UNIVERSITY PARK, Pa. — Mysteries of the ancient world, buried deep in the earth or hidden in a silent tomb, can provide clues and context to history. However, for those mysteries to be fully understood, radiocarbon dating is often an essential step in the process. The researchers in Penn State’s Radiocarbon Laboratory, Brendan Culleton and Maggie Davis, provide those services to Penn State researchers. They also collaborate with researchers from around the world. Through these collaborations, they share best practices, their expertise and training to improve what can be a delicate science with no room for error.
Radiocarbon dating is the process of determining the age of things that once lived. The process is possible because during any living thing’s existence, it absorbs carbon. That includes a portion of carbon that is radioactive, called carbon-14. When the plant or animal dies, carbon is no longer absorbed. However, the carbon-14 inside the now-deceased fauna or flora continues its radioactive decay. Radiocarbon dating measures the amount of radioactive carbon remaining in the subject and provides an estimated date of when something died.