δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 (2017)
Source: Climate of the Past. Unidade: EACH
Subjects: PALEOCLIMATOLOGIA, PALEOCEANOGRAFIA, CIRCULAÇÃO OCEÂNICA, CARBONO 14, MUDANÇA CLIMÁTICA
ABNT
CAMPOS, Marília de Carvalho et al. δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2. Climate of the Past, v. 13, p. 345-358, 2017Tradução . . Disponível em: https://doi.org/10.5194/cp-13-345-2017. Acesso em: 08 set. 2024.APA
Campos, M. de C., Chiessi, C. M., Voigt, I., Piola, A. R., Kuhnert, H., & Mulitza, S. (2017). δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2. Climate of the Past, 13, 345-358. doi:10.5194/cp-13-345-2017NLM
Campos M de C, Chiessi CM, Voigt I, Piola AR, Kuhnert H, Mulitza S. δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 [Internet]. Climate of the Past. 2017 ; 13 345-358.[citado 2024 set. 08 ] Available from: https://doi.org/10.5194/cp-13-345-2017Vancouver
Campos M de C, Chiessi CM, Voigt I, Piola AR, Kuhnert H, Mulitza S. δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2 [Internet]. Climate of the Past. 2017 ; 13 345-358.[citado 2024 set. 08 ] Available from: https://doi.org/10.5194/cp-13-345-2017