Publikace na Přírodovědecká fakulta, 1. lékařská fakulta, Matematicko-fyzikální fakulta |
2015
Abstrakt
The Arctic is one of the fastest changing regions of the Earth and environmental changes are of great magnitude (Miller et al., 2010). Our aim is to investigate the lacustrine sediments that are natural archives of past changes, among which we are interested mainly in the evolution of the climate, the lake basin and the lake itself including its biota.
For this purpose, three sediment cores were retrieved from the high-altitude lake Garmaksla, located in the northern Billefjorden, Svalbard archipelago. A multi-proxy approach was applied to study deposited material.