During the Mid-Pleistocene Transition (MPT), occurring approximately to million years ago, Earth's glacial-interglacial cycles shifted from a -year to a -year periodicity. Paleoceanographers long debated whether this transition was driven primarily by internal ice-sheet dynamics or by atmospheric carbon dioxide fluctuations. Recent reconstructions utilizing boron-to-calcium () ratios in fossilized shells of the benthic foraminifer *Epistominella exigua* have provided crucial empirical constraints on deep-ocean carbonate chemistry.
Boron incorporates into calcite shells predominantly as the charged borate ion, , whose concentration relative to bicarbonate is directly proportional to seawater and carbonate ion concentration (). By analyzing ratios isolated from North Atlantic sediment cores, researchers led by Dr. Elena Rostova established that deep-water experienced a marked drop of roughly during marine isotope stage 22 (MIS 22). Crucially, Rostova’s team noted that this drawdown of deep-ocean carbon storage preceded the expansion of continental ice sheets by nearly years.
Previous hypotheses by paleoclimatologist Marcus Thorne had posited that deep-water sequestration of carbon dioxide was merely a secondary consequence of reduced oceanic overturn caused by initial ice-sheet growth. However, Rostova's direct measurements of ratios demonstrate that deep-ocean reorganization and carbon storage preceded continental glaciation rather than following it. Moreover, while earlier proxies such as carbon isotope ratios () were frequently confounded by regional terrestrial vegetation shifts, the proxy depends strictly on the thermodynamic equilibrium of seawater borate, thereby isolating marine carbon dynamics from terrestrial biosphere noise.
According to the passage, Rostova's research team established which of the following regarding the drawdown of deep-ocean carbon storage during marine isotope stage 22?
- It occurred prior to the expansion of continental ice sheets rather than as a subsequent outcome of that expansion.Answer
- BIt was caused primarily by regional terrestrial vegetation shifts that altered seawater thermodynamic equilibrium.
- CIt triggered an immediate shift from a 100,000-year cycle to a 41,000-year cycle in glacial-interglacial periodicity.
- DIt occurred approximately 20,000 years after reduced oceanic overturn initiated initial continental glaciation.
- EIt proved conclusively that atmospheric carbon dioxide fluctuations were the sole driver of the Mid-Pleistocene Transition.