“…Early incremental radiocarbon work in known-age tree-ring sequences revealed that the radiocarbon production in the atmosphere is not constant (Stuiver and Quay, 1981) and that calibration is required to compare radiocarbon dates and develop coherent chronological sequences. Tree-ringbased calibration first became available in the early 1960s (e.g., Satterthwaite and Ralph, 1960;Suess, 1967), but the coverage was spotty and internationally accepted curves were not available until the late 1980s (Vogel et al, 1986). Wider access to calibration via the Internet (e.g., OxCal: Bronk Ramsey, 1995, 2000, 2001, 2009aCALIB: Stuiver andReimer, 1986, 1993;Stuiver et al, 2005;BCal: Buck et al, 1996, 1999CalPal: Danzeglocke et al, 2007;Weninger et al, 2007) since the 1990s has made calibration routine, and international efforts to improve and extend the tree-ring calibration curve continue to this day (Reimer et al, 2013).…”