This document provides an overview of radiocarbon dating and discusses reporting standards. It explains that radiocarbon dating uses the radioactive isotope carbon-14 to determine the age of carbon-bearing materials by comparing the amount of carbon-14 remaining to the amount expected in a fresh sample. Key points include how samples are calibrated to convert determinations into calendar dates, the importance of reporting details like laboratory codes and pretreatment methods, and an example of how radiocarbon dates from a site in Ireland can be compared to other contemporary dates. It also describes an Irish radiocarbon dating project that compiles over 6,000 radiocarbon determinations to allow comparisons across different sites and regions.