The Open UniversitySkip to content
 

Palynological signal of the Younger Dryas in the tropical Venezuelan Andes

Rull, Valentí; Stansell, Nathan D.; Montoya, Encarni; Bezada, Maximiliano and Abbott, Mark B. (2010). Palynological signal of the Younger Dryas in the tropical Venezuelan Andes. Quaternary Science Reviews, 29(23-24) pp. 3045–3056.

DOI (Digital Object Identifier) Link: https://doi.org/10.1016/j.quascirev.2010.07.012
Google Scholar: Look up in Google Scholar

Abstract

The occurrence, or not, of the Younger Dryas cold reversal in the tropical Andes remains a controversial topic. This study reports a clear signal for this event in the Venezuelan Andes, employing high-resolution palynological analysis of a well-dated sediment core from Laguna de Los Anteojos, situated around 3900 m elevation, within grass páramo vegetation. The lake is surrounded by some Polylepis forests which are close to their upper distribution limit. The section of the core discussed here is 150-cm long and dated between about 14.68 and 9.35 cal kyr BP, using a polynomial age-depth model based on six AMS radiocarbon dates. Between 12.86 and 11.65 cal kyr BP, an abrupt shift occurred in the pollen assemblage, manifested by a decline of Podocarpus, Polylepis and Huperzia, combined with an increase in Poaceae and Asteraceae. The aquatic pteridophyte Isoëtes also decreased and disappeard, and the algae remains show their minimum values. Pollen assemblages from the Younger Dryas interval show maximum dissimilarity values compared with today’s pollen assemblage, and are more similar to modern analogs from superpáramo vegetation, growing at elevations 400–500 m higher. A lowering of vegetation zones of this magnitude corresponds to a temperature decline of between 2.5 and 3.8 °C. During this colder interval lake levels may have been lower, suggesting a decrease in available moisture. The vegetation shift documented in Anteojos record between 12.86 and 11.65 cal kyr BP is comparable to the El Abra Stadial in the Colombian Andes but it differs in magnitude. The Anteojos shift is better dated and coincides with the Younger Dryas chron as recorded in the Cariaco Basin sea surface temperature reconstructions and records of continental runoff, as well as in the oxygen isotope measurements from the Greenland ice cores. When compared to other proxies of quasi-immediate response to climate, the time lag for the response of vegetation to climate is found to be negligible at a centennial scale. The Polylepis pollen curve is especially noteworthy, as it reproduces the overall pollen trends and matches well with paleoclimatic reconstructions based on other proxies. Hence, Polylepis might be used as a reliable paleoclimatic indicator in lake sediments close to its uppermost distribution boundary.

Item Type: Journal Item
Copyright Holders: 2010 Elsevier Ltd.
ISSN: 0277-3791
Academic Unit/School: Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
Item ID: 35713
Depositing User: Encarnacion Montoya Romo
Date Deposited: 10 Dec 2012 09:44
Last Modified: 07 Dec 2018 10:11
URI: http://oro.open.ac.uk/id/eprint/35713
Share this page:

Metrics

Altmetrics from Altmetric

Citations from Dimensions

Actions (login may be required)

Policies | Disclaimer

© The Open University   contact the OU