Abstract
The understanding that some natural organic molecules can resist microbial decomposition because of certain molecular properties forms the basis of the biogeochemical paradigm of 'intrinsic recalcitrance'. In this concept paper I argue that recalcitrance is an indeterminate abstraction whose semantic vagueness encumbers research on terrestrial carbon cycling. Consequently, it appears to be advantageous to view the perceived 'inherent resistance' to decomposition of some forms of organic matter not as a material property, but as a logistical problem constrained by (i) microbial ecology; (ii) enzyme kinetics; (iii) environmental drivers; and (iv) matrix protection. A consequence of this view would be that the frequently observed temperature sensitivity of the decomposition of organic matter must result from factors other than intrinsic molecular recalcitrance. © CSIRO 2010.
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CITATION STYLE
Kleber, M. (2010). What is recalcitrant soil organic matter? Environmental Chemistry, 7(4), 320–332. https://doi.org/10.1071/EN10006
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