Permafrost in the Cretaceous supergreenhouse

Earth’s climate during the last 4.6 billion years has changed repeatedly between cold (icehouse) and warm (greenhouse) conditions. The hottest conditions (supergreenhouse) are widely assumed to have lacked an active cryosphere. Here we show that during the archetypal supergreenhouse Cretaceous Earth...

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Detalles Bibliográficos
Autores principales: Rodríguez-López, Juan Pedro, Wu, Chihua, Vishnivetskaya, Tatiana A., Murton, Julian B., Tang, Wenqiang, Ma, Chao
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/PMC9792593/
https://www.ncbi.nlm.nih.gov/pubmed/36572668
http://dx.doi.org/10.1038/s41467-022-35676-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9792593/
https://www.ncbi.nlm.nih.gov/pubmed/36572668
http://dx.doi.org/10.1038/s41467-022-35676-6

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