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Stable isotope and modelling evidence for CO<sub>2</sub> as a driver of glacial–interglacial vegetation shifts in southern Africa

By F. J. Bragg, I. C. Prentice, S. P. Harrison, G. Eglinton, P. N. Foster, F. Rommerskirchen and J. Rullkötter

Abstract

Atmospheric CO<sub>2</sub> concentration is hypothesized to influence vegetation distribution via tree–grass competition, with higher CO<sub>2</sub> concentrations favouring trees. The stable carbon isotope (&delta;<sup>13</sup>C) signature of vegetation is influenced by the relative importance of C<sub>4</sub> plants (including most tropical grasses) and C<sub>3</sub> plants (including nearly all trees), and the degree of stomatal closure – a response to aridity – in C<sub>3</sub> plants. Compound-specific &delta;<sup>13</sup>C analyses of leaf-wax biomarkers in sediment cores of an offshore South Atlantic transect are used here as a record of vegetation changes in subequatorial Africa. These data suggest a large increase in C<sub>3</sub> relative to C<sub>4</sub> plant dominance after the Last Glacial Maximum. Using a process-based biogeography model that explicitly simulates <sup>13</sup>C discrimination, it is shown that precipitation and temperature changes cannot explain the observed shift in &delta;<sup>13</sup>C values. The physiological effect of increasing CO<sub>2</sub> concentration is decisive, altering the C<sub>3</sub>/C<sub>4</sub> balance and bringing the simulated and observed &delta;<sup>13</sup>C values into line. <br><br> It is concluded that CO<sub>2</sub> concentration itself was a key agent of vegetation change in tropical southern Africa during the last glacial–interglacial transition. Two additional inferences follow. First, long-term variations in terrestrial &delta;<sup>13</sup>Cvalues are not simply a proxy for regional rainfall, as has sometimes been assumed. Although precipitation and temperature changes have had major effects on vegetation in many regions of the world during the period between the Last Glacial Maximum and recent times, CO<sub>2</sub> effects must also be taken into account, especially when reconstructing changes in climate between glacial and interglacial states. Second, rising CO<sub>2</sub> concentration today is likely to be influencing tree–grass competition in a similar way, and thus contributing to the "woody thickening" observed in savannas worldwide. This second inference points to the importance of experiments to determine how vegetation composition in savannas is likely to be influenced by the continuing rise of CO<sub>2</sub> concentration

Topics: Geology, QE1-996.5, Science, Q, DOAJ:Earth Sciences, DOAJ:Earth and Environmental Sciences, Biology (General), QH301-705.5, DOAJ:Biology, DOAJ:Biology and Life Sciences, Ecology, QH540-549.5, Life, QH501-531
Publisher: Copernicus Publications
Year: 2013
DOI identifier: 10.5194/bg-10-2001-2013
OAI identifier: oai:doaj.org/article:1c344008e9a146d89ad336f15f354026
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