“…A short-lived 14 C sample formed in AD 775, such as a leaf or seed, could appear to date to the early tenth century if its 14 C age is calibrated using the international consensus calibration curve for the Northern Hemisphere [11]. On the other hand, the 14 C peak means that wood samples spanning the AD 770s can be wiggle-matched precisely: for example, Wacker et al [12] used a series of 7 14 C samples from single annual rings in a conifer timber from Holy Cross chapel, St John's convent (Müstair, Switzerland) to confirm a tentative dendrochronological felling date of winter AD 785/6 for this timber.…”