Abstract
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.
| Original language | English |
|---|---|
| Pages (from-to) | 350-361 |
| Number of pages | 12 |
| Journal | Palynology |
| Volume | 39 |
| Issue number | 3 |
| DOIs | |
| State | Published - 2 Sep 2015 |
Bibliographical note
Publisher Copyright:© 2014 AASP - The Palynological Society.
Funding
| Funders |
|---|
| Deutsche Forschungsgemeinschaft |
Keywords
- central Ecuadorian Andes
- mid-Holocene
- palaeoecology
- páramo
- vegetation dynamic