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    Greenhouse gas emissions along a peat swamp forest degradation gradient in the Peruvian Amazon: soil moisture and palm roots effects

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    Authors
    Lent, Jeffrey van
    Hergoualc'h, Kristell
    Verchot, Louis V.
    Oenema, Oene
    Groenigen, Jan Willem van
    Date Issued
    2019-04
    Date Online
    2018-03
    Language
    en
    Type
    Journal Article
    Review status
    Peer Review
    ISI journal
    Accessibility
    Open Access
    Usage rights
    CC-BY-4.0
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    Citation
    van Lent, Jeffrey, Hergoualc’h, Kristell, Verchot, Louis, Oenema, Oene, van Groenigen, Jan Willem. (2018). Greenhouse gas emissions along a peat swamp forest degradation gradient in the Peruvian Amazon: soil moisture and palm roots effects. Mitigation and Adaptation Strategies for Global Change, 1–19 p.
    Permanent link to cite or share this item: https://hdl.handle.net/10568/93077
    DOI: https://doi.org/10.1007/s11027-018-9796-x
    Abstract/Description
    Tropical peatlands in the Peruvian Amazon exhibit high densities of Mauritia flexuosa palms, which are often cut instead of being climbed for collecting their fruits. This is an important type of forest degradation in the region that could lead to changes in the structure and composition of the forest, quality and quantity of inputs to the peat, soil properties, and greenhouse gas (GHG) fluxes. We studied peat and litterfall characteristics along a forest degradation gradient that included an intact site, a moderately degraded site, and a heavily degraded site. To understand underlying factors driving GHG emissions, we examined the response of in vitro soil microbial GHG emissions to soil moisture variation, and we tested the potential of pneumatophores to conduct GHGs in situ. The soil phosphorus and carbon content and carbon-to-nitrogen ratio as well as the litterfall nitrogen content and carbon-to-nitrogen ratio were significantly affected by forest degradation. Soils from the degraded sites consistently produced more carbon dioxide (CO2) than soils from the intact site during in vitro incubations. The response of CO2 production to changes in water-filled pore space (WFPS) followed a cubic polynomial relationship with maxima at 60–70% at the three sites. Methane (CH4) was produced in limited amounts and exclusively under water-saturated conditions. There was no significant response of nitrous oxide (N2O) emissions to WFPS variation. Lastly, the density of pneumatophore decreased drastically as the result of forest degradation and was positively correlated to in situ CH4 emissions. We conclude that recurrent M. flexuosa harvesting could result in a significant increase of in situ CO2 fluxes and a simultaneous decrease in CH4 emissions via pneumatophores. These changes might alter long-term carbon and GHG balances of the peat, and the role of these ecosystems for climate change mitigation, which stresses the need for their protection.
    CGIAR Author ORCID iDs
    Louis Verchothttps://orcid.org/0000-0001-8309-6754
    Other CGIAR Affiliations
    Climate Change, Agriculture and Food Security; Forests, Trees and Agroforestry
    AGROVOC Keywords
    greenhouse gases; gases de efecto invernadero; mauritia flexuosa; carbon dioxide; dioxido de carbono; nitrous oxide; óxido nitroso; methane; metano
    Regions
    Latin America; South America
    Organizations Affiliated to the Authors
    International Center for Tropical Agriculture
    Collections
    • CIAT Articles in Journals [2636]
    • CIAT Soils [227]
    • CIFOR publications [7743]

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