“…The transitions are often characterized by an abruptness that can be explained by mechanisms such as climate-biosphere feedbacks functioning as strong amplifiers of basically moderate trends (Renssen et al, 2006;Castañeda et al, 2009). Apart from orbitally-forced variability, centennial-scale variations such as DansgaardeOeschger cycles, Heinrich events and the Younger Dryas (YD) have also influenced low-latitude climate, although the sign, magnitude and phasing of their impact are debated (Partridge et al, 2004;Brown et al, 2007;Carto et al, 2009;Chase et al, 2011;Stager et al, 2011). Furthermore, Atlantic and Indian Ocean SST changes, related to the thermohaline circulation, are considered to have a strong influence on African climate (Gasse and Van Campo, 1994;deMenocal et al, 2000;Trauth et al, 2010).…”