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dc.contributor.author
Morales Oliveira, Juliano  
dc.contributor.author
Roig Junent, Fidel Alejandro  
dc.contributor.author
Depatta Pillar, Valério  
dc.date.available
2025-12-05T09:36:14Z  
dc.date.issued
2010-03  
dc.identifier.citation
Morales Oliveira, Juliano; Roig Junent, Fidel Alejandro; Depatta Pillar, Valério; Climatic signals in tree‐rings of Araucaria angustifolia in the southern Brazilian highlands; Wiley Blackwell Publishing, Inc; Austral Ecology; 35; 2; 3-2010; 134-147  
dc.identifier.issn
1442-9985  
dc.identifier.uri
http://hdl.handle.net/11336/276916  
dc.description.abstract
Araucaria angustifolia (Bertol.) O. Kuntze (Araucariaceae) is a Neotropical tree, widely distributed in subtropical mountain rain forests and nearby natural grasslands of Southern Brazil. This species produces annual growth rings, but its dendroclimatic potential is barely known. In the present paper, the long-term growth patterns of A. angustifolia were investigated using annual growth ring time series and association to climate over the lastcentury.Wood cores of A.angustifolia trees growing in forest and grassland habitats were obtained with an increment borer.The cores were surfaced, measured and cross-dated.The dated ring-width time series were standardized and submitted to correlation and principal component analysis to verify growth trends among sites and trees. Growth/climaterelationships were investigated using correlation and regression analyses, comparing the ordination axes scores to regional time series of precipitation and temperature. Due to anatomical irregularities, mainly partial rings, only 35 out of 60 trees were cross-dated. The correlation and ordination analyses showed common tree-growth trends within and between sites, indicative of a regional environmental force determining inter-annual cambial activity variation. Despite growing in distinct habitats and disturbance regimes, A. angustifolia trees share a common long-term growth pattern, which is significantly related to thermal conditions during the current and previous growing seasons. Moreover, site-specific characteristics may have influenced opposite growth responses and association to climate conditions between forest and grassland trees.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Wiley Blackwell Publishing, Inc  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
Araucaria forest  
dc.subject
Campos grassland  
dc.subject
dendrochronology  
dc.subject
fire  
dc.subject.classification
Investigación Climatológica  
dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente  
dc.subject.classification
CIENCIAS NATURALES Y EXACTAS  
dc.title
Climatic signals in tree‐rings of Araucaria angustifolia in the southern Brazilian highlands  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2025-12-04T12:54:04Z  
dc.journal.volume
35  
dc.journal.number
2  
dc.journal.pagination
134-147  
dc.journal.pais
Reino Unido  
dc.journal.ciudad
Londres  
dc.description.fil
Fil: Morales Oliveira, Juliano. Universidade Federal do Rio Grande do Sul; Brasil  
dc.description.fil
Fil: Roig Junent, Fidel Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina  
dc.description.fil
Fil: Depatta Pillar, Valério. Universidade Federal do Rio Grande do Sul; Brasil  
dc.journal.title
Austral Ecology  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/10.1111/j.1442-9993.2009.02018.x  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1111/j.1442-9993.2009.02018.x