The analysis of fossilized leaves of the deciduous tree *Ginkgo biloba* from the Cretaceous-Paleogene transition reveals a sharp decrease in stomatal density—the number of pores per unit of leaf area. Because modern *Ginkgo* trees respond to elevated atmospheric carbon dioxide () concentrations by reducing their stomatal density to conserve water, some researchers conclude that global levels rose significantly during this period. However, skeptics suggest that this reduction was merely a localized adaptation to regional soil moisture levels in the specific basins where the fossils were deposited. This skeptical view is undermined, however, by the discovery of fossilized *Ginkgo* leaves from geographically isolated regions of the same era that also show uniform stomatal reduction, which suggests that
Which choice most logically completes the text?
- the stomatal changes were likely a response to a widespread atmospheric shift rather than localized soil factors.Answer
- Bdeciduous trees in the Cretaceous-Paleogene period were more resilient to changes in soil moisture than modern trees are.
- Celevated atmospheric carbon dioxide levels actually increased soil moisture in the geographically isolated regions.
- Dthe local soil moisture levels of the different depositional basins were identical during this transition period.