Wood density variation across an Andes-to-Amazon elevational gradient

dc.contributor.affiliationPontificia Universidad Católica del Perú. Departamento de Ciencias
dc.contributor.authorFarfan-Rios, W.
dc.contributor.authorSaatchi, S.
dc.contributor.authorOliveras Menor, I.
dc.contributor.authorMalhi, Y.
dc.contributor.authorRobinson, C.M.
dc.contributor.authorPhillips, O.L.
dc.contributor.authorNina-Quispe, A.
dc.contributor.authorGibaja, J.A.
dc.contributor.authorCuba, I.
dc.contributor.authorGarcía-Cabrera, K.
dc.contributor.authorSalinas Revilla, N.
dc.contributor.authorTerborgh, J.
dc.contributor.authorPitman, N.
dc.contributor.authorVasquez, R.
dc.contributor.authorMonteagudo-Mendoza, A.
dc.contributor.authorNunez Vargas, P.;
dc.date.accessioned2026-03-13T16:57:49Z
dc.date.issued2025
dc.description.abstractAbstract Understanding how functional traits are related to species diversity and ecosystem properties is a central goal of ecology. Wood density is a trait that integrates many aspects of plant form and function and is highly variable among species. Previous studies of wood density across elevational gradients have been based on limited sampling and have reported declines with increasing elevation, though even this simple pattern remains unknown, much less its underlying functional and evolutionary relationships. Here, we use one of the longest and most speciose elevational gradients in the world, extending from the Andean tree line to the Amazon basin, to test the extent to which elevation, species composition, phylogenetic affinity and forest structure determine variation in wood density. Using field‐collected wood samples and global databases, we assigned wood density to 1231 species and 31,330 stems across 41 (47.5 ha) mature forest plots arrayed across a 3500‐m vertical gradient. Our results show that mean wood density, either weighted by abundance, basal area or species, was highly variable but tended to decline from low to middle elevations and increase again from mid‐elevations to the tree line. As a result of this non‐linearity, forests at the Andean tree line had higher wood density than their lowland Amazon counterparts. We observed an abrupt transition in wood density at the lower limit of persistent cloud formation (cloud base), where the lowest wood density values were found. The decline of wood density is attributed to a significant shift in life forms, with an abundance of tree ferns at middle elevations and a higher probability of landslides and disturbances favouring a suite of traits associated with low wood density, such as softer wood and higher elasticity. Species turnover explained most of the among‐species variation across the gradient, with elevation having no consistent effect on within‐species variation in wood density. Together, both gradual compositional changes and sharp local changes in the importance of non‐dicot life forms, such as arborescent ferns and palms, define patterns of forest‐level carbon density, with wood density per se controlling ecosystem properties, such as carbon flux, across the Andes‐to‐Amazon elevational gradient.
dc.description.sponsorshipFunding: This paper is a product of the Andes Biodiversity and Ecosystem Research Group (ABERG; http://www.andesconservation.org/ ) with contributions from affiliated networks RAINFOR, GEM and the ForestPlots.net data management utility for permanent plots. Data included in this study are the result of an extraordinary effort by a large team in Peru, including from the Universidad Nacional de San Antonio Abad de Cusco. Special thanks go to Luis Imunda and Erickson Urquiaga for their assistance in the field sampling campaigns. SERFOR, SERNANP and personnel of Manu National Park Peru assisted with logistics and permission to work in the protected area. Pantiacolla Tours and the Amazon Conservation Association provided logistical support. Support came from the Gordon and Betty Moore Foundation's Andes to Amazon initiative and the US National Science Foundation (NSF) DEB 0743666 and NSF Long-Term Research in Environmental Biology (LTREB) 1754647. The research in this study was also supported by the National Aeronautics and Space Administration (NASA) Terrestrial Ecology Program grant # NNH08ZDA001N-TE/08-TE08-0037. Support for RAINFOR and ForestPlots.net plot monitoring in Peru has come from a European Research Council (ERC) Advanced Grant (T-FORCES, ‘Tropical Forests in the Changing Earth System', 291585), Natural Environment Research Council grants (including NE/F005806/1, NE/D005590/1, NE/N012542/1 and AMSINK, NE/X014347/1) and the Gordon and Betty Moore Foundation. This manuscript is an output of ForestPlots.net Research Project 77. "Expanding the frontiers of our understanding of forest responses to climate change across the Andean-to-Amazon environmental gradient: A continental-scale approach".; Funding text 2: This paper is a product of the Andes Biodiversity and Ecosystem Research Group (ABERG; http://www.andesconservation.org/) with contributions from affiliated networks RAINFOR, GEM and the ForestPlots.net data management utility for permanent plots. Data included in this study are the result of an extraordinary effort by a large team in Peru, including from the Universidad Nacional de San Antonio Abad de Cusco. Special thanks go to Luis Imunda and Erickson Urquiaga for their assistance in the field sampling campaigns. SERFOR, SERNANP and personnel of Manu National Park Peru assisted with logistics and permission to work in the protected area. Pantiacolla Tours and the Amazon Conservation Association provided logistical support. Support came from the Gordon and Betty Moore Foundation's Andes to Amazon initiative and the US National Science Foundation (NSF) DEB 0743666 and NSF Long-Term Research in Environmental Biology (LTREB) 1754647. The research in this study was also supported by the National Aeronautics and Space Administration (NASA) Terrestrial Ecology Program grant # NNH08ZDA001N-TE/08-TE08-0037. Support for RAINFOR and ForestPlots.net plot monitoring in Peru has come from a European Research Council (ERC) Advanced Grant (T-FORCES, ‘Tropical Forests in the Changing Earth System', 291585), Natural Environment Research Council grants (including NE/F005806/1, NE/D005590/1, NE/N012542/1 and AMSINK, NE/X014347/1) and the Gordon and Betty Moore Foundation. This manuscript is an output of ForestPlots.net Research Project 77. "Expanding the frontiers of our understanding of forest responses to climate change across the Andean-to-Amazon environmental gradient: A continental-scale approach".; Funding text 3: US National Science Foundation (NSF) Grant Number: DEB 0743666 and NSF Long-Term Research in Environmental Biology (LTREB) Grant Number: 1754647. National Aeronautics and Space Administration (NASA) Terrestrial Ecology Program Grant Number: NNH08ZDA001N-TE/08-TE08-0037. European Research Council (ERC) Advanced Grant Number: 291585. Natural Environment Research Council Grant Number: NE/F005806/1, NE/D005590/1, NE/N012542/1 and AMSINK, NE/X014347/1.
dc.identifier.doihttps://doi.org/10.1111/1365-2745.70100
dc.identifier.urihttp://hdl.handle.net/20.500.14657/205679
dc.language.isoeng
dc.publisherJohn Wiley and Sons
dc.relation.ispartofurn:issn:0022-0477
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.sourceJournal of Ecology; Vol. 113, Núm. 9 (2025)
dc.subjectBasal area
dc.subjectAmazon rainforest
dc.subjectAbundance (ecology)
dc.subjectTree line
dc.subjectTrait
dc.subjectEnvironmental gradient
dc.subjectEcosystem
dc.subjectCloud forest
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.06.00
dc.titleWood density variation across an Andes-to-Amazon elevational gradient
dc.typehttp://purl.org/coar/resource_type/c_6501
dc.type.otherArtículo
dc.type.versionhttps://vocabularies.coar-repositories.org/version_types/c_970fb48d4fbd8a85/

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