Lake Tauca highstand (Heinrich Stadial 1a) driven by a southward shift of the Bolivian High

Heinrich events are characterized by worldwide climate modifications. Over the Altiplano endorheic basin (high tropical Andes), the second half of Heinrich Stadial 1 (HS1a) was coeval with the highstand of the giant paleolake Tauca. However, the atmospheric mechanisms underlying this wet event are s...

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Detalles Bibliográficos
Autores principales: Martin, Léo C. P., Blard, Pierre-Henri, Lavé, Jérôme, Condom, Thomas, Prémaillon, Mélody, Jomelli, Vincent, Brunstein, Daniel, Lupker, Maarten, Charreau, Julien, Mariotti, Véronique, Tibari, Bouchaïb, Davy, Emmanuel
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2018
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6114991/
https://www.ncbi.nlm.nih.gov/pubmed/30167458
http://dx.doi.org/10.1126/sciadv.aar2514

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6114991/
https://www.ncbi.nlm.nih.gov/pubmed/30167458
http://dx.doi.org/10.1126/sciadv.aar2514

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