Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events (2022)
Source: Nature Communications. Unidades: IO, IAG
Subjects: OCEANOGRAFIA, VULCANISMO, ISÓTOPOS ESTÁVEIS, HIDROTERMALISMO
ABNT
MATSUMOTO, Hironao; COCCIONI, Rodolfo; FRONTALINI, Fabrizio; et al. Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events. Nature Communications, London, v. 13, n. 2022. Article 239, 2022. Disponível em: < http://dx.doi.org/10.1038/s41467-021-27817-0 >.APA
Matsumoto, H., Coccioni, R., Frontalini, F., Shirai, K., Jovane, L., Trindade, R. I. F. da, et al. (2022). Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events. Nature Communications, 13( 2022. Article 239). Recuperado de http://dx.doi.org/10.1038/s41467-021-27817-0NLM
Matsumoto H, Coccioni R, Frontalini F, Shirai K, Jovane L, Trindade RIF da, Savian JF, Kuroda J. Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events [Internet]. Nature Communications. 2022 ; 13( 2022. Article 239):Available from: http://dx.doi.org/10.1038/s41467-021-27817-0Vancouver
Matsumoto H, Coccioni R, Frontalini F, Shirai K, Jovane L, Trindade RIF da, Savian JF, Kuroda J. Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events [Internet]. Nature Communications. 2022 ; 13( 2022. Article 239):Available from: http://dx.doi.org/10.1038/s41467-021-27817-0