Friday, August 10, 2007: 9:50 AM
J3, San Jose McEnery Convention Center
Chemistry of plant material is a crucial control on litter decomposition rates. However, we know less about the fate of plant-derived compounds entering soils. A variety of mechanisms stabilize (or destabilize) plant litter in soil. Despite lignin dominance as a structural control in litter decomposition, other plant compounds such as epicuticular waxes may be more important in soils. Employing several analytical methods (FT-infrared spectromicroscopy, flash-pyrolytic gas chromatography-mass spectrometry, and 13C-nuclear magnetic resonance), we examined plant-soil chemistry over a range of decomposition. We examined: (1) live foliage and fresh litter from a fast-decomposing tree in the Araliaceae (Cheirodendron trigynum), and a slow-decomposing Gleicheniales fern (Dicranopteris linearis); (2) litter differing in mass loss % from decomposition experiments; (3) root mats below stands of certain species; and (4) size fractions of O- and A- soil horizons from 3-ky and 150-ky Hawai`ian sites. PyGC-MS comparisons of foliage and litter indicate fatty acid methylesters distinguish the slow-decomposing fern from fast-decomposing tree. We removed epicuticular wax from the two species for GC-MS. Not only is the wax / wax-ester load much higher in fern than the tree, but novel secondary waxy alcohols / diols were detected in fern cuticles. Remaining tissues yielded significantly different FT-IR signals from polysaccharides and cell wall-phenolics, with preferential preservation of polysaccharides in the fern, and lipids in the tree. In the field, py-GCMS suggests plant composition plays a role in controlling soil chemistry, tending towards higher concentrations of lipid derived materials in soils under vegetation with high fatty acid content.