Ca. 8 m thick continuous sedimentary record of the Holocene. Pollen and fluorescence-X as proxies for temperature and humidity record at near-decadal to sub-annual timescale. Climate changes with millennial-down to decadal-scale variability. Cold Younger Dryas equivalent followed by Holocene thermal maximum. Interactions between Pacific (ENSO) and Atlantic (ITCZ) climate mechanisms.