Evidence for global cooling in the Late Cretaceous

The Late Cretaceous ‘greenhouse’ world witnessed a transition from one of the warmest climates of the past 140 million years to cooler conditions, yet still without significant continental ice. Low-latitude sea surface temperature (SST) records are a vital piece of evidence required to unravel the c...

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Detalles Bibliográficos
Autores principales: Linnert, Christian, Robinson, Stuart A., Lees, Jackie A., Bown, Paul R., Pérez-Rodríguez, Irene, Petrizzo, Maria Rose, Falzoni, Francesca, Littler, Kate, Arz, José Antonio, Russell, Ernest E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4082635/
https://www.ncbi.nlm.nih.gov/pubmed/24937202
http://dx.doi.org/10.1038/ncomms5194

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4082635/
https://www.ncbi.nlm.nih.gov/pubmed/24937202
http://dx.doi.org/10.1038/ncomms5194

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