The role of naturally-occurring soil organic matter (SOM) in the translocation of metal ions from parent materials to biological systems is discussed. To explain the movement of essential elements, a hypothesis or model is proposed where the translocation includes a sequence of reactions involving competition among electron-donor simple molecules and highly polymerized organic materials with numerous functional groups. The sequence has a cascade character through which the metals are gradually transferred from the inert rocks to the higher animals. Naturally-occurring SOM binds the metal ions constituting an intermediate stage by which substantial losses by percolation of free cations, metallic aquo complexes, or simple organic metal complexes are avoided. Also SOM, highly saturated with metal ions, may constitute the most important pool of micronutrients available to biological systems. Microbial humic-acidlike polymers and polysaccharides with free functional groups likely constitute new or young SOM. Since extraction of unaltered SOM may be a difficult or impossible task, it is proposed that microbial polymers would constitute an excellent source material to investigate the role of SOM in metal-ion translocation in soils. A good approach to study the involvement of SOM would be to measure its maximum metal-ion binding ability (MBA). MBA would be a measurement indicating the potential total capacity of the macromolecules to bind metal ions. Stability constant measurements are not involved as these could only be properly determined if organic macromolecules of a definite molecular weight were available.