total biological output per square meter than active hydrothermal vent fields.
- CThey rely primarily on sulfur-oxidizing bacteria that metabolize hydrogen sulfide plumes.
- DThey completely block subsurface methane from diffusing through surrounding porous volcanic rock.
- EThey were widely recognized as primary centers of deep-sea biological activity prior to recent sediment analyses.