Insight into Canary Island pine physiology provided by stable isotope patterns of water and plant tissues along an altitudinal gradient
Jazyk angličtina Země Kanada Médium print
Typ dokumentu časopisecké články, práce podpořená grantem
PubMed
33824979
DOI
10.1093/treephys/tpab046
PII: 6212644
Knihovny.cz E-zdroje
- Klíčová slova
- Pinus canariensis, Canary Islands, cloud forest, drought, relative humidity, stable isotopes, tree rings, vapor pressure deficit,
- MeSH
- borovice * MeSH
- ekosystém MeSH
- izotopy kyslíku analýza MeSH
- izotopy uhlíku analýza MeSH
- stromy MeSH
- voda * MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Geografické názvy
- Španělsko MeSH
- Názvy látek
- izotopy kyslíku MeSH
- izotopy uhlíku MeSH
- Oxygen-18 MeSH Prohlížeč
- voda * MeSH
The Canary Islands, an archipelago east of Morocco's Atlantic coast, present steep altitudinal gradients covering various climatic zones from hot deserts to subalpine Mediterranean, passing through fog-influenced cloud forests. Unlike the majority of the Canarian flora, Pinus canariensis C. Sm. ex DC. in Buch grow along most of these gradients, allowing the study of plant functioning in contrasting ecosystems. Here we assess the water sources (precipitation, fog) of P. canariensis and its physiological behavior in its different natural environments. We analyzed carbon and oxygen isotope ratios of water and organics from atmosphere, soil and different plant organs and tissues (including 10-year annual time series of tree-ring cellulose) of six sites from 480 to 1990 m above sea level on the Canary Island La Palma. We found a decreasing δ18O trend in source water that was overridden by an increasing δ18O trend in needle water, leaf assimilates and tree-ring cellulose with increasing altitude, suggesting site-specific tree physiological responses to relative humidity. Fog-influenced and fog-free sites showed similar δ13C values, suggesting photosynthetic activity to be limited by stomatal closure and irradiance at certain periods. In addition, we observed an 18O-depletion (fog-free and timberline sites) and 13C-depletion (fog-influenced and fog-free sites) in latewood compared with earlywood caused by seasonal differences in: (i) water uptake (i.e., deeper ground water during summer drought, fog water frequency and interception) and (ii) meteorological conditions (stem radial growth and latewood δ18O correlated with winter precipitation). In addition, we found evidence for foliar water uptake and strong isotopic gradients along the pine needle axis in water and assimilates. These gradients are likely the reason for an unexpected underestimation of pine needle water δ18O when applying standard leaf water δ18O models. Our results indicate that soil water availability and air humidity conditions are the main drivers of the physiological behavior of pine along the Canary Island's altitudinal gradients.
Departamento de Sistemas y Recursos Naturales Universidad Politécnica de Madrid 28034 Madrid Spain
Institute of Botany Czech Academy of Science 25243 Průhonice Czech Republic
Swiss Federal Institute for Forest Snow and Landscape Research WSL 8903 Birmensdorf Switzerland
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