Increased water-use efficiency during the 20th century did not translate into enhanced tree growth

Authors

  • Josep Peñuelas,

    Corresponding author
    1. Global Ecology Unit CREAF-CEAB-CSIC, Center for Ecological Research and Forestry Applications, Facultat de Ciències, Universitat Autònoma de Barcelona, 08193 Bellaterra, Catalonia, Spain
      Josep Peñuelas, Global Ecology Unit CREAF-CEAB-CSIC, Center for Ecological Research and Forestry Applications, Facultat de Ciències, Universitat Autònoma de Barcelona, 08193 Bellaterra, Catalonia, Spain. E-mail: josep.penuelas@uab.cat
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  • Josep G Canadell,

    1. Global Carbon Project, CSIRO Marine and Atmospheric Research, Canberra, Australia
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  • Romà Ogaya

    1. Global Ecology Unit CREAF-CEAB-CSIC, Center for Ecological Research and Forestry Applications, Facultat de Ciències, Universitat Autònoma de Barcelona, 08193 Bellaterra, Catalonia, Spain
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Josep Peñuelas, Global Ecology Unit CREAF-CEAB-CSIC, Center for Ecological Research and Forestry Applications, Facultat de Ciències, Universitat Autònoma de Barcelona, 08193 Bellaterra, Catalonia, Spain. E-mail: josep.penuelas@uab.cat

ABSTRACT

Aim  The goals of this study are: (1) to determine whether increasing atmospheric CO2 concentrations and changing climate increased intrinsic water use efficiency (iWUE, as detected by changes in Δ13C) over the last four decades; and if it did increase iWUE, whether it led to increased tree growth (as measured by tree-ring growth); (2) to assess whether CO2 responses are biome dependent due to different environmental conditions, including availability of nutrients and water; and (3) to discuss how the findings of this study can better inform assumptions of CO2 fertilization and climate change effects in biospheric and climate models.

Location  A global range of sites covering all major forest biome types.

Methods  The analysis encompassed 47 study sites including boreal, wet temperate, mediterranean, semi-arid and tropical biomes for which measurements of tree ring Δ13C and growth are available over multiple decades.

Results  The iWUE inferred from the Δ13C analyses of comparable mature trees increased 20.5% over the last 40 years with no significant differences between biomes. This increase in iWUE did not translate into a significant overall increase in tree growth. Half of the sites showed a positive trend in growth while the other half had a negative or no trend. There were no significant trends within biomes or among biomes.

Main conclusions  These results show that despite an increase in atmospheric CO2 concentrations of over 50 p.p.m. and a 20.5% increase in iWUE during the last 40 years, tree growth has not increased as expected, suggesting that other factors have overridden the potential growth benefits of a CO2-rich world in many sites. Such factors could include climate change (particularly drought), nutrient limitation and/or physiological long-term acclimation to elevated CO2. Hence, the rate of biomass carbon sequestration in tropical, arid, mediterranean, wet temperate and boreal ecosystems may not increase with increasing atmospheric CO2 concentrations as is often implied by biospheric models and short-term elevated CO2 experiments.

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