Paleoecologists investigating the timing of late-Pleistocene megafaunal extinctions in North America have analyzed the stratigraphic distribution of *Sporormiella* fungal spores preserved in lake sediment cores. Because *Sporormiella* reproduces obligately in the dung of large herbivorous mammals, spore abundance serves as an indirect proxy for local megafaunal biomass. In several Appalachian sedimentary sequences, *Sporormiella* spore concentrations decline precipitously from high baseline values to near-zero levels between 14,800 and 13,700 calibrated radiocarbon years before present (cal BP). This spore decline predates the onset of the Younger Dryas climatic cooling event (~12,900 cal BP) by more than eight centuries. Furthermore, pollen records extracted from the same core strata reveal that major shifts in forest composition—specifically the proliferation of deciduous hardwood taxa at the expense of spruce-dominated woodlands—occurred only after the *Sporormiella* crash was already complete. Because the deposition rate of windborne pollen is not mechanically influenced by the presence or absence of herbivore dung, the temporal lag between the spore reduction and subsequent floral restructuring suggests that the megafaunal decline was not initially triggered by climate-induced vegetation turnover, but rather preceded the major ecological reorganization of the region.
Which of the following assertions are logically supported by the passage? (Select all that apply.)
- The reduction in megafaunal biomass in the Appalachian region examined did not occur simultaneously with the regional expansion of deciduous hardwood forests.Cevap
- BThe onset of the Younger Dryas cooling event was the primary driver of the initial decline in Appalachian *Sporormiella* spore concentrations.
- The mechanisms governing the deposition of windborne tree pollen in lake sediments operate independently of the presence of *Sporormiella* spores.Cevap
- DOverhunting by early human hunters was the exclusive catalyst for the reduction of large herbivore biomass documented in the Appalachian sediment cores.
- EDeciduous hardwood taxa were completely absent from the Appalachian region prior to the decline of *Sporormiella* spores.