“…Southerly migration of the mean position of the Atlantic ITCZ is controlled by different forcing mechanisms, such as i) reduction of the Atlantic Meridional Overturning Circulation (AMOC), which decreases the cross-equatorial heat flux from the South to North Atlantic and strengthens the northeast trade winds (Timmermann et al, 2005; Cheng et al, 2007), ii) decreasing latitudinal gradients of the sea surface temperature (SST), associated with cooling of SST in the North Atlantic (Chiang and Bitz, 2005;Peterson and Haug, 2006), iii) increasing intensity of the annual cycle in the southern hemisphere tropics, associated with the ∼21,000-year precessional component of Milankovitch forcing (Hodell et al, 1991;Haug et al, 2001), iv) increasing land-sea ice cover in the Northern Hemisphere (Chiang and Bitz, 2005), v) weakening of the Caribbean Low-Level Jet (CLLJ) (Mestas-Nunez et al, 2007), vi) increased ENSO-variability in the tropical Pacific (Haug et al, 2001), vii) weakening of the Walker circulation (Stott et al, 2002), and/or viii) changes in the seasonal distribution of the North Atlantic Oscillation (NAO) (Giannini et al, 2001). Regardless of the forcing mechanisms that dominated and ultimately caused the inferred climate shifts, we note that the drying trend registered in the Petén, and more broadly in equatorial regions of the Northern Hemisphere, parallels an increased commitment to maize-based food production and the emergence of hierarchically organized societies on the Pacific and Gulf Coasts of Mexico (Clark and Blake 1994;Pope et al 2001;Kennett et al, 2007) that later influenced similar cultural developments in the Maya lowlands (Rice, 1976;Rice and Rice, 1990;Neff et al 2006). …”