Late Quaternary millennial-scale stability of the feeding strategy of the gray brocket deer in Southeastern Brazil.

There is limited evidence, both contemporary and archaeological/paleontological, regarding the feeding ecology of the gray brocket deer (Subulo gouazoubira) in Brazils Cerrado biome. Using stable carbon ({delta}13C) and oxygen ({delta}18O) isotope analyses of dental enamel bioapatite from individuals recovered from Cuvieri Cave, Minas Gerais, we explore dietary and environmental changes between the Late Pleistocene and Holocene epochs in this biome. The average Pleistocene {delta}13C was -10.9{+/-}1.7{per thousand} and {delta}18Odw was -7.9{+/-}0.4{per thousand}, while Holocene individuals averaged a {delta}13C of -10.5{+/-}1.2{per thousand} and {delta}18Odw of -5.8{+/-}0.9{per thousand}. The {delta}13C data suggest no significant shift in feeding strategy between the Late Pleistocene and Holocene, with both sets of individuals displaying {delta}13C values consistent with browsing in environments other than closed canopy forests. However, {delta}18Odw values indicate an approximate temperature increase of 3.5{degrees}C between the two epochs and/or a reduction in precipitation. This study highlights the stability in the feeding behavior of the gray brocket deer despite biotic and abiotic changes between the epochs.