CONICET | Buscador de Institutos y Recursos Humanos

Coastal marshes store large amounts of organic carbon in their sediments and accountfor an important fraction of carbon storage in the ocean and adjacencies. However, themagnitude of carbon storage in salt marsh soil deposits is variable, and adequateinventories have not been made for most coastal settings in the southern hemisphere.We quantified and characterized the soil organic carbon pool stored in Sarcocorniaperennis marshes of the Bahía Blanca Estuary, a major coastal wetland system in theSW Atlantic. Land cover classes were mapped from aerial photographs (year 1967)and high-resolution satellite images (years 2005 and 2017) and rates of salt marsherosion were evaluated. Erosion rates of S. perennis marshes (% loss per year)increased from 0.8 % (from 1967 to 2005) to 2.0 % (from 2005 to 2017). For this laterperiod, salt marshes lost to mudflats at an average rate of 1.03 km2 year -1. Consideringthe average erosion depths and soil organic carbon densities, between 2005 and 2017the northern section of the Bahia Blanca Estuary exported organic carbon at a rate of2893 tC year-1. The stored organic material under erosion presents a very low C : Nratio (8 - 10), and its bulk isotopic composition (δ13C -24.7 to -16.8 ?; δ15N +8.7 to +11.3?) reflects a dominance of organic matter of marine origin. Bulk organic matter from adeep section of one core (2.14 m below surface) was 14C dated 4710 ± 30 years BP. Inthe study area, transgressive sea level events took place throughout the Holocene.Thus, the presently intertidal platform occupied by S. perennis marshes is likelycomposed of marine deposits that formed under a higher relative sea level. Under thecurrent rates of relative sea level rise (+1.51 + 0.32 mm year-1, Buenos Aires Harbor)there is accelerated erosion, and salt marsh soils act as a significant net source oforganic carbon and nitrogen to estuarine waters