In evaluating marine sediment cores from the North Atlantic, paleoclimatologist Hélène Gautier analyzed the isotopic ratios of oxygen () in benthic foraminifera to reconstruct deep-sea temperature fluctuations during the Mid-Pleistocene Transition. Previous studies postulated that the transition from -year to -year glacial cycles was driven exclusively by changes in high-latitude insolation resulting from orbital obliquity. Gautier’s analysis, however, revealed that deep-water cooling preceded the expansion of continental ice sheets by approximately years. Furthermore, by cross-referencing trace element ratios of magnesium to calcium () in the calcite shells of *Cibicidoides wuellerstorfi*, she demonstrated that deep-ocean temperatures dropped by prior to any measurable increase in global ice volume, indicating that oceanic circulation changes functioned as an active driver rather than a passive response.
According to the passage, Gautier's analysis of benthic foraminifera revealed which of the following regarding the relationship between deep-ocean cooling and continental ice sheet expansion?
- A reduction in deep-ocean temperatures occurred prior to the expansion of continental ice masses.Cevap
- BContinental ice sheets expanded for approximately years before any measurable decline in deep-ocean temperatures took place.
- COrbital obliquity shifts directly induced a drop in deep-sea temperatures without influencing high-latitude insolation.
- DDeep-ocean temperature drops coincided exactly with measurable increases in global ice volume.
- EChanges in high-latitude insolation actively prevented deep-water cooling during the Mid-Pleistocene Transition.