Paleoecologist: Fossilized molars of late Pleistocene steppe bison reveal a pronounced decrease in microscopic enamel striations beginning roughly 20,000 years ago. Because abrasive silica phytoliths in steppe grasses cause heavy tooth wear, some researchers concluded that a severe drought forced the bison to alter their diet from rough grasses to softer shrubs. However, soil isotope samples from that period establish that grass abundance did not decline. Therefore, the decrease in striations was instead caused by deeper winter snowpack, which prevented the bison from grazing down to the soil-covered bases of the grass stems where gritty mineral dust accumulates.
Which of the following, if true, most strengthens the paleoecologist's argument?
- ADuring the late Pleistocene, winter snowpack in the steppe region formed a dense ice crust that frequently forced large herbivores to expend extra energy digging for forage.
- Contemporary bison grazing in areas with deep winter snowpack feed almost exclusively on the exposed upper blades of grasses and exhibit significantly less tooth enamel wear than bison grazing on the same grasses in snow-free areas.Cevap
- CNo herbivore species native to the Pleistocene steppe ever incorporated tundra shrubs into its diet during seasons when grass was readily accessible.
- DSoil isotope analysis provides far more precise measurements of prehistoric plant distribution than does microscopic analysis of fossilized tooth wear.
- ESteppe grasses from 20,000 years ago produced substantially higher concentrations of abrasive silica phytoliths than did grasses from earlier periods.