Cargando…
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...
| Autores principales: | , , , , , , , , , , , |
|---|---|
| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2018
|
| Materias: | |
| 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 |