To define a unit of geological time, scientists study the chemical makeup of rocks and the fossils they contain. That allows researchers to date the rocks and understand the conditions on Earth during their formation. “Every kind of rock is a record of an event from the past,” explains Stan Finney, a geologist involved in approving geological units of time for the International Union of Geological Sciences.
In the case of the new Meghalayan age, researchers analyzed a rock formation called a stalagmite growing on the ground of a cave in the northeastern state of Meghalaya, India. They found oxygen (O) isotopes, or different types of an element, that indicated the rock formed during a period of long drought. Geologists around the globe eventually made the same observations within rock and ice samples from all seven continents. That confirmed the initial findings, providing proof of the new age.