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dc.contributor.authorRoig Junent, Fidel [Univ Mayor, Fac Ciencias, Hemera Ctr Observac Tierra, Santiago, Chile]es_CL
dc.contributor.authorMacedo, Tahysa Motaes_CL
dc.contributor.authorBarros, Claudia Francaes_CL
dc.contributor.authorde Lima, Haroldo Cavalcantees_CL
dc.contributor.authordas Neves Brandes, Arno Fritzes_CL
dc.contributor.authorda Costa, Warlen Silvaes_CL
dc.contributor.authorCosta, Cecilia Goncalveses_CL
dc.date.accessioned2020-04-12T14:11:55Z
dc.date.accessioned2020-04-14T15:37:54Z
dc.date.available2020-04-12T14:11:55Z
dc.date.available2020-04-14T15:37:54Z
dc.date.issued2020es_CL
dc.identifier.citationMacedo, T. M., Barros, C. F., de Lima, H. C., das Neves Brandes, A. F., da Costa, W. S., Costa, C. G., & Roig, F. (2019). Climate signals in tree rings of Paubrasilia echinata (Leguminosae-Caesalpinioidea) from the Atlantic Forest of Brazil. Trees, 1-11.es_CL
dc.identifier.issn0931-1890es_CL
dc.identifier.issn1432-2285es_CL
dc.identifier.urihttps://doi.org/10.1007/s00468-019-01919-1es_CL
dc.identifier.urihttp://repositorio.umayor.cl/xmlui/handle/sibum/6556
dc.description.abstractKey message Tree-ring chronologies were built for wild and cultivated Paubrasilia echinata, a presently endangered species. Significantly P. echinata showed measurably different growth patterns related to the environment where wild and cultivated trees have grown. Paubrasilia echinata once grew so abundantly along the tropical coast of South America that the names given to the tree by early Europeans colonists-Bresil, Brasil, Brazil-became synonymous with an entire geography. Today, despite restoration and protection efforts, the species remains under threat of extinction throughout Brazil's Atlantic Forest. Considering the past overexploitation and ongoing climate changes, the future of P. echinata significantly depends upon human understanding of the species' growth dynamics and growth-climate relations. Therefore, this work aims to: (1) demonstrate the feasibility of calendar dating P. echinata tree rings; (2) build chronologies by analyzing its growth rings; and (3) establish with detail the specific influence of climate on annual radial xylem production. Differences in vessel and axial parenchyma frequency, local distended rays and marginal parenchyma were the wood anatomical markers used to distinguish boundaries between adjacent rings so that dendrochronological methods could be applied. For climate-growth responses, we developed tree-ring width chronologies from wild and cultivated trees. Results revealed that seasonal rainfall is the most important factor influencing P. echinata growth. More specifically, positive correlation was observed between the tree-ring chronology of wild trees and precipitation during the rainy months of the growing season, while the tree-ring chronology of cultivated trees correlated negatively with precipitation in months before the growth period. Wild trees showed increment growth rates lower than planted trees. Rainfall's observed effect on P. echinata is, of course, not surprising. However, our results contribute a detailed quantitative record of that effect, which expands the body of ecological knowledge regarding P. echinata necessary for ongoing conservation efforts under current and future human-caused climate change.es_CL
dc.description.sponsorshipCNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)National Council for Scientific and Technological Development (CNPq); PPBIO (Programa de Pesquisa em Biodiversidade); FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro)Carlos Chagas Filho Foundation for Research Support of the State of Rio de Janeiro (FAPERJ)es_CL
dc.description.sponsorshipWe thank the Laboratorio de Dendrocronologia e Historia Ambiental, Instituto Argentino de Nivologia, Glaciologia y Ciencias Ambientales (IANIGLA), Centro Cientifico Tecnologico CONICET-Mendoza, Argentina, for technical support. We also thank the Laboratorio de Botanica Estrutural, the Instituto de Pesquisas Jardim Botanico do Rio de Janeiro, and the Museu Nacional do Rio de Janeiro-UFRJ. We acknowledge anonymous referees for suggestions that improved the manuscript, Christopher Lesser and David Martin for English language review, as well as Bruna Luna, PhD for their valuable fieldwork. Finally, we thank CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) for the PDSE, as well as CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico), PPBIO (Programa de Pesquisa em Biodiversidade), and FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro) for the research fellowship grant.es_CL
dc.language.isoenes_CL
dc.publisherSPRINGER HEIDELBERGes_CL
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile
dc.sourceTrees-Struct. Funct., 2020. 34: p. 337-347
dc.subjectForestryes_CL
dc.titleClimate signals in tree rings of Paubrasilia echinata (Leguminosae-Caesalpinioidea) from the Atlantic Forest of Braziles_CL
dc.typeArticle; Early Accesses_CL
umayor.facultadCIENCIAS
umayor.politicas.sherpa/romeoRoMEO green journal (Se puede archivar el pre-print y el post-print o versión de editor/PDF). Disponible en: http://sherpa.ac.uk/romeo/index.phpes_CL
umayor.indexadoWOS:000492361800001es_CL
umayor.indexadoSIN PMIDes_CL
dc.identifier.doiDOI: 10.1007/s00468-019-01919-1es_CL]
umayor.indicadores.wos-(cuartil)Q2es_CL
umayor.indicadores.scopus-(scimago-sjr)SCIMAGO/ INDICE H: 77 Hes_CL


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