Abstract

Abstract. Terrestrial carbon resources are major drivers of development in West Africa. The distribution of these resources co-varies with ecosystem type and rainfall along a strong Northeast-Southwest climatic gradient. Soil organic carbon, a strong indicator of soil quality, has been severely depleted in some areas by human activities, which leads to issues of soil erosion and desertification, but this trend can be altered with appropriate management. There is significant potential to enhance existing soil carbon stores in West Africa, with benefits at the global and local scale, for atmospheric CO2 mitigation as well as supporting and provisioning ecosystem services. Three key factors impacting carbon stocks are addressed in this review: climate, biotic factors, and human activities. Climate risks must be considered in a framework of global change, especially in West Africa, where landscape managers have few resources available to adapt to climatic perturbations. Among biotic factors, biodiversity conservation paired with carbon conservation may provide a pathway to sustainable development, and biodiversity conservation is also a global priority with local benefits for ecosystem resilience, biomass productivity, and provisioning services such as foodstuffs. Finally, human management has largely been responsible for reduced carbon stocks, but this trend can be reversed through the implementation of appropriate carbon conservation strategies in the agricultural sector, as shown by multiple studies. Owing to the strong regional climatic gradient, country-level initiatives will need to consider carbon sequestration approaches for multiple ecosystem types. Given the diversity of environments, global policies must be adapted and strategies developed at the national or sub-national levels to improve carbon storage above and belowground. Initiatives of this sort must act locally at farmer scale, and focus on ecosystem services rather than on carbon sequestration solely.

Highlights

  • Soils are major reservoirs of terrestrial carbon (C), containing an estimated mass of 1200–1600×109 Mg of C (Eswaran et al, 1993; Batjes, 1996; Zech et al, 1997), which makes them an essential component of atmospheric CO2 mitigation

  • A strong indicator of soil quality, has been severely depleted in some areas by human activities, which leads to issues of soil erosion and desertification, but this trend can be altered with appropriate management

  • These two goals, along with others, may be compatible in some forestry or agriculture applications in West Africa, and we show that temporal C dynamics and sequestration capacity will differ between systems

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Summary

Introduction

Soils are major reservoirs of terrestrial carbon (C), containing an estimated mass of 1200–1600×109 Mg of C (Eswaran et al, 1993; Batjes, 1996; Zech et al, 1997), which makes them an essential component of atmospheric CO2 mitigation. In this review we discuss the importance of SOC in West Africa for climate change mitigation and conservation of soil fertility. These two goals, along with others, may be compatible in some forestry or agriculture applications in West Africa, and we show that temporal C dynamics and sequestration capacity will differ between systems. We discuss patterns of land use and management, and how social structures may affect the accumulation of SOC Overall, this synthesis is aimed towards identifying the processes that have the greatest effect on soil C–based ecosystem service provision, and how increased soil C sequestration might be achieved to assist both local sustainability and climate change mitigation (Fig. 2)

Climate changes and soil C release in Africa
Contribution to mitigation of global warming
Local relevance – SOM and nutrient cycling
Land use change and soil carbon evolution
Soil carbon and socio-economic structure
Findings
Concluding remarks
Full Text
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