Saprotrophic fungi are key moderators in the global carbon cycle because of their ability to degrade the three most abundant biopolymers: cellulose, lignin, and chitin. Fungi are a signifi cant contributor to soil microbial biomass but little is known about the contributions of fungal biomass to diagenetically altered soil organic carbon. Here we show that a portion of fungal necromass is resistant to decay by a natural soil microbial community over a month-long degradation study. The results of FTIR analysis indicate that this resistant portion is likely composed mainly of fungal chitin.
CITATION STYLE
Schreiner, K. M., Blair, N. E., Levinson, W., & Egerton-Warburton, L. M. (2014). Contribution of Fungal Macromolecules to Soil Carbon Sequestration. In Soil Carbon (pp. 155–161). Springer International Publishing. https://doi.org/10.1007/978-3-319-04084-4_16
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