Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2

The Cenomanian–Turonian Oceanic Anoxic Event (OAE2; ~94.5 million years ago) represents an episode of global-scale marine anoxia and biotic turnover, which corresponds to one of the warmest time intervals in the Phanerozoic. Despite its global significance, information on continental ecosystem respo...

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Detalles Bibliográficos
Autores principales: Heimhofer, Ulrich, Wucherpfennig, Nina, Adatte, Thierry, Schouten, Stefan, Schneebeli-Hermann, Elke, Gardin, Silvia, Keller, Gerta, Kentsch, Sarah, Kujau, Ariane
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6148089/
https://www.ncbi.nlm.nih.gov/pubmed/30237441
http://dx.doi.org/10.1038/s41467-018-06319-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6148089/
https://www.ncbi.nlm.nih.gov/pubmed/30237441
http://dx.doi.org/10.1038/s41467-018-06319-6

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