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dc.contributor.authorVan Straaten, Oliver-
dc.contributor.authorCorre, Marife D.-
dc.contributor.authorWolf, Katrin-
dc.contributor.authorTchienkoua, Martin-
dc.contributor.authorCuellar Bautista, José Eloy-
dc.contributor.authorMatthews, Robin-
dc.contributor.authorVeldkamp, Edzo-
dc.coverage.spatialIndonesia, Camerún y Perúes_PE
dc.date.accessioned2020-11-27T13:39:59Z-
dc.date.available2020-11-27T13:39:59Z-
dc.date.issued2015-08-11-
dc.identifier.citationVan Straaten, O.; Corre, M.; Wolf, K.; Tchienkoua, M.; Cuellar, E.; Matthews, R. & Veldkamp, E. (2015). Conversion of lowland tropical forests to tree cash crop plantations loses up to one-half of stored soil organic carbon. PNAS 112 (32) 9956-9960. doi: 10.1073/pnas.1504628112es_PE
dc.identifier.urihttp://repositorio.inia.gob.pe/handle/20.500.12955/1191-
dc.description.abstractTropical deforestation for the establishment of tree cash crop plantations causes significant alterations to soil organic carbon (SOC) dynamics. Despite this recognition, the current Intergovernmental Panel on Climate Change (IPCC) tier 1 method has a SOC change factor of 1 (no SOC loss) for conversion of forests to perennial tree crops, because of scarcity of SOC data. In this pantropic study, conducted in active deforestation regions of Indonesia, Cameroon, and Peru, we quantified the impact of forest conversion to oil palm (Elaeis guineensis), rubber (Hevea brasiliensis), and cacao (Theobroma cacao) agroforestry plantations on SOC stocks within 3-m depth in deeply weathered mineral soils. We also investigated the underlying biophysical controls regulating SOC stock changes. Using a space-for-time substitution approach, we compared SOC stocks from paired forests (n = 32) and adjacent plantations (n = 54). Our study showed that deforestation for tree plantations decreased SOC stocks by up to 50%. The key variable that predicted SOC changes across plantations was the amount of SOC present in the forest before conversion—the higher the initial SOC, the higher the loss. Decreases in SOC stocks were most pronounced in the topsoil, although older plantations showed considerable SOC losses below 1-m depth. Our results suggest that (i) the IPCC tier 1 method should be revised from its current SOC change factor of 1 to 0.6 ± 0.1 for oil palm and cacao agroforestry plantations and 0.8 ± 0.3 for rubber plantations in the humid tropics; and (ii) land use management policies should protect natural forests on carbon-rich mineral soils to minimize SOC losses.es_PE
dc.description.tableofcontentsStudy Description. Results. Discussion. Methods. Referenceses_PE
dc.formatapplication/pdfes_PE
dc.language.isoenges_PE
dc.publisherStanford Universityes_PE
dc.relation.ispartofPNAS August 11, 2015 112 (32) 9956-9960es_PE
dc.rightsinfo:eu-repo/semantics/openAccesses_PE
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/es_PE
dc.sourceInstituto Nacional de Innovación Agrariaes_PE
dc.source.uriRepositorio Institucional - INIAes_PE
dc.subjectSoil carbones_PE
dc.subjectLand-use changees_PE
dc.subjectOil palmes_PE
dc.subjectRubberes_PE
dc.subjectCacaoes_PE
dc.titleConversion of lowland tropical forests to tree cash crop plantations loses up to one-half of stored soil organic carbones_PE
dc.typeinfo:eu-repo/semantics/articlees_PE
dc.subject.ocdeForestales_PE
dc.identifier.journalPNASes_PE
dc.relation.publisherversionhttps://doi.org/10.1073/pnas.1504628112es_PE
dc.publisher.countryEstados Unidoses_PE
dc.identifier.doihttps://doi.org/10.1073/pnas.1504628112-
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