Sediment to atmosphere CO2 efflux increases at retreating salt marsh edges

Abstract

Coastal intertidal wetlands are dynamic and biodiverse habitats with carbon-rich waterlogged soils. When the soil gets exposed to oxygen, carbon can be emitted as CO₂ back into the atmosphere. In this study we investigate whether contrasting stepped vs. gradual marsh edge topography, resulting from lateral cliff erosion versus expansion influences the soil-atmosphere CO₂ fluxes. CO₂ fluxes were quantified alongside groundwater level, soil temperature, and local sediment grain size across an estuarine salt marsh with differing seaward edge topography. We found that the CO₂ flux from the marsh soil was on average greater at cliffed-eroding compared to sloped-prograding sites, 1.11 ± 0.77 g/m² hr⁻¹ and 0.88 ± 0.74 g/m² hr⁻¹, respectively. The presented CO₂ emissions from the soil to the atmosphere consider the static morphology, i.e., the fluxes from the soil as it sits in place during the respective measurement. Soil respiration varied temporally with tidal cycle, groundwater levels, soil temperature, and spatially with distance to the seaward vegetation edge. Overall, fluxes during a neap cycle were significantly larger compared to spring tidal cycles. Our study thus highlights that soil CO₂ efflux is affected by marsh topography resulting from cliff formation and marsh edge undercutting. The eroding and prograding sites differed in their site characteristics related to groundwater level, grain size and soil temperature, influencing the soil to atmosphere CO₂ flux from the remaining marsh platform. Our findings highlight the spatial and temporal variability of carbon fluxes in a salt marsh environment and the importance of geomorphic form and process in understanding coastal carbon dynamics.