Authors
F Alayne Street-Perrott, Yongsong Huang, R Alan Perrott, Geoffrey Eglinton, Philip Barker, Leila Ben Khelifa, Douglas D Harkness, Daniel O Olago
Publication date
1997/11/21
Journal
Science
Volume
278
Issue
5342
Pages
1422-1426
Publisher
American Association for the Advancement of Science
Description
Carbon-isotope values of bulk organic matter from high-altitude lakes on Mount Kenya and Mount Elgon, East Africa, were 10 to 14 per mil higher during glacial times than they are today. Compound-specific isotope analyses of leaf waxes and algal biomarkers show that organisms possessing CO2-concentrating mechanisms, including C4 grasses and freshwater algae, were primarily responsible for this large increase. Carbon limitation due to lower ambient CO2 partial pressures had a significant impact on the distribution of forest on the tropical mountains, in addition to climate. Hence, tree line elevation should not be used to infer palaeotemperatures.
Total citations
Scholar articles
FA Street-Perrott, Y Huang, RA Perrott, G Eglinton… - Science, 1997
FAS Perrott, Y Huang, RA Perrott, G Eglinton, P Barker… - Science, 1997