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Simulating carbon accumulation and loss in the central Congo peatlands
Dylan M Young1, Andy J Baird1, Paul J Morris1
1School of Geography, University of Leeds, Leeds, UK.
Tropical peatlands store vast carbon. A new model shows surface wetness and slow decay control accumulation, but drying can cause catastrophic carbon loss, highlighting vulnerability to climate change.
Area of Science:
- Earth and Environmental Sciences
- Climate Science
- Ecology
Background:
- Central Congo Basin peatlands store approximately 29 billion tonnes of carbon.
- Understanding peat carbon dynamics and climate change vulnerability is limited.
Purpose of the Study:
- To model peat carbon accumulation and loss in a tropical peatland.
- To identify key controls on peatland carbon dynamics.
- To assess the vulnerability of peat carbon stores to climate shifts.
Main Methods:
- Development of the DigiBog_Congo model for tropical peatland simulation.
- Simulation of peat carbon accumulation and loss over ~20,000 years.
- Comparison of model age-depth curves with palaeoenvironmental reconstructions.
Main Results:
- Model simulations align well with palaeoenvironmental data.
- Surface wetness and slow anoxic decay are primary controls on peat accumulation.
- A drying phase ~5200 years BP led to significant carbon loss (57% of stock) over millennia.
Conclusions:
- Rainfall variability alone can trigger catastrophic, long-term peat carbon loss.
- Tropical peatlands are highly vulnerable to climate change-induced drying.
- The model provides a framework for assessing future climate and land-use impacts on peat carbon.
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