In order to determine the mechanisms involved in the persistence of extracellular DNA in soils and to monitor whether bacterial transformation could occur in such an environment, we developed artificial models composed of plasmid DNA adsorbed on clay particles. We determined that clay-bound DNA submitted to an increasing range of nuclease concentrations was physically protected. The protection mechanism was mainly related to the adsorption of the nuclease on the clay mineral. The biological potential of the resulting DNA was monitored by transforming the naturally competent proteobacterium Acinetobacter sp. strain BD413, allowing us to demonstrate that adsorbed DNA was only partially available for transformation. This part of the clay-bound DNA which was available for bacteria, was also accessible to nucleases, while the remaining fraction escaped both transformation and degradation. Finally, transformation efficiency was related to the perpetuation mechanism, with homologous recombination being less sensitive to nucleases than autonomous replication, which requires intact molecules.In the environment, three mechanisms are thought to be involved in gene uptake by bacteria (31), namely, conjugation, transformation, and transduction. Natural bacterial genetic transformation is the mechanism by which a bacterium acquires naked DNA. Such a mechanism is thought to have been involved in gene transfers during evolution and particularly in transfers among unrelated organisms such as plants and bacteria (1,8,21). However, numerous reports indicate that gene transfer events may be very rare in the environment (14,18,33). This could be due to the numerous steps that are required to achieve transformation. DNA released by organisms must persist under adverse conditions such as those encountered in soils. Naked DNA must then encounter competent recipient bacteria. Moreover, the incorporated DNA will only be perpetuated if its nucleotide sequences exhibit sufficient similarity to the recipient genome to allow recombination, unless the sequences possess a replicon which is operational in the new host (14,16,33).Nevertheless, there is a general agreement that natural transformation may occur in complex media such as soils. Indeed, large amounts of naked DNA, which is the preliminary key factor for transformation, can be detected in soils (7,35,40). Moreover, there is much evidence that extracellular DNA can persist for periods of time up to several months or years (8,18,25,27,28,38). Adsorption of DNA on soil components, particularly on clay minerals such as montmorillonite, illite, and kaolinite, is thought to be involved in protection of nucleic acids against nucleases, and could explain the high content of DNA in soils (2, 10, 32). However, soil or microcosm-based experiments have indicated that the adsorption-related protection process has only limited impact (3,17,25,27). In fact, very little is known about the protection mechanism itself, and the influence of parameters such as clay type, the size of DNA or its conformati...