Structural and functional changes in Nothofagus pumilio forests along an altitudinal gradient in Tierra del Fuego, Argentina.
By M. Barrera, J. Frangi, L. L. Richter, Marcelo H. Perdomo, L. B. Pinedo. 2000
133 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/e3f9902cd63cc48772746dbc7dad1faae78979cd
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In Atmospheric Science
In Global and Planetary Change
- Guangsheng Zhou
- A. Sparrow
- A. Premoli
- C. Brewer
- Peter Vesk
- M. Westoby
- Peter Clarke
- Kirsten J. E. Knox
In Nature and Landscape Conservation
Citations in the corpus
- Environmental v. genetically driven variation in ecophysiological traits of Nothofagus pumilio from contrasting elevations (2007, background): “Variable physical conditions characterise N. pumilio forests along these gradients, including decreases in soil temperature and the period with frost-free soils, as well as increased total annual precipitation and percentage of snowfall at high elevation (Barrera et al. 2000).”
- Photosynthetic plasticity of Nothofagus pumilio seedlings to light intensity and soil moisture (2007, result): “The leaf phenology in the experimental conditions was comparable to the natural growing conditions (Rusch, 1993; Barrera et al., 2000), except for leaf unfolding, which was more concentrated at the beginning of the summer in the natural forests.”
- Distribution, species diversity and life-form spectra of plant communities along an altitudinal gradient in the northern slopes of Qilianshan Mountains, Gansu, China (2003, background): “Various studies show that elevation provides a complex gradient where ecological factors vary in different spatial scales, and plants respond to different combinations of ecological factors (Barrera et al. 2000).”
- Multi‐stemmed trees in montane rain forests: their frequency and demography in relation to elevation, soil nutrients and disturbance (2009, background): “This could be determined along latitudinal gradients and should consider forests where cold-temperature extremes are greater than those encountered in New Zealand forests (e.g. rain forests at high latitudes in South America, Barrera et al. 2000).”