A stronger role for long-term moisture change than for CO2in determining tropical woody vegetation change

Author:

Gosling William D.1ORCID,Miller Charlotte S.2,Shanahan Timothy M.3ORCID,Holden Philip B.4ORCID,Overpeck Jonathan T.5ORCID,van Langevelde Frank67ORCID

Affiliation:

1. Institute for Biodiversity & Ecosystem Dynamics, University of Amsterdam, Netherlands.

2. Leeds Trinity University,Leeds, UK.

3. Department of Geological Sciences, University of Texas at Austin, Austin, TX, USA.

4. School of Environment, Earth & Ecosystem Sciences, The Open University, Milton Keynes, UK.

5. School for Environment & Sustainability, University of Michigan, Ann Arbor, MI, USA.

6. Department of Environmental Sciences, Wageningen University & Research, Wageningen, Netherlands.

7. School of Life Sciences, University of KwaZulu-Natal, KwaZulu-Natal, South Africa.

Abstract

Anthropogenically elevated CO2(eCO2) concentrations have been suggested to increase woody cover within tropical ecosystems through fertilization. The effect of eCO2is built into Earth system models, although testing the relationship over long periods remains challenging. Here, we explore the relative importance of six drivers of vegetation change in western Africa over the past ~500,000 years (moisture availability, fire activity, mammalian herbivore density, temperature, temperature seasonality, CO2) by coupling past environmental change data from Lake Bosumtwi (Ghana) with global data. We found that moisture availability and fire activity were the most important factors in determining woody cover, whereas the effect of CO2was small. Our findings suggest that the role of eCO2effects on tropical vegetation in predictive models must be reconsidered.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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