This review covers historical perspectives, the role of plant inputs, and the nature and 12 dynamics of soil organic matter (SOM), often known as humus. Information on turnover 13 of organic matter components, the role of microbial products, and modeling of SOM, and 14 tracer research should help us to anticipate what future research may answer today's challenges. Our globe's most important natural resource is best studied relative to its chemistry, dynamics, matrix interactions, and microbial transformations. Humus has similar, worldwide characteristics, but varies with abiotic controls, soil type, vegetation inputs and composition, and the soil biota. It contains carbohydrates, proteins, lipids, phenol-aromatics, protein-derived and cyclic nitrogenous compounds, and some still unknown compounds. Protection of transformed plant residues and microbial products occurs through spatial inaccessibility-resource availability, aggregation of mineral and organic constituents, and interactions with sesquioxides, cations, silts, and clays. Tracers that became available in the mid-20 th century made the study of SOM dynamics possible. 24 Carbon dating identified resistant, often mineral-associated, materials to be thousands of 25 years old, especially at depth in the profile. The 13 C associated with C 3-C 4 plant switches characterized slow turnover pools with ages ranging from dozens to hundreds of years. Added tracers, in conjunction with compound-specific product analysis and incubation, identified active pools with fast turnover rates. Physical fractionations of the intra-and inter-aggregate materials, and those associated with silt and clay, showed that all pools contain both old and young materials. Charcoal is old but not inert. The C:N ratio changes from 25 to 70:1 for plant residues to 6 to 9:1 for soil biota and microbial 3 products associated with soil minerals. Active, slow and passive (resistant) pool concepts 33 have been well used in biogeochemical models. The concepts discussed herein have 34 implications for today's challenges in nutrient cycling, biogeochemistry, soil ecosystem 35 functioning, pollution control, feeding the expanding global population and global 36 change.