The occurrence of high extracellular DNA concentrations in aquatic sediments (concentrations that are 3 to 4 orders of magnitude greater than those in the water column) might play an important role in biogeochemical cycling, as well as in horizontal gene transfer through natural transformation. Since isolation of extracellular DNA from sediments is a difficult and unsolved task, in this study we developed an efficient procedure to recover simultaneously DNA associated with microbial cells and extracellular DNA from the same sediment sample. This procedure is specifically suitable for studying extracellular DNA because it avoids any contamination with DNA released by cell lysis during handling and extraction. Applying this procedure to different sediment types, we obtained extracellular DNA concentrations that were about 10 to 70 times higher than the intracellular DNA concentrations. Using specific targeted prokaryotic primers, we obtained evidence that extracellular DNA recovered from different sediments did not contain amplifiable 16S rRNA genes. By contrast, using DNA extracted from microbial cells as the template, we always amplified 16S rRNA genes. Although 16S rRNA genes were not detected in extracellular DNA, analyses of the sizes of extracellular DNA indicated the presence of high-molecular-weight fragments that might have contained other gene sequences. This protocol allows investigation of extracellular DNA and its possible participation in natural transformation processes.All aquatic sediments are characterized by high DNA concentrations (concentrations that are 3 to 4 orders of magnitude greater than those found in the water column), mostly (up to 90%) due to extracellular DNA (3,5,7,8,23). Previous studies reported that complex refractory organic molecules and/or inorganic particles are able to bind, adsorb, and stabilize free DNA in sediments (17,21,28). Dell'Anno et al. (8) reported that the free extracellular DNA fraction represented less than 5% of the total extracellular DNA pool. The adsorption of extracellular DNA in the sediment might reduce its degradability, and indeed only about 50% of this DNA can be hydrolyzed by nucleases (8). Consequently, the residence time of extracellular DNA in sediments can be much longer than the residence time in the water column (17,22). The presence and persistence of large amounts of extracellular DNA in the deeper sediment layers (2, 5) might have important implications for bacterial metabolism, providing a source of nitrogen and phosphorous and/or exogenous nucleotides (3,7,14,27,32), and may also contribute to horizontal gene transfer through natural transformation (17,24).In the last few years, several protocols for extraction of DNA from soils and sediments have been developed and improved (13,15,29,31,35). In fact, application of culture-independent nucleic acid techniques involving DNA extraction and molecular analyses has allowed the detection and identification of microorganisms in natural environments (10). At the same time, much effort has also b...