Changes to Yucatán Peninsula precipitation associated with salinity and temperature extremes of the Caribbean Sea during the Maya civilization collapse

Explanations of the Classic Maya civilization demise on the Yucatán Peninsula during the Terminal Classic Period (TCP; ~CE 750–1050) are controversial. Multiyear droughts are one likely cause, but the role of the Caribbean Sea, the dominant moisture source for Mesoamerica, remains largely unknown. H...

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Detalles Bibliográficos
Autores principales: Wu, Henry C., Felis, Thomas, Scholz, Denis, Giry, Cyril, Kölling, Martin, Jochum, Klaus P., Scheffers, Sander R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5696513/
https://www.ncbi.nlm.nih.gov/pubmed/29158534
http://dx.doi.org/10.1038/s41598-017-15942-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5696513/
https://www.ncbi.nlm.nih.gov/pubmed/29158534
http://dx.doi.org/10.1038/s41598-017-15942-0

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