In contrast to magmatically driven black-smoker hydrothermal vents, which rely on intense volcanic heat to circulate highly acidic, mineral-rich fluids, alkaline hydrothermal vents—such as those found at the Lost City field—are powered by serpentinization. This exothermic geochemical reaction occurs when seawater percolates into mantle peridotite rock, oxidizing iron and hydrating olivine minerals into serpentine. Because serpentinization produces vast quantities of molecular hydrogen () and methane in a strongly alkaline environment ( 9–11) at moderate temperatures (40°C–90°C), it establishes steep electrochemical and proton gradients across porous, carbonate-mineral chimneys when the effluent meets cooler, slightly acidic ambient ocean water. Consequently, several geochemists hypothesize that such alkaline vent networks served as natural inorganic incubators for prebiotic metabolic pathways prior to the evolution of cellular membranes, since the microporous inorganic cavities could have concentrated catalytic iron-nickel sulfides while sustaining a continuous flow of chemical energy without requiring sunlight or volcanic activity.
Which of the following inferences regarding alkaline hydrothermal vents is most strongly supported by the passage?
- AMagmatically driven black-smoker vents produce steeper electrochemical gradients across their structures than alkaline vent systems do.
- BSerpentinization reactions require ongoing thermal energy from active volcanic magma chambers to sustain geochemical activity.
- The generation of proton gradients across the vent chimneys depends on a difference in acidity between the hydrothermal fluid and the surrounding seawater.Answer
- DSubmarine hydrothermal vents are the only geological settings on early Earth where prebiotic metabolic reactions could have emerged.
- EThe microporous cavities within the carbonate chimneys were formed through the metabolic processes of early cellular life.