With the aim of evaluating temporal changes in sedimentation and organic carbon (C org ) supplied over the last~100 years, a sediment core was collected at Soledad Lagoon, a costal ecosystem surrounded by mangroves, located in the Cispatá Estuary (Caribbean coast of Colombia). The core sediments were characterized by low concentrations of calcium carbonate (0.2-2.9%), organic matter (3-8%), total nitrogen (0.11-0.38%), and total phosphorus (0.19-0.65 mg g −1 ). Fe and Al concentrations ranged from 4% to 5%, and Mn from 356 to 1,047 μg g −1 .The 210 Pb-derived sediment and mass accumulation rates were 1.54±0.18 mm year −1 and 0.08±0.01 gcm −2 year −1 , respectively. The sediment core did not provide evidence of human impact, such as enhancement of primary production or nutrient enrichment, which may result from recent land uses changes or climate change. The C org fluxes estimated for Soledad Lagoon core lay in the higher side of carbon fluxes to coastal ecosystems (314-409 gm −2 year −1 ) and the relatively high C org preservation observed (~45%) indicate that these lagoon sediments has been a net and efficient sink of C org during the last century, which corroborate the importance of mangrove areas as important sites for carbon burial and therefore, long-term sequestration of C org .