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dc.contributor.authorLloyd, Jon-
dc.contributor.authornull, Tomas-
dc.contributor.authorSchrodt, Franziska-
dc.contributor.authorIshida, Francoise Yoko-
dc.contributor.authorFeldpausch, Ted R.-
dc.contributor.authorSaiz, Gustavo-
dc.contributor.authorQuesada, Carlos Alberto-
dc.contributor.authorSchwarz, Michael-
dc.contributor.authorTorello-Raventos, Mireia-
dc.contributor.authorGilpin, Martin-
dc.contributor.authorMarimon, Beatriz Schwantes-
dc.contributor.authorMarimon Júnior, Ben Hur-
dc.contributor.authorRatter, James Alexander-
dc.contributor.authorGrace, John-
dc.contributor.authorNardoto, G. B.-
dc.contributor.authorVeenendaal, Elmar M.-
dc.contributor.authorArroyo, Luzmila P.-
dc.contributor.authorVillarroel, Daniel-
dc.contributor.authorKilleen, Timothy J.-
dc.contributor.authorSteininger, Marc K.-
dc.contributor.authorPhillips, Oliver L.-
dc.date.accessioned2020-05-07T13:47:21Z-
dc.date.available2020-05-07T13:47:21Z-
dc.date.issued2015-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/14911-
dc.description.abstractSampling along a precipitation gradient in tropical South America extending from ca. 0.8 to 2.0 m ag-1, savanna soils had consistently lower exchangeable cation concentrations and higher C/N ratios than nearby forest plots. These soil differences were also reflected in canopy averaged leaf traits with savanna trees typically having higher leaf mass per unit area but lower mass-based nitrogen (Nm) and potassium (Km). Both Nm and Km also increased with declining mean annual precipitation (PA), but most area-based leaf traits such as leaf photosynthetic capacity showed no systematic variation with PA or vegetation type. Despite this invariance, when taken in conjunction with other measures such as mean canopy height, area-based soil exchangeable potassium content, [K]sa , proved to be an excellent predictor of several photosynthetic properties (including 13C isotope discrimination). Moreover, when considered in a multivariate context with PA and soil plant available water storage capacity (θP) as covariates, [K]sa also proved to be an excellent predictor of stand-level canopy area, providing drastically improved fits as compared to models considering just PA and/or θP. Neither calcium, nor magnesium, nor soil pH could substitute for potassium when tested as alternative model predictors (ΔAIC > 10). Nor for any model could simple soil texture metrics such as sand or clay content substitute for either [K]sa or θP. Taken in conjunction with recent work in Africa and the forests of the Amazon Basin, this suggests-in combination with some newly conceptualised interacting effects of PA and θP also presented here-a critical role for potassium as a modulator of tropical vegetation structure and function. © 2015 Author(s).en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 12, Número 22, Pags. 6529-6571pt_BR
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Brazil*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/br/*
dc.subjectCarbonen
dc.subjectEcotoneen
dc.subjectForest Canopyen
dc.subjectLeaf Morphologyen
dc.subjectMagnesiumen
dc.subjectNitrogenen
dc.subjectPhotosynthesisen
dc.subjectPhysiological Responseen
dc.subjectPotassiumen
dc.subjectPrecipitation (climatology)en
dc.subjectSavannaen
dc.subjectSoil Textureen
dc.subjectTropical Regionen
dc.subjectVegetation Structureen
dc.subjectWoody Planten
dc.subjectAfricaen
dc.subjectAmazon Basinen
dc.titleEdaphic, structural and physiological contrasts across Amazon Basin forest-savanna ecotones suggest a role for potassium as a key modulator of tropical woody vegetation structure and functionen
dc.typeArtigopt_BR
dc.identifier.doi10.5194/bg-12-6529-2015-
dc.publisher.journalBiogeosciencespt_BR
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