Question

Passage:
For decades, geobiologists attributed the deposition of Paleoproterozoic banded iron formations (BIFs)—massive sedimentary structures composed of alternating layers of iron oxides and chert—primarily to the biological activity of oxygenic photosynthetic cyanobacteria. According to the classical model, cyanobacteria generated free oxygen as a metabolic byproduct, which subsequently reacted with dissolved ferrous iron ($Fe^{2+}$) in shallow oceanic waters to precipitate insoluble ferric iron ($Fe^{3+}$) oxides. However, recent geochemical analyses of trace element distributions and chromium isotope fractionation have challenged this singular mechanism, suggesting that non-oxygenic photoferrotrophic bacteria played a far more substantial role than previously acknowledged. Photoferrotrophs utilize light energy to oxidize dissolved ferrous iron directly into ferric hydroxide without releasing free oxygen, operating efficiently under anoxic conditions. This alternative pathway explains how extensive BIF accumulation occurred prior to widespread atmospheric oxygenation. Furthermore, numerical modeling of ocean circulation patterns during the Paleoproterozoic indicates that deep-sea hydrothermal vents supplied a continuous flux of ferrous iron, while upwelling currents transported these ions into the photic zone where both bacterial communities flourished. Consequently, researchers now view BIF deposition not as a simple indicator of atmospheric oxygenation, but as a complex interplay between hydrothermal iron supply, microbial metabolic diversity, and dynamic oceanic circulation.

According to the passage, all of the following factors are identified as contributing to or explaining the deposition of banded iron formations EXCEPT: