High resolution X-ray Fluorescence (XRF) is presented as a robust palaeoclimatic proxy
XRF identifies wet and dry shifts in a complex sedimentary sequence extracted from a volcanic crater in NE Australia
XRF record correlates well with magnetic susceptibility, humification, grainsize, macrocharcoal, δ13C, C/N and pollen
Abrupt climate events recorded at 32,690, 30,080, 24,660, 21,870, 11,880, 10,020, 9170 and 5120 cal. yr BP