Journal Article
Evidence for Holocene climate variability from the sediments of a Scottish remote mountain lake
Richard W. Battarbee; Nigel G. Cameron; Paul Golding; Stephen J. Brooks; Roy Switsur; Doug Harkness; Peter Appleby; Frank Oldfield; Roy Thompson; Don T. Monteith; Andrew McGovern
Journal of Quaternary Science · Vol. 16, Issue 4 · pp. 339-346 · 2001
Abstract
High resolution sampling of sediment cores covering approximately the last 4000 yr from Lochan Uaine, a small corrie loch in the Scottish Cairngorm Mountains, show quasi‐periodic cycles in organic matter (measured as percentage loss on ignition). Analysis of these cycles show correspondences between loss on ignition, δ 13 C values and chironomid head capsule abundance. We interpret the changes as reflecting changes in lake productivity and hypothesise that they are driven by climate variability. However, it is not yet clear whether the periods of relatively high organic matter production and preservation are associated with colder or with warmer conditions. Nevertheless the results indicate the value of using sediments from remote, undisturbed mountain lakes as recorders of Holocene climate variability. Copyright © 2001 John Wiley & Sons, Ltd.