Abstract
Aims
In tropical rainforests, soil respiration accounts for the major part of ecosystem respiration, yet a deep understanding of the influence of forest type and species composition is still lacking. We therefore selected patches of the rainforest in the Central Congo basin differing in their species composition, some patches under the Scorodophloeus zenkeri Harms mixed forests (MIF) and others in the Gilbertiodendron dewevrei (De Wild.) J.Léonard monodominant forests (MOF). We measured daily soil respiration over a one-year period.
Methods
By fitting a simple conceptual model of soil respiration, including fine root biomass, soil organic C stocks and ground climate measurements (soil moisture and temperature), we attempted to distinguish autotrophic and heterotrophic soil respiration, and to better understand the drivers behind total soil respiration.
Results
On an annual basis, soil respiration was 10% higher under MOF (22.10 Mg C ha−1 y−1) compared to MIF (20.01 Mg C ha−1 y−1) (p < 10−3). While the estimated autotrophic and heterotrophic soil respiration contributed about equally to soil respiration in MOF, autotrophic soil respiration slightly dominated (59%) in MIF. In both forests, the combined contribution of litterfall inputs and fine roots productivity was lower than the heterotrophic flux, with the largest difference observed under MOF (−6.16 Mg C ha−1 year−1) compared to MIF (−2.62 Mg C ha−1 year−1). The sensitivity analysis of the model showed that the higher heterotrophic soil respiration under MOF was driven by the twofold C accumulation in MOF topsoil compared to MIF. Soil moisture was a major driver of temporal changes in soil respiration, but hardly impacted the differences in annual soil respiration between forests.
Conclusion
While the difference in SOC accumulation between forests was driven by the low nutrient to C ratios of Gilbertiodendron dewevrei tissues, additional research is needed to identify the causes behind the unbalanced C budget.
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Acknowledgments
Benoît Cassart obtained a PhD grant from the ‘Fonds National de la Recherche Scientifique’ (FNRS-FRIA), and received additional support for field work and laboratory analyses from a joint WBI-ERAIFT grant. Albert Angbonga Basia was funded by the ‘AFORCO – Appui à l’organisation d’un master en aménagement forestier pour le renforcement des capacités des chercheurs congolais en vue de la relance socio-économique de la République Démocratique du Congo’ project, funded by the ‘Commission Universitaire au Développement’ (CUD, ARES-CCD) and coordinated by Prof. Jan Bogaert (ULiège – Gembloux Agro-Bio Tech). All authors thank the numerous persons who contributed to the field work in DRC. They are also greateful to Karine Henin who carried out most of the chemical analyses. We would also like to thank Bernard Longdoz for his helpful comments on an earlier version of this manuscript. Finally, we are debtful to the Section Editor as well as to two anonymous reviewers for their constructive comments that greatly improved a previous version of the manuscript.
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BC and QP conceived and designed the experiments. ABA and BC performed the experiments. BC, MJ and QP analysed the data
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Cassart, B., Angbonga Basia, A., Jonard, M. et al. Functional traits drive the difference in soil respiration between Gilbertiodendron dewevrei monodominant forests patches and Scorodophloeus zenkeri mixed forests patches in the Central Congo basin.. Plant Soil 460, 313–331 (2021). https://doi.org/10.1007/s11104-020-04808-6
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DOI: https://doi.org/10.1007/s11104-020-04808-6