a: Radiocarbon laboratory: KIA = Leibniz Laboratory in Kiel (Germany); NOSAMS = National Ocean Sciences Accelerator Mass Spectrometry Facility, Woods Hole Oceanographic Institution (USA); Poz = Poznań Radiocarbon Laboratory (Poland).b: Material: pF = planktonic foraminifers; bF = benthic foraminifers; bv = bivalves; gp = gastropods; co = coral pieces; os = ostracods.c: For reservoir correction, the conventional age of 405 years is applied using CALIB 6.1.1. (Reimer et al., 2009; Stuiver et al., 1998).d: The extrapolation of the calibrated 14C ages at 18 and 35 cm core depth results in an age close to 0 cal yr BP for the core top and allows assigning a modern age to the uppermost centimeters of the core sequence.e: Interpolated value between the 14C ages at 95 and 101 cm depth.f: Because of the lack of carbonate, the age model for GeoB6308-3 below 107 cm core depth was established based on stratigraphic correlation of the 7th degree polynomial fit of GeoB6308-3 Fe/K record to February insolation at 30°S (Laskar et al., 2004).