Changes in palaeoclimate and palaeoenvironment in the Upper Yangtze area (South China) during the Ordovician–Silurian transition

The Ordovician–Silurian transition was a critical period in geological history, during which profound changes in climatic, biotic, and oceanic conditions occurred. To explore the provenance, palaeoclimate, and palaeoredox conditions in the Sichuan Basin during the Late Ordovician–early Silurian inte...

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Detalles Bibliográficos
Autores principales: Men, Xin, Mou, Chuanlong, Ge, Xiangying
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9343391/
https://www.ncbi.nlm.nih.gov/pubmed/35915216
http://dx.doi.org/10.1038/s41598-022-17105-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9343391/
https://www.ncbi.nlm.nih.gov/pubmed/35915216
http://dx.doi.org/10.1038/s41598-022-17105-2

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