Contrary to other current estimates for recent decades, our results showedthat Mexico was a C sink over the period 1990–2009 (+31 TgC yr−1) andthat C accumulation over the last century amounted to 1210 ± 1040 TgC.We attributed this sink to the CO2 fertilization effect on GPP, whichled to an increase of 3408 ± 1060 TgC, while both climate and land usereduced the country C stocks by −458 ± 1001 and −1740 ± 878 TgC,respectively. Under different future scenarios, the C sink will likelycontinue over the 21st century, with decreasing C uptake as the climateforcing becomes more extreme. Our work provides valuable insights onrelevant driving processes of the C cycle such as the role of drought indrylands (e.g., grasslands and shrublands) and the impact of climate changeon the mean residence time of soil C in tropical ecosystems.