Read the following passage:
Oceanic carbon sequestration relies heavily on the biological carbon pump, a process primarily mediated by the descent of organic detritus known as "marine snow." The formation of these sinking aggregates is initiated by the excretion of transparent exopolymeric particles (TEPs) by diatoms during the terminal phase of an algal bloom. These TEPs effectively glue smaller organic fragments together, significantly increasing their mass and sinking velocity. While early climate models posited that the physical fragmentation of these aggregates by ocean turbulence was the primary factor limiting downward carbon transport, recent microbial research has elucidated a different primary mechanism. According to these researchers, as the heavy aggregates descend through the mesopelagic zone, their colonization by heterotrophic bacteria results in the enzymatic hydrolysis of particulate organic carbon into dissolved organic carbon. The researchers conclude that it is precisely this bacterial enzymatic activity, rather than physical disruption, that diminishes the efficiency of deep-ocean carbon sequestration, because the resulting dissolved carbon is subsequently remineralized and circulated back to the ocean's surface by upwelling currents.
Based on the passage, the recent microbial researchers assert that the diminished efficiency of deep-ocean carbon sequestration is directly caused by which of the following?
- The enzymatic conversion of particulate organic carbon into dissolved organic carbon by colonizing bacteriaAnswer
- BThe physical fragmentation of descending organic aggregates driven by turbulence in the mesopelagic zone
- CThe excretion of transparent exopolymeric particles by diatoms during the terminal phase of algal blooms
- DThe circulation of remineralized carbon dioxide back to the ocean's surface via strong upwelling currents
- EThe complete consumption of all descending marine snow by heterotrophic bacteria prior to reaching the benthic floor