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: Nature Communications
- Volume/Número/Paginação/Ano: v. 13, n. 1, 2022. Article n. 239
- Este periódico é de acesso aberto
- Este artigo NÃO é de acesso aberto
-
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: 13 fev. 2026. -
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 2026 fev. 13 ] 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 2026 fev. 13 ] 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)
- Middle Eocene to Early Oligocene climate: preliminary magnetobiostratigraphic from Monte Cagnero section, central Italy
- High-resolution magneto-biostratigraphy of the early Eocene to early Oligocene from Indian Hole 711A and Italian Monte Cagnero section
- Enhanced primary productivity and magnetotactic bacterial production in response to middle Eocene warming in the Neo-Tethys Ocean
- Long-term Aptian marine osmium isotopic record of Ontong Java Nui activity
- Middle Eocene Climatic Optimum (MECO) in the Monte Cagnero section, Central Italy
- The Barremian-Aptian boundary in the Poggio le Guaine core (central Italy): evidence for magnetic polarity Chron M0r and oceanic anoxic event 1a
- Impact of the middle eocene climatic optimum (MECO) on foraminiferal and calcareous nannofossil assemblages in the neo-Tethyan Baskil section (Eastern Turkey): Paleoenvironmental and paleoclimatic reconstructions
- Oceanographic exchanges between the Southern and Northern Atlantic during the Cenozoic inferred from mixed contourite-turbidite systems in the Brazilian Equatorial Margin
- Multistratigraphic records of the Lower Cretaceous (Valanginian–Cenomanian) Puez key area in N. Italy
Informações sobre o DOI: 10.1038/s41467-021-27817-0 (Fonte: oaDOI API)
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