Abstract

Plants produce above- and below-ground biomass. However, our understanding of both production and decomposition of below-ground biomass is poor, largely because of the difficulties of accessing roots. Below-ground organic matter decomposition studies are scant and especially rare in the tropics. In this study, we used a litter bag experiment to quantify the mass loss and nutrient dynamics of decomposing twigs and small roots from an arbuscular mycorrhizal fungal associated tree, Parashorea chinensis Wang Hsie, in a tropical rain forest in Southwest China. Overall, twig litter decomposed 1.9 times faster than small roots (decay rate (k) twig = 0.255, root = 0.134). The difference in decomposition rates can be explained by a difference in phosphorus (P) concentration, availability, and use by decomposers or carbon quality. Twigs and small roots showed an increase in nitrogen concentration, with final concentrations still higher than initial levels. This suggests nitrogen transfer from the surrounding environment into decomposing twigs and small roots. Both carbon and nitrogen dynamics were significantly predicted by mass loss and showed a negative and positive relationship, respectively. Our study results imply that small roots carbon and nitrogen increase the resident time in the soil. Therefore, a better understanding of the carbon cycle requires a better understanding of the mechanisms governing below-ground biomass decomposition.

Highlights

  • Litter production and decomposition represent the principle pathways of carbon and nutrient cycling in terrestrial ecosystems

  • We set up a standard litter bag experiment to examine the patterns of twig and fine root decomposition in an arbuscular mycorrhizal (AM) tree, Parashorea chinensis Wang Hsie, in a tropical rain forest in SW

  • We found that twigs decomposed faster than small roots and that C and N concentration had a negative and positive relationship, respectively, with percentage mass loss regardless to the litter substrate

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Summary

Introduction

Litter production and decomposition represent the principle pathways of carbon and nutrient cycling in terrestrial ecosystems These pathways are much better understood for the above-ground organs, as compared to below-ground ones [1]. This is mostly due to difficulties related to accessing and sampling below-ground litter materials [2,3]. This has led to derivation of climate models and carbon cycle model parameters mainly based on studies of above-ground biomass [4]. From studies on above-ground litter materials, we know that decomposition is controlled by both abiotic and biotic factors [5,6]

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