Fragmentation as a condition for persistence - exploring a new perspective of mineral-organic interactions

High radiocarbon ages (centennial to millennial) of soil organic matter tend to occur in soils with high proportions of reactive, hydroxylated minerals, including andisols, spodosols and oxisols. This indicates that the most reactive mineral surfaces, i.e. those that should in theory be particularly efficient in promoting transformations of organic matter are among the most powerful in protecting organic matter against decomposition on long time scales. The easiest way to reconcile this apparent paradox is to assume that organic compounds become fragmented upon contact with minerals, thereby generating fragmentation products which in turn are more likely to become preserved within the soil fabric than their precursor molecules. Here we use Vacuum Ultraviolet - Post Ionisation -Mass Spectroscopy (VUV-PI-MS) in combination with thermal and laser desorption to show how organic compounds undergo complete fragmentation upon contact with mineral surfaces. Fragmentation patterns were generally different between oxidic minerals and minerals belonging to the phyllosilicate group. Also, desorption from phyllosilicates generally required significantly higher energies than desorption from oxide phases. Our investigation suggests that, at low energy levels, breakdown and fragmentation is a probably major outcome of mineral-organic interactions. This observation supports a new model for the role of mineral-organic interactions in the preservation of organic compounds in the environment: mineral-induced fragmentation as a prerequisite for long term protection against decomposition.