Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events (2022)
- Authors:
- USP affiliated authors: JOVANE, LUIGI - IO ; TRINDADE, RICARDO IVAN FERREIRA DA - IAG
- Unidades: IO; IAG
- DOI: 10.1038/s41467-021-27817-0
- Subjects: OCEANOGRAFIA; VULCANISMO; ISÓTOPOS ESTÁVEIS; HIDROTERMALISMO
- Language: Inglês
- Imprenta:
- Source:
- Título do periódico: Nature Communications
- Volume/Número/Paginação/Ano: v. 13, n. 1, 2022. Article n. 239
- Este periódico é de acesso aberto
- Este artigo é de acesso aberto
- URL de acesso aberto
- Cor do Acesso Aberto: gold
- Licença: cc-by
-
ABNT
MATSUMOTO, Hironao et al. Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events. Nature Communications, v. 13, n. 2022. Article 239, 2022Tradução . . Disponível em: https://doi.org/10.1038/s41467-021-27817-0. Acesso em: 28 abr. 2024. -
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). doi:10.1038/s41467-021-27817-0 -
NLM
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):[citado 2024 abr. 28 ] Available from: https://doi.org/10.1038/s41467-021-27817-0 -
Vancouver
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):[citado 2024 abr. 28 ] Available from: https://doi.org/10.1038/s41467-021-27817-0 - Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a)
- High-resolution magneto-biostratigraphy of the early Eocene to early Oligocene from Indian Hole 711A and Italian Monte Cagnero section
- Middle Eocene to Early Oligocene climate: preliminary magnetobiostratigraphic from Monte Cagnero section, central Italy
- Middle Eocene Climatic Optimum (MECO) in the Monte Cagnero section, Central Italy
- Enhanced primary productivity and magnetotactic bacterial production in response to middle Eocene warming in the Neo-Tethys Ocean
- The Barremian-Aptian boundary in the Poggio le Guaine core (central Italy): evidence for magnetic polarity Chron M0r and oceanic anoxic event 1a
- Long-term Aptian marine osmium isotopic record of Ontong Java Nui activity
- Mixed Carbonate–Siliciclastic Sedimentation Along the Great Barrier Reef Upper Slope: A Challenge To the Reciprocal Sedimentation Model
- The Romanche fracture zone influences the segmentation of the equatorial margin of Brazil
- Magnetic methods and the timing of geological processes
Informações sobre o DOI: 10.1038/s41467-021-27817-0 (Fonte: oaDOI API)
How to cite
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
