Thermal limits of leaf metabolism across biomes

Authors

  • Odhran S. O'sullivan,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
    2. Department of Animal and Plant Sciences, University of Sheffield, Sheffield, UK
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  • Mary A. Heskel,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
    2. The Ecosystems Center, Marine Biological Laboratory, Woods Hole, MA, USA
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  • Peter B. Reich,

    1. Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, Australia
    2. Department of Forest Resources, University of Minnesota, St. Paul, MN, USA
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  • Mark G. Tjoelker,

    1. Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, Australia
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  • Lasantha K. Weerasinghe,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
    2. Faculty of Agriculture, University of Peradeniya, Peradeniya, Sri Lanka
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  • Aurore Penillard,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
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  • Lingling Zhu,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
    2. ARC Centre of Excellence in Plant Energy Biology, Research School of Biology, The Australian National University, Canberra, ACT, Australia
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  • John J. G. Egerton,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
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  • Keith J. Bloomfield,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
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  • Danielle Creek,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
    2. Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, Australia
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  • Nur H. A. Bahar,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
    2. ARC Centre of Excellence in Plant Energy Biology, Research School of Biology, The Australian National University, Canberra, ACT, Australia
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  • Kevin L. Griffin,

    1. Department of Earth and Environment Sciences, Columbia University, Palisades, NY, USA
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  • Vaughan Hurry,

    1. Umeå Plant Science Centre, Department of Forest Genetics and Plant Physiology, Swedish University of Agricultural Sciences, Umeå, Sweden
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  • Patrick Meir,

    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
    2. School of Geosciences, University of Edinburgh, Edinburgh, UK
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  • Matthew H. Turnbull,

    1. Centre for Integrative Ecology, School of Biological Sciences, University of Canterbury, Christchurch, New Zealand
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  • Owen K. Atkin

    Corresponding author
    1. Division of Plant Sciences, Research School of Biology, The Australian National University, Canberra, ACT, Australia
    2. ARC Centre of Excellence in Plant Energy Biology, Research School of Biology, The Australian National University, Canberra, ACT, Australia
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Abstract

High-temperature tolerance in plants is important in a warming world, with extreme heat waves predicted to increase in frequency and duration, potentially leading to lethal heating of leaves. Global patterns of high-temperature tolerance are documented in animals, but generally not in plants, limiting our ability to assess risks associated with climate warming. To assess whether there are global patterns in high-temperature tolerance of leaf metabolism, we quantified Tcrit (high temperature where minimal chlorophyll a fluorescence rises rapidly and thus photosystem II is disrupted) and Tmax (temperature where leaf respiration in darkness is maximal, beyond which respiratory function rapidly declines) in upper canopy leaves of 218 plant species spanning seven biomes. Mean site-based Tcrit values ranged from 41.5 °C in the Alaskan arctic to 50.8 °C in lowland tropical rainforests of Peruvian Amazon. For Tmax, the equivalent values were 51.0 and 60.6 °C in the Arctic and Amazon, respectively. Tcrit and Tmax followed similar biogeographic patterns, increasing linearly (˜8 °C) from polar to equatorial regions. Such increases in high-temperature tolerance are much less than expected based on the 20 °C span in high-temperature extremes across the globe. Moreover, with only modest high-temperature tolerance despite high summer temperature extremes, species in mid-latitude (~20–50°) regions have the narrowest thermal safety margins in upper canopy leaves; these regions are at the greatest risk of damage due to extreme heat-wave events, especially under conditions when leaf temperatures are further elevated by a lack of transpirational cooling. Using predicted heat-wave events for 2050 and accounting for possible thermal acclimation of Tcrit and Tmax, we also found that these safety margins could shrink in a warmer world, as rising temperatures are likely to exceed thermal tolerance limits. Thus, increasing numbers of species in many biomes may be at risk as heat-wave events become more severe with climate change.

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