Bernal, Juan PabloLachniet, MatthewMcCulloch, MalcolmMortimer, GrahamMorales, PedroCienfuegos, Edith2015-12-100033-5894http://hdl.handle.net/1885/57254A paleoclimate reconstruction for the Holocene based upon variations of δ18O in a U-Th dated stalagmite from southwestern Mexico is presented. Our results indicate that the arrival of moisture to the area has been strongly linked to the input of glacialKeywords: Holocene climate variability; ITCZ. ENSO; Me-xico; Oxygen isotopes; Stalagmite; Isotopes; Moisture; Oxygen; Climatology; atmospheric moisture; climate variation; El Nino-Southern Oscillation; geological record; Holocene; intertropical convergence zone; ox Holocene climate variability; ITCZ. ENSO; Mexico; Oxygen isotopes; Stalagmite201110.1016/j.yqres.2010.09.0022016-02-24