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dc.contributor.authorLent, Jeffrey vanen_US
dc.contributor.authorHergoualc'h, Kristellen_US
dc.contributor.authorVerchot, Louis V.en_US
dc.contributor.authorOenema, Oeneen_US
dc.contributor.authorGroenigen, Jan Willem vanen_US
dc.date.accessioned2018-06-06T13:28:13Zen_US
dc.date.available2018-06-06T13:28:13Zen_US
dc.identifier.urihttps://hdl.handle.net/10568/93077en_US
dc.titleGreenhouse gas emissions along a peat swamp forest degradation gradient in the Peruvian Amazon: soil moisture and palm roots effectsen_US
dcterms.abstractTropical 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.en_US
dcterms.accessRightsOpen Accessen_US
dcterms.available2018-03-21en_US
dcterms.bibliographicCitationvan 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.en_US
dcterms.extent1-19 p.en_US
dcterms.issued2019-04en_US
dcterms.languageenen_US
dcterms.licenseCC-BY-4.0en_US
dcterms.publisherSpringer Science and Business Media LLCen_US
dcterms.subjectgreenhouse gasesen_US
dcterms.subjectgases de efecto invernaderoen_US
dcterms.subjectmauritia flexuosaen_US
dcterms.subjectcarbon dioxideen_US
dcterms.subjectdioxido de carbonoen_US
dcterms.subjectnitrous oxideen_US
dcterms.subjectóxido nitrosoen_US
dcterms.subjectmethaneen_US
dcterms.subjectmetanoen_US
dcterms.typeJournal Articleen_US
cg.contributor.affiliationInternational Center for Tropical Agricultureen_US
cg.identifier.doihttps://doi.org/10.1007/s11027-018-9796-xen_US
cg.isijournalISI Journalen_US
cg.coverage.regionLatin Americaen_US
cg.coverage.regionSouth Americaen_US
cg.contributor.crpClimate Change, Agriculture and Food Securityen_US
cg.contributor.crpForests, Trees and Agroforestryen_US
cg.creator.identifierLouis Verchot: 0000-0001-8309-6754en_US
cg.reviewStatusPeer Reviewen_US
cg.howPublishedFormally Publisheden_US
cg.journalMitigation and Adaptation Strategies for Global Changeen_US
cg.issn1381-2386en_US


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