

The use of carbon isotopes ( (super 13) C, (super 14) C) in soil to evaluate vegetation changes during the Holocene in Central Brazil.
Keywords
central Brazil;Minas Gerais Brazil;Salitre Brazil;subtropical environment;changes;forests;climate;biogeography;Brazil;South America;vegetation;Holocene;soils;Cenozoic;charcoal;Quaternary;C 14;carbon;isotopes;radioactive isotopes;stable isotopes;C 13