Hawkins, H. orcid.org/0000-0001-9334-0669, Cramer, M.D. orcid.org/0000-0003-0989-3266, Simpson, K.J. orcid.org/0000-0001-6673-227X et al. (6 more authors) (2026) Savanna soil carbon accrual occurs through particulate organic matter from grass rather than tree biomass, regardless of atmospheric CO2 levels. Functional Ecology. ISSN: 0269-8463
Abstract
1. Afforestation schemes in savannas are increasingly promoted as a carbon storage strategy despite threats to biodiversity. We also lack a clear understanding of how trees and grasses differentially contribute to the major carbon store in savannas, that is, soil organic carbon (SOC) and its fractions. Because SOC fractions vary in their persistence, saturation potential, and vulnerability to loss, it is crucial to understand how shifts in tree cover and biomass will influence both the amount and stability of SOC, particularly under disturbance regimes and future climate scenarios such as rising atmospheric CO2.
2. Using an Open-Top Chamber system, we examined the responses of five C3 leguminous savanna tree species and the C4 grass species Themeda triandra to grass-tree competition under ambient (400 ppm) or elevated (550 ppm) atmospheric CO2. We hypothesised that SOC increases will mostly depend on plant biomass rather than plant life form; and that CO2 fertilisation will benefit C3 savanna trees more than C4 grasses, leading to a loss in labile grass root exudates and thus the mineral-associated organic carbon (MAOC) that depends on these exudates.
3. We found that grasses, not trees, were associated with increased SOC in savanna soil to a depth of 0.3 m due to their relatively large biomass, regardless of CO2 concentration. Soil planted with both grass and trees had 10% more carbon and 8% more nitrogen compared to trees only. End-member mixing models indicated that 50% to more than 90% of this carbon was grass-derived. Savanna SOC accumulation occurred primarily through below-ground and indirectly through aboveground biomass, which drove the formation of the occluded particulate organic carbon fraction (oPOC) according to a structural equation model. Similar results were observed for soil nitrogen. The responsiveness of oPOC (and not MAOC) in this savanna soil is different to temperate grassland soils, emphasising the need to understand savanna SOC dynamics.
4. While recognising the limitations of pot culture, our results provide a clear message for policymakers and land managers: Conservation of grassy biomes such as savannas, and not afforestation, aligns with both climate and biodiversity goals.
Metadata
| Item Type: | Article |
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| Authors/Creators: |
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| Copyright, Publisher and Additional Information: | © 2026 The Author(s). Functional Ecology published by John Wiley & Sons Ltd on behalf of British Ecological Society. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. http://creativecommons.org/licenses/by/4.0/ |
| Keywords: | afforestation; climate change; elevated carbon dioxide; nitrogen; woody thickening |
| Dates: |
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| Institution: | The University of Sheffield |
| Academic Units: | The University of Sheffield > Faculty of Science (Sheffield) > School of Biosciences (Sheffield) |
| Date Deposited: | 30 Jun 2026 11:17 |
| Last Modified: | 30 Jun 2026 11:17 |
| Status: | Published online |
| Publisher: | Wiley |
| Refereed: | Yes |
| Identification Number: | 10.1111/1365-2435.70394 |
| Related URLs: | |
| Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:242679 |

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