Multiple paleoclimate, paleovegetation and paleoenvironmental records from Jaraguá cave, located at center of South America. In this dataset that covers the last 28,000 year is included δ13C and δ18O values and 87Sr/86Sr ratios in stalagmites combined with XRF-derived elemental chemistry, δ13Corg, total organic carbon and total inorganic carbon (carbonate) in a sedimentary profile from the same cave.

Supplement to: Novello, Valdir Felipe; da Cruz Junior, Francisco William; McGlue, Michael M; Wong, Corinne I; Ward, Brittany Marie; Vuille, Mathias; Santos, Rudney A; Jaqueto, Plinio; Pessenda, Luiz C R; Atorre, Tiago; Ribeiro, Ligia M A L; Karmann, Ivo; Barreto, Eline S; Cheng, Hai; Edwards, R Lawrence; Paula, Marcos S; Scholz, Denis (2019): Vegetation and environmental changes in tropical South America from the last glacial to the Holocene documented by multiple cave sediment proxies. Earth and Planetary Science Letters, 524, 115717