The Tooth Drawers
1On Saturdays, eighth grader Noa Feldstein volunteers in the collections room of a natural history museum, behind the public halls, where fossils are stored in rows of wooden drawers. Her project with the curator, Dr. Kwabena Ostrander, uses fossil horse teeth from rock layers in one region of the Great Plains. The layers formed one on top of another from about 24 million to 9 million years ago. The horses in them were related to today's horses, though most were much smaller.
2A horse grinds its food with its broad cheek teeth. Some fossil horses had low-crowned teeth, with a short crown. Others had high-crowned teeth, with a tall crown that sits mostly inside the jaw and slowly pushes up as its top wears away. The volunteers counted a tooth as high-crowned if its crown was more than twice as tall as it was wide. A crown's height is set while the tooth forms in a young horse. Chewing wears a crown down, but it cannot make the crown taller. In mammals, the size and shape of teeth are largely inherited from the parents.
3Grasses make tiny, hard bits of silica, a glassy mineral, inside their leaves. These bits, called phytoliths, last in rock for millions of years, so scientists count them to learn what plants grew in a place. Grasses also grow low to the ground, where wind-blown dust and grit settle on them. Scientists think the silica and the grit wear teeth down much faster than the soft leaves of shrubs and trees do. A horse whose teeth wear down to the roots can no longer chew well, and it may starve.
4Table 1 shows simplified data like the data scientists collect from layers like these. The grass share is the percent of all plant phytoliths in a layer that came from grasses. Some layers held more horse teeth than others, so the volunteers did not measure the same number of teeth in every layer.
5Horses usually begin to breed at about 3 years old, and a mare has at most one foal a year. Dr. Ostrander told Noa that a new generation of horses came along about every 8 years.