Concentration profiles of NH., and NO? in pore water and particulate matter were determined at high spatial resolution (mm bcale) in surface sediment from a coastal bay area (Aarhus Bight, Denmark) at 15 m depth during an annual cycle. Pore water pools of NH: and NO; were always considerably lower than particulate pools in the surface sediment. Particulate NH: and NO; were apparently intracellular pools in deposited microalgae and were extracted after freezing sedlment samples in liquid NZ (-196 "C). Pore water NH: and most of the adsorbed (KCI-extractable) NH: were also extracted by the freezing technique, and an estimate of the intracellular NH: pool was obtained by difference. In the absence of an adsorbed NOS pool, intracellular NO? was determined by subtraction of the pore water pool from the liquid NZ-extractable pool. Highest concentrations of intracellular NH: and NO; were always observed in the upper 2 mm of sediment, declining sharply with depth. A distinct seasonal maximum for both pools, ca 200 nmol cm-3 at 0 to 2 mm depth, appeared after sedimentation of a phytoplankton bloom in early spring, and should be compared to a minimum of only 25 nmol or less in fall and winter. The freeze-extraction technique is proposed for a reliable estimate of intracellular NH: and NO; pools in surface sediments r~c h In microalgae, and may thus be used as an indicator of sedimentation of phytoplankton blooms. The signiflcance of intracellular pools for sediment nitrogen cycling is discussed.