Rapid human-induced landscape transformation in Madagascar at the end of the first millennium of the Common Era

Abstract The environmental impact of the early human inhabitants of Madagascar remains heavily debated. We present results from a study using two stalagmitescollected from Anjohibe Cave in northwestern Madagascar to investigate the paleoecologyand paleoclimate of northwestern Madagascar over the past 1800 years. Carbon stable isotopic data indicate a rapid, complete transformation from a flora dominated by C 3 plants to a C 4 grassland system. This transformation is well replicated in both stalagmites, occurred at 890 CE and was completed within one century. We infer that the change was the result of a dramatic increase in the use of fire to promote the growth of grass for cattle fodder. Further, stalagmiteoxygen isotope ratios show no significant variation across the carbon isotope excursion, demonstrating that the landscape transformation was not related to changes in precipitation. Our study illustrates the profound impact early inhabitants had on the environment, and implies that forest loss was one trigger of megafaunal extinction.