The most significant climax vegetation in Uruguay is a type of grassla
nd commonly known as evergreen prairie. The evolution of the Uruguayan
prairie since the days of the first European settlements involved 3 m
ain stages: (1) 'hardening' as a result of the introduction of livesto
ck, (2) 'refinement' by the action of fire and overgrazing, and (3) fu
rther degradation, including preferential development of warm-season s
pecies, due to persistent overgrazing. Predicted climate changes (seas
onal decrease in water availability coupled with increase in both temp
erature and atmospheric CO2 concentration) are likely to favor, in the
short term, even further preferential development of warm-season spec
ies. Whether or not this trend will persist in the long term is diffic
ult to predict with confidence because of uncertainties regarding the
responses of the different prairie species to variation in atmospheric
CO2 concentration.