During ebb situations in tidal estuaries with high tidal amplitude most of the system is out of water. ln this period intertidal pool formation takes place in very extended areas. These pools differ with respect to intemal nutrient loading, hydraulic conditions, duration, plant coverage, sediment properties such as organic content in the sediment, C/N/P-ratios of the sediment nutrient sources and porewater concentrations of nutrients. Therefore, the objective was to study and compare the nutrient sources and dynamics in different types of intertidal pools of the Mondego estuary. ln each intertidal pool the nutrient dynamics were followed on a seasonal scale by measuring oxygen dynamic, phosphate, ammonia, nitrate besides physical parameters as salinity. temperature, sediment organic matter; sediment total phosphorus, potential phosphate adsorption, total sediment nitrogen, sediment water contento pool volume and pool area The results showed that the nutrient dynamics in shallow intertidal pools are much faster than in subtidal areas. This is most probably due to the shallowness of the systems giving anabolic as well as catabolic processes optimal conditions with respect to light climate, oxygen concentrations, higher concentrations of dissolved inorganic nutrient and higher mean temperature during the growth season. At1ogether; this study indicate that in the Sportino moritimo covered areas the plants are able to control the phosphorus dynamic due to Sportino moritimo take up phosphate for growth purposes, that without plant coverage would have retumed to the watercolumn and that Sportino do also facilitates the increased phosphate adsorption. On the system levei most pools are situated on bare bottom without connection to rooted vegetation, and these leaks with substantial amounts of phosphate. 50 the intertidal pool system of the Mondego estuary at10gether are exporting significant amounts of phosphorus in these years.