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The Bay of Cádiz is surrounded by a broad zone of salt marshes that exchange water through a seawater channel 18 km in length (the Sancti Petri Channel). These littoral zones are characterized by their extreme shallowness (with a mean depth of less than 1 m) and their high content of organic matter, which in relative terms is highest in the surface sediments (between 1.2% and 2.6% organic carbon). Under these conditions, an intensive benthic regeneration of nutrients takes place, with mean fluxes in the zone of 83.2 ± 36.9 mmol m[sup-2] d[sup-1] of inorganic carbon, 6.36 ± 4.56 mmol m[sup-2] d[sup-1] of NH[sub4][sup+], 1.14 ± 0.56 mmol m[sup-2] d[sup-1] of HPO[sub4]&sup2-; and 4.54 ± 2.25 mmol m[sup-2] d[sup-1] of SiO[sub2]. A proportion of these The Bay of Cádiz is surrounded by a broad zone of salt marshes that exchange water through a seawater channel 18 km in organic carbon produced make their way through secondary channels to the Sancti Petri Channel, and the material is later transported by the tides to the Bay of Cádiz and other bordering littoral zones. In this work, the concentrations of inorganic carbon and nutrients (NH[sub4][sup+], NO[sub2][sup-], NO[sub3][sub-] HPO[sub4[-]&sup2-; and SiO[sub2]) have been determined at three different depths, every hour, during complete tidal cycles. Simultaneously, the current velocities at different depths have been measured continuously. From this set of experimental data, calculations have been made of the evolution of the instantaneous velocities of these substances at each end of the channel, and by integration, the net balance for the Complete tidal cycle. In general terms, there is an export of inorganic carbon and nutrients with the tides, although the net transports are very variable and depend to a large extent on the hydrodynamics of the zone. The results obtained correlate with balances previously made in the Bay of Cádiz. [ABSTRACT FROM AUTHOR]