Cargando…
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...
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: | |
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 |
Ejemplares similares
-
The Cenomanian/Turonian boundary in light of new developments in terrestrial palynology
por: Galasso, Francesca, et al.
Publicado: (2023) -
Rapid light carbon releases and increased aridity linked to Karoo–Ferrar magmatism during the early Toarcian oceanic anoxic event
por: Font, Eric, et al.
Publicado: (2022) -
Global ocean redox changes before and during the Toarcian Oceanic Anoxic Event
por: Kunert, Alexandra, et al.
Publicado: (2023) -
Global controls on phosphatization of fossils during the Toarcian Oceanic Anoxic Event
por: Sinha, Sinjini, et al.
Publicado: (2021) -
Secrets of warmth : for comfort or survival /
por: Weiss, Harold E.
Publicado: (1998)