Resumen
The last ca. 4100 cal yr BP of palaeoenviromental conditions in the Llanganates National Park, central Ecuadorian Andes, has been reconstructed from the pollen record 'Anteojos Valley' (3984 m elevation). The pollen record, dated with four radiocarbon dates, indicates that the local páramo vegetation was relatively stable with only minor fluctuations since the mid-Holocene. The páramo vegetation was characterised mainly by Asteraceae, Cyperaceae and Poaceae. The regional lower mountain rainforest vegetation is mainly represented by Moraceae/Urticaceae, and the upper mountain rainforest by Melastomataceae, Polylepis and Weinmannia. Between ca. 4100 to 2100 cal yr BP, páramo was the main vegetation type with a low presence of mountain rainforest, probably reflecting cool conditions. Between ca. 2100 cal yr BP and the present, the proportion of páramo vegetation increased with a decreased occurrence of mountain rainforest, suggesting cooler and moister conditions. Low frequencies of fires were evidenced since the mid-Holocene. However, there is a slight increase of regional fire between ca. 4100 and 3100 cal yr BP. The low abundance of larger carbonised particles since the beginning of the record suggests a low occurrence of local fire in the study area.
| Idioma original | Inglés |
|---|---|
| Páginas (desde-hasta) | 350-361 |
| Número de páginas | 12 |
| Publicación | Palynology |
| Volumen | 39 |
| N.º | 3 |
| DOI | |
| Estado | Publicada - 2 sept 2015 |
Nota bibliográfica
Publisher Copyright:© 2014 AASP - The Palynological Society.
Financiación
| Financiadores |
|---|
| Deutsche Forschungsgemeinschaft |
Citar esto
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver