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dc.contributor.authorTeh, Y.A.
dc.contributor.authorDiem, T.
dc.contributor.authorJones, S.
dc.contributor.authorHuaraca Quispe, L.P.
dc.contributor.authorBaggs, E.
dc.contributor.authorMorley, N.
dc.contributor.authorRichards, M.
dc.contributor.authorSmith, P.
dc.contributor.authorMeir, P.
dc.date.accessioned2014-07-09T10:01:01Z
dc.date.available2014-07-09T10:01:01Z
dc.date.issued2014-04-25
dc.identifier.citationTeh , Y A , Diem , T , Jones , S , Huaraca Quispe , L P , Baggs , E , Morley , N , Richards , M , Smith , P & Meir , P 2014 , ' Methane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andes ' , Biogeosciences , vol. 11 , no. 8 , pp. 2325-2339 . https://doi.org/10.5194/bg-11-2325-2014en
dc.identifier.issn1726-4170
dc.identifier.otherPURE: 130513184
dc.identifier.otherPURE UUID: 0b3c7613-58a9-4ea2-8764-401dbf66534b
dc.identifier.otherScopus: 84899473747
dc.identifier.otherWOS: 000335374200015
dc.identifier.urihttp://hdl.handle.net/10023/4977
dc.descriptionThe authors acknowledge the agencies that funded this research; the UK Natural Environment Research Council (NERC; joint grant references NE/H006583, NE/H007849 and NE/H006753) and the Norwegian Agency for Development Cooperation (Norad; via a sub-contract to Yit Arn Teh managed by the Amazon Conservation Association). Pete Smith is a Royal Society Wolfson Research Merit Award holder and Patrick Meir is supported by an Australian Research Council Fellowship (FT110100457).en
dc.description.abstractRemote sensing and inverse modelling studies indicate that the tropics emit more CH4 and N2O than predicted by bottom-up emissions inventories, suggesting that terrestrial sources are stronger or more numerous than previously thought. Tropical uplands are a potentially large and important source of CH4 and N2O often overlooked by past empirical and modelling studies. To address this knowledge gap, we investigated spatial, temporal and environmental trends in soil CH4 and N2O fluxes across a long elevation gradient (600-3700 m a.s.l.) in the Kosñipata Valley, in the southern Peruvian Andes, that experiences seasonal fluctuations in rainfall. The aim of this work was to produce preliminary estimates of soil CH4 and N2O fluxes from representative habitats within this region, and to identify the proximate controls on soil CH4 and N2O dynamics. Area-weighted flux calculations indicated that ecosystems across this altitudinal gradient were both atmospheric sources and sinks of CH4 on an annual basis. Montane grasslands (3200–3700 m a.s.l.) were strong atmospheric sources, emitting 56.94 ± 7.81 kg CH4-C haĝ̂'1 yrĝ̂'1. Upper montane forest (2200-3200 m a.s.l.) and lower montane forest (1200-2200 m a.s.l.) were net atmospheric sinks (ĝ̂'2.99 ± 0.29 and ĝ̂'2.34 ± 0.29 kg CH4-C haĝ̂'1 yrĝ̂'1, respectively); while premontane forests (600-1200 m a.s.l.) fluctuated between source or sink depending on the season (wet season: 1.86 ± 1.50 kg CH4-C haĝ̂'1 yrĝ̂'1; dry season: ĝ̂'1.17 ± 0.40 kg CH4-C haĝ̂'1 yr−1). Analysis of spatial, temporal and environmental trends in soil CH4 flux across the study site suggest that soil redox was a dominant control on net soil CH4 flux. Soil CH4 emissions were greatest from habitats, landforms and during times of year when soils were suboxic, and soil CH4 efflux was inversely correlated with soil O2 concentration (Spearman's ρ Combining double low line −0.45,P< 0.0001) and positively correlated with water-filled pore space (Spearman's ρ Combining double low line 0.63,P<0.0001). Ecosystems across the region were net atmospheric N2O sources. Soil N2O fluxes declined with increasing elevation; area-weighted flux calculations indicated that N2O emissions from premontane forest, lower montane forest, upper montane forest and montane grasslands averaged 2.23 ± 1.31, 1.68 ± 0.44, 0.44 ± 0.47 and 0.15 ± 1.10 kg N2O-N haĝ̂'1 yrĝ̂'1, respectively. Soil N2O fluxes from premontane and lower montane forests exceeded prior model predictions for the region. Comprehensive investigation of field and laboratory data collected in this study suggest that soil N2O fluxes from this region were primarily driven by denitrification; that nitrate (NO3−) availability was the principal constraint on soil N2O fluxes; and that soil moisture and water-filled porosity played a secondary role in modulating N2O emissions. Any current and future changes in N management or anthropogenic N deposition may cause shifts in net soil N2O fluxes from these tropical montane ecosystems, further enhancing this emission source.
dc.format.extent15
dc.language.isoeng
dc.relation.ispartofBiogeosciencesen
dc.rights© Author(s) 2014. CC Attribution 3.0 License. http://creativecommons.org/licenses/by/3.0/en
dc.subjectG Geography (General)en
dc.subject.lccG1en
dc.titleMethane and nitrous oxide fluxes across an elevation gradient in the tropical Peruvian Andesen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.Geography & Sustainable Developmenten
dc.contributor.institutionUniversity of St Andrews.Earth and Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.School of Biologyen
dc.contributor.institutionUniversity of St Andrews.School of Managementen
dc.identifier.doihttps://doi.org/10.5194/bg-11-2325-2014
dc.description.statusPeer revieweden
dc.identifier.urlhttp://www.biogeosciences.net/11/2325/2014/en


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