Part of the Marchamalo saltpans (Murcia, Spain) has been abandoned for 28 years. The
project “RESALAR” aims to restore 8 ha of this saltpan to extract salt in a traditional way
while preserving biodiversity and historical heritage. The principal primary producers in
hypersaline wetlands are microorganisms such as cyanobacteria and chlorophytes. Once the
microorganism’s biomass becomes part of the decomposing sediment organic matter, the high
sediment salinity and moisture levels leads to an anoxic environment, allowing it to be buried
in the sediments. In this context, our study, previous to the restoration, aims to assess the
carbon stock accumulated during the period of disuse as well as measure the carbon dioxide
(CO2) efflux from the saltpan to the atmosphere and the effect of various physicochemical
variables on soil CO2 emissions. To determine the carbon stock in the first 0.5 m we extracted
a core from every tank, analyzed the bulk density, organic carbon, inorganic carbon and
salinity in 5 cm sections. CO2 fluxes were measured using a soil respiration chamber
connected to an infrared gas analyzer, and samples were taken from the first 10 cm of soil to
analyze physicochemical variables. Our preliminary results shows that mean carbon stock
value was 1349.71±251.39 Mg ha-1 and mean CO2 flux was 0.55±0.84 g m-2 h-1. Temperature
was the main CO2 flux driver, while sediment moisture was the main carbon burial driver.
Our results will be used to suggest management strategies to make the salt extraction
compatible with carbon burial
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