Degradation-driven changes in fine root carbon stocks, productivity, mortality, and decomposition rates in a palm swamp peat forest of the Peruvian Amazon

Nelda Dezzeo; Julio Grandez-Rios; Christopher Martius; Kristell Hergoualc'h

doi:10.1186/s13021-021-00197-0

Degradation-driven changes in fine root carbon stocks, productivity, mortality, and decomposition rates in a palm swamp peat forest of the Peruvian Amazon

Carbon Balance Manag. 2021 Oct 29;16(1):33. doi: 10.1186/s13021-021-00197-0.

Authors

Nelda Dezzeo^{1

2}, Julio Grandez-Rios^{1

3}, Christopher Martius⁴, Kristell Hergoualc'h⁵

Affiliations

¹ Center for International Forestry Research (CIFOR), c/o Centro Internacional de la Papa (CIP), Av. La Molina 1895, La Molina, Apdo Postal 1558, 15024, Lima, Peru.
² Venezuelan Institute for Scientific Research (IVIC), Caracas, Venezuela.
³ Universidad Nacional de la Amazonia Peruana (UNAP), Loreto, Peru.
⁴ Center for International Forestry Research (CIFOR), Bonn, Germany.
⁵ Center for International Forestry Research (CIFOR), c/o Centro Internacional de la Papa (CIP), Av. La Molina 1895, La Molina, Apdo Postal 1558, 15024, Lima, Peru. k.hergoualch@cgiar.org.

Abstract

Background: Amazon palm swamp peatlands are major carbon (C) sinks and reservoirs. In Peru, this ecosystem is widely threatened owing to the recurrent practice of cutting Mauritia flexuosa palms for fruit harvesting. Such degradation could significantly damage peat deposits by altering C fluxes through fine root productivity, mortality, and decomposition rates which contribute to and regulate peat accumulation. Along a same peat formation, we studied an undegraded site (Intact), a moderately degraded site (mDeg) and a heavily degraded site (hDeg) over 11 months. Fine root C stocks and fluxes were monthly sampled by sequential coring. Concomitantly, fine root decomposition was investigated using litter bags. In the experimental design, fine root stocks and dynamics were assessed separately according to vegetation type (M. flexuosa palm and other tree species) and M. flexuosa age class. Furthermore, results obtained from individual palms and trees were site-scaled by using forest composition and structure.

Results: At the scale of individuals, fine root C biomass in M. flexuosa adults was higher at the mDeg site than at the Intact and hDeg sites, while in trees it was lowest at the hDeg site. Site-scale fine root biomass (Mg C ha^-1) was higher at the mDeg site (0.58 ± 0.05) than at the Intact (0.48 ± 0.05) and hDeg sites (0.32 ± 0.03). Site-scale annual fine root mortality rate was not significantly different between sites (3.4 ± 1.3, 2.0 ± 0.8, 1.5 ± 0.7 Mg C ha^-1 yr^-1 at the Intact, mDeg, and hDeg sites) while productivity (same unit) was lower at the hDeg site (1.5 ± 0.8) than at the Intact site (3.7 ± 1.2), the mDeg site being intermediate (2.3 ± 0.9). Decomposition was slow with 63.5-74.4% of mass remaining after 300 days and it was similar among sites and vegetation types.

Conclusions: The significant lower fine root C stock and annual productivity rate at the hDeg site than at the Intact site suggests a potential for strong degradation to disrupt peat accretion. These results stress the need for a sustainable management of these forests to maintain their C sink function.

Keywords: Belowground biomass; Decomposition; Necromass; Peatland; Peru; Tropical regions.

Abstract

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