𝔖 Bobbio Scriptorium
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Late Quaternary vegetation changes around Lake Rutundu, Mount Kenya, East Africa: evidence from grass cuticles, pollen and stable carbon isotopes

✍ Scribed by Dr M. J. Wooller; D. L. Swain; K. J. Ficken; A. D. Q. Agnew; F. A. Street-Perrott; G. Eglinton


Book ID
102419844
Publisher
John Wiley and Sons
Year
2003
Tongue
English
Weight
269 KB
Volume
18
Category
Article
ISSN
0267-8179

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✦ Synopsis


Abstract

Woody, subalpine shrubs and grasses currently surround Lake Rutundu, Mount Kenya. Multiple proxies, including carbon isotopes, pollen and grass cuticles, from a 755‐cm‐long core were used to reconstruct the vegetation over the past 38 300 calendar years. Stable carbon‐isotope ratios of total organic carbon and terrestrial biomarkers from the lake sediments imply that the proportion of terrestrial plants using the C~4~ photosynthetic pathway was greater during the Late Pleistocene than in the Holocene. Pollen data show that grasses were a major constituent of the vegetation throughout the Late Pleistocene and Holocene. The proportion of grass pollen relative to the pollen from other plants was greatest at the last glacial maximum (LGM). Grass cuticles confirm evidence that C~4~ grass taxa were present at the LGM and that the majority followed the cold‐tolerant NADP‐MEC~4~ subpathway. Copyright © 2003 John Wiley & Sons, Ltd.