4.7 Article

Insight into Canary Island pine physiology provided by stable isotope patterns of water and plant tissues along an altitudinal gradient

Journal

TREE PHYSIOLOGY
Volume 41, Issue 9, Pages 1611-1626

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/treephys/tpab046

Keywords

Canary Islands; cloud forest; drought; Pinus canariensis; relative humidity; stable isotopes; tree rings; vapor pressure deficit

Categories

Funding

  1. fellowship Emilio Gonzalez Esparcia
  2. Ramon Areces Foundation [BEVP31A6157]
  3. Swiss National Science Foundation [SNF 200021_175888, PZ00P2_179978]
  4. Czech Science Foundation [20-05840Y]
  5. Czech Ministry of Education, Youth and Sports [INTER-EXCELLENCE LTAUSA19137]
  6. project of the Czech Academy of Sciences [RVO 67985939]
  7. Swiss National Science Foundation (SNF) [PZ00P2_179978] Funding Source: Swiss National Science Foundation (SNF)

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The study analyzed the physiological behavior of Pinus canariensis at different altitudes on La Palma in the Canary Islands, revealing that increasing altitude leads to higher oxygen isotope ratios in needle water and tree-ring cellulose, indicating specific tree responses to humidity. Sites influenced by fog and those without fog showed similar carbon isotope values, suggesting photosynthetic activity is limited by stomatal closure and irradiance at certain periods. Additionally, seasonal differences in water uptake and meteorological conditions were found to cause isotopic variations in latewood, with soil water availability and air humidity as the main drivers of pine physiological behavior across altitudinal gradients in the Canary Islands.
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 delta O-18 trend in source water that was overridden by an increasing delta O-18 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 delta C-13 values, suggesting photosynthetic activity to be limited by stomatal closure and irradiance at certain periods. In addition, we observed an O-18-depletion (fog-free and timberline sites) and C-13-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 delta O-18 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 delta O-18 when applying standard leaf water delta O-18 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.

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