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Tropical wetlands significantly impact global greenhouse gas (GHG) budgets and carbon storage; however, data from sub-Saharan Africa (SSA) remain limited. Highland valley-bottom wetland (HVBW) agriculture supports millions, yet its effects on GHG emissions and carbon storage remain undocumented. This study quantified soil emissions of nitrous oxide (N 2 O), carbon dioxide (CO 2 ), and methane (CH 4 ) in the Taita Hills, Kenya, from 12 converted, 10 recovering, and one reference (intact) HVBW. Agricultural conversion shifted wetland emissions from CH 4 to N 2 O dominance. Converted HVBWs were N 2 O sources (1.6 kgN2O-Nha-1yr-1), driven by elevated soil nitrate, whereas the intact HVBW was an N 2 O sink (−0.3 kgN2O-Nha-1yr-1), with high soil moisture and a high soil C/NO3--N ratio suggesting complete denitrification. Recovering HVBWs showed intermediate N 2 O emissions (0.5 kgN2O-Nha-1yr-1). CO 2 emissions were similar between converted and recovering HVBWs (9534 vs. 9610 kgCO2-Cha-1yr-1) but lower in the intact (2923 kgCO2-Cha-1yr-1). CH 4 emissions were highest in the intact HVBW (2757 kgCH4-Cha-1yr-1), intermediate in recovering sites (781 kgCH4-Cha-1yr-1), and lowest in converted sites (38 kgCH4-Cha-1yr-1). The intact HVBW had an SOC stock of 224 Mg C ha −1 , indicating carbon loss rates of 2.7 MgCha-1yr-1 over 45 years for converted HVBWs. Comparing recovering with converted HVBWs suggests an SOC recovery of about 1.1 MgCha-1yr-1 after abandonment, offsetting ∼0.0005 % of Kenya's annual agricultural GHG emissions, or 9.8 % when scaled nationally. However, recovering HVBWs also emitted considerably more CH 4 , so their net climate effect cannot be derived from SOC stocks alone. These findings highlight trade-offs between GHG emissions and carbon storage in HVBWs, with wetland recovery promoting partial functional restoration and SOC recovery in SSA, but at the cost of increased CH 4 emissions.
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Gubamwoyo et al. (2026) studied this question.
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