Read the following passage snippet from a study on marine geochemistry:
"Although nineteenth-century geologists assumed that deep subseafloor basaltic crust was entirely devoid of metabolic activity, recent oceanographic drilling reveals that chemolithoautotrophic microbes thrive within subcrustal microfractures; notably, while these endolithic communities account for less than one percent of total marine biomass, their steady oxidation of ferrous iron within fluids sequestered from open ocean circulation buffers local seawater pH over millennial timescales—a stabilizing function previously attributed exclusively to the dissolution of surface carbonate sediments."
Which of the following inferences regarding surface carbonate sediment dissolution is most strictly supported by the passage?
- It was formerly believed by scientists to be the sole process responsible for stabilizing local ocean pH over periods spanning thousands of years.Cevap
- BIt is carried out by microbial populations that constitute less than one percent of total oceanic biomass.
- CIt has been proven to be entirely ineffective at regulating long-term seawater acidity compared to microbial iron oxidation.
- DIt takes place primarily within isolated subcrustal fluids that do not mix with open ocean circulation.
- EIt fails to maintain ocean pH because surface sediments are rapidly depleted by deep-sea microbial consumption.