A sequential extraction method consisting of six operationally-defined fractions has been developed for determining the geochemical partitioning of natural (U, Th, 4~ and antropogenic (Pu, Am, 137Cs) radionuclides in a 40-50 cm deep sediment sample collected in a Venice canal.Extraction chromatography with Microthene-TOPO (U, Th), Microthene-TNOA (Pu) and Microthene-HDEHP (Am) column was used for the chemical separation of a single radionuclide; the final recoveries were calculated by adding 236U, 229Th, 242pu and 243Am as the yield tracers. After electrodeposition the alpha spectrometry was carried out. 137Cs and 4~ were measured by gamma spectrometry.The total concentrations in the wet sample (Bq/kgd), obtained by a complete disgregation of the matrix by wet and dry treatment, were the following: 239+24~ + 0.07, 23Spu = 0.022 + 0.005,241Am = 0.337 _+ 0.027, 137Cs = 9.78 + 0.78, 238U = 28.84 + 1.62, 232Th --21.42 _+ 1.93, 4~ = 376.05 + 12.78. The mean ratio 238pu]239+240pu (0.02) shows a contamination due essentially to fall-out and U and Th alpha spectra indicate the natural origin of two elements. The absence of 134Cs in the sample proves that at 40 -50 cm depth the sediment was not affected by the Chernobyl fall-out. As far as the speciation is concerned the following fractions were considered: water soluble, carbonates, Fe-Mn oxides, organic matter, acid soluble, residue. Pu (-67%) and Am (~ 95%) were present principally in the carbonate fraction; U was more distributed and about 30% and 45% appeared in the carbonate fraction and in the residue respectively; the majority of Th was present in the residue (-60%); 4~ was totally present in the residue; finally 137Cs was found mostly in the acid soluble fraction (-53%) and in the residue (~ 47%).Some stable elements (Fe, Mn, A1, Ti, Ca, Pb, Ba) were also determined in the different fractions to get more information about the chemical association of the single radionuclides.