Abstract

Tropical peatlands are a significant carbon store and source of carbon dioxide (CO2) and methane (CH4) to the atmosphere. Plants can contribute to these gas emissions through the release of root exudates, including sugars and organic acids amongst other biomolecules, but the roles of concentration and composition of exudates in regulating emissions remains poorly understood. We conducted a laboratory incubation to assess how the type and concentration of root exudate analogues regulate CO2 and CH4 production from tropical peats under anoxic conditions. For CO2 production, substrate concentration was the more important driver, with increased CO2 fluxes following higher addition rates of four out of the six exudate analogues. In contrast, exudate type was the more important driver of CH4 production, with acetate addition associated with the greatest production, and inverse correlations between exudate concentration and CH4 emission for the remaining five treatments. Root exudate analogues also altered pH and redox potential, dependent on the type of addition (organic acid or sugar) and the concentration. Overall, these findings demonstrate the contrasting roles of composition and concentration of root exudate inputs in regulating greenhouse gas emissions from tropical peatlands. In turn this highlights how changes in plant communities will influence emissions through species specific inputs, and the possible impacts of increased root exudation driven by rising atmospheric CO2 and warming.

Highlights

  • Peatlands are a significant source of methane (CH4) emissions, contributing between 20 and 39% of annual CH4 production, as well as making a significant contribution to atmospheric carbon dioxide (CO2) emissions (Laanbroek, 2010)

  • We previously showed that root exudate analogues significantly increase peat microbial community activity and enhance the production of both CO2 and CH4 (Girkin et al, 2018a)

  • All Root exudate compounds (RECs) additions were associated with a significant increase in CO2 fluxes (F18,90 = 12.72, p < 0.001, Fig. 1a–f), with a significant increase in fluxes over time (F6,570 = 1498.4, p < 0.001)

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Summary

Introduction

Peatlands are a significant source of methane (CH4) emissions, contributing between 20 and 39% of annual CH4 production, as well as making a significant contribution to atmospheric carbon dioxide (CO2) emissions (Laanbroek, 2010). Plants release root exudates, which represent a significant source of labile C released at depth This addition can impact peat properties, but the precise effect on net GHG emissions is unclear (Kuzyakov and Domanski, 2000). Changes in nutrient availability and pH, amongst other peat properties, can regulate GHG emissions, through processes mediated by microbial communities (Sjӧgersten et al, 2011; Troxler et al, 2012). This represents an important process in the context of land use change in tropical peatlands, as any process that alters plant communities may affect the concentration and composition of exudate inputs, as well as alter peat properties (Tonks et al, 2017)

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