Human disturbance drives loss of soil organic matter and changes its stability and sources in mangroves

Mangrove soils with high organic carbon (Corg) content are likely to contain Corg that is vulnerable to remineralization during land use changes. Mangrove conversion to different land uses might deplete soil Corg stocks causing variable carbon dioxide emissions, but the extent of these emissions and the fraction of soil Corg (i.e., labile or stable/recalcitrant) that is mostly lost is poorly understood. Here, we study mangrove soil Corg degradability and its susceptibility to mineralization after mangrove disturbance. We measured changes in soil properties, organic matter (OM) stability and Corg pools and sources across a mangrove disturbance gradient (i.e., pristine forests, degraded mangroves receiving domestic sewage and shrimp farm effluents, and shrimp ponds). Results showed that the conversion of mangroves to shrimp ponds caused the most severe changes in soil properties, OM and Corg characteristics. Shrimp pond soils contained the lowest OM-Corg pools, consisted mostly of stable OM (i.e., recalcitrant and refractory; 36.0 +/- 5.7% of the total OM) and enriched delta 13Corg (-22.6 +/- 2.7%o). Conversely, control mangrove soils had the largest OM-Corg pools consisting of a large unstable OM fraction (i.e., labile; 46.4 +/- 4.2%) and lighter delta 13Corg (-26.8 +/- 0.4%o) being characteristic of Corg from a mangrove origin. Conversion of mangroves to shrimp ponds and its degradation by shrimp farm and domestic sewage effluents caused a loss of 97%, 61%, and 35% of soil Corg stocks in the upper meter, representing potential emissions of -1200, 800, and 400 Mg CO2 ha-1, respectively. These losses were explained by enhanced OM mineralization of unstable fractions driven by the loss of the physico-chemical protection provided by finegrained soils and vegetation cover. The differences in Corg stability among sites can be used to predict potential carbon dioxide produced during mineralization, hence aid at prioritizing areas for conservation, restoration or management.

Automated summary

Conversion of mangroves to shrimp ponds resulted in severe changes in soil properties, organic matter stability and Corg characteristics. Shrimp pond soils contained the lowest OM-Corg pools, consisting mostly of stable OM, while control mangrove soils had the largest OM-Corg pools consisting of unstable OM.