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dc.contributor.authorNavarrete, D
dc.contributor.authorSitch, S
dc.contributor.authorAragão, LEOC
dc.contributor.authorPedroni, L
dc.date.accessioned2018-10-25T09:27:16Z
dc.date.issued2016-03-01
dc.description.abstractStrategies to mitigate climate change by reducing deforestation and forest degradation (e.g. REDD+) require country- or region-specific information on temporal changes in forest carbon (C) pools to develop accurate emission factors. The soil C pool is one of the most important C reservoirs, but is rarely included in national forest reference emission levels due to a lack of data. Here, we present the soil organic C (SOC) dynamics along 20 years of forest-to-pasture conversion in two subregions with different management practices during pasture establishment in the Colombian Amazon: high-grazing intensity (HG) and low-grazing intensity (LG) subregions. We determined the pattern of SOC change resulting from the conversion from forest (C3 plants) to pasture (C4 plants) by analysing total SOC stocks and the natural abundance of the stable isotopes (13) C along two 20-year chronosequences identified in each subregion. We also analysed soil N stocks and the natural abundance of (15) N during pasture establishment. In general, total SOC stocks at 30 cm depth in the forest were similar for both subregions, with an average of 47.1 ± 1.8 Mg C ha(-1) in HG and 48.7 ± 3.1 Mg C ha(-1) in LG. However, 20 years after forest-to-pasture conversion SOC in HG decreased by 20%, whereas in LG SOC increased by 41%. This net SOC decrease in HG was due to a larger reduction in C3-derived input and to a comparatively smaller increase in C4-derived C input. In LG both C3- and C4-derived C input increased along the chronosequence. N stocks were generally similar in both subregions and soil N stock changes during pasture establishment were correlated with SOC changes. These results emphasize the importance of management practices involving low-grazing intensity in cattle activities to preserve SOC stocks and to reduce C emissions after land-cover change from forest to pasture in the Colombian Amazon.en_GB
dc.description.sponsorshipThis study was funded by AXA Research Fund (2012‐Doc‐University‐of‐Exeter‐NAVARRETE‐D).en_GB
dc.identifier.citationVol. 22 (10), pp. 3503 - 3517en_GB
dc.identifier.doi10.1111/gcb.13266
dc.identifier.urihttp://hdl.handle.net/10871/34438
dc.language.isoenen_GB
dc.publisherWileyen_GB
dc.relation.urlhttps://www.ncbi.nlm.nih.gov/pubmed/26929394en_GB
dc.rights© 2016 John Wiley & Sons Ltden_GB
dc.subjectColombian Amazonen_GB
dc.subjectREDD+en_GB
dc.subjectcarbon-13en_GB
dc.subjectemission factorsen_GB
dc.subjectforest reference emission levelen_GB
dc.subjectforest-to-pasture conversionen_GB
dc.subjectgrazing intensityen_GB
dc.subjectsoil organic carbon poolen_GB
dc.subjectAnimalsen_GB
dc.subjectCarbonen_GB
dc.subjectCattleen_GB
dc.subjectClimate Changeen_GB
dc.subjectConservation of Natural Resourcesen_GB
dc.subjectForestsen_GB
dc.subjectSoilen_GB
dc.titleConversion from forests to pastures in the Colombian Amazon leads to contrasting soil carbon dynamics depending on land management practicesen_GB
dc.typeArticleen_GB
dc.date.available2018-10-25T09:27:16Z
exeter.place-of-publicationEnglanden_GB
dc.descriptionThis is the author accepted manuscript. The final version is available from Wiley via the DOI in this recorden_GB
dc.identifier.journalGlobal Change Biologyen_GB


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