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Global warming and droughts push forests closer to their thermal limits, altering tree carbon uptake and growth. To prevent critical overheating, trees can adjust their thermotolerance (T ), temperature and photosynthetic optima (T and A ), and canopy temperature (T ) to stay below damaging thresholds. However, we lack an understanding of how soil droughts affect photosynthetic thermal plasticity and T regulation. In this study, we measured the effect of soil moisture on the seasonal and diurnal dynamics of net photosynthesis (A), stomatal conductance (g ), and T , as well as the thermal plasticity of photosynthesis (T , T , and A ), over the course of 1 yr using a long-term irrigation experiment in a drought-prone Pinus sylvestris forest in Switzerland. Irrigation resulted in higher needle-level A, g , T , and A compared with naturally drought-exposed trees. No daily or seasonal differences in T were observed between treatments. Trees operated below their thermal thresholds (T ), independently of soil moisture content. Despite strong T and T coupling, we provide evidence that drought reduces trees' temperature optimum due to a substantial reduction of g during warm and dry periods of the year. These findings provide important insights regarding the effects of soil drought on the thermal tolerance of P. sylvestris.
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http://dx.doi.org/10.1111/nph.19136 | DOI Listing |
Background And Aims: Trait-based approaches have advanced our understanding of plant strategies, yet they often focus on leaf-level traits, overlooking the functional roles of stem anatomy and twig characteristics. We investigated intraspecific trait variation in Salix flabellaris, an alpine dwarf shrub, along climatic gradients in the Himalayas. Our goal was to identify distinct axes of trait variation related to stem, twig, and leaf traits, assess their environmental drivers, and evaluate population-specific growth responses to recent climate change.
View Article and Find Full Text PDFEnviron Monit Assess
September 2025
Institute of Environmental Studies, Kurukshetra University, Kurukshetra, Haryana, 136119, India.
India produces an estimated 6.38 million tons of surplus sugarcane trash annually. When burned in fields, this trash emits approximately 12,948 kg CO equivalent greenhouse gases per hectare and causes nutrient losses (41 kg ha nitrogen, 5.
View Article and Find Full Text PDFFront Plant Sci
August 2025
Institute of Crop Sciences, Chinese Academy of Agricultural Sciences, Key Laboratory of Crop Physiology and Ecology, Ministry of Agriculture and Rural Affairs of China, Beijing, China.
Simultaneously enhancing the crop yield and reducing nitrous oxide (NO) emissions presents a critical challenge in sustainable agriculture. The application of nitrogen (N) fertilizer is a key strategy to enhance crop yield. However, conventional N application practices often lead to excessive soil N accumulation, insufficient crop N uptake and elevated greenhouse gas (GHG) emissions.
View Article and Find Full Text PDFNew Phytol
September 2025
Environment and Natural Resources Institute, University of Alaska Anchorage, Anchorage, AK, 99508, USA.
Snow is an important insulator of Arctic soils during winter and may be a source of soil moisture in summer. Changes in snow depth are likely to affect fine root growth and mortality via changes in soil temperature, moisture, and/or nutrient availability, which could alter aboveground growth and reproduction of Arctic vegetation. We explored fine root dynamics at three contrasting treelines in northwest Alaska.
View Article and Find Full Text PDFJ Environ Manage
September 2025
College of Water Resources and Architectural Engineering at Northwest Agriculture and Forestry University/Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas at Ministry of Education, Yangling, Shaanxi, 712100, PR China; Academy of Plateau Science and Sustainability,
Alpine ecosystems are critical for water regulation but highly sensitive to climate change. In the Three-River Source Region (TRSR) of the Qinghai-Tibet Plateau, changes in temperature, precipitation, and large-scale ecological restoration have significantly altered vegetation phenology-including the start (SOS), end (EOS), and length (LOS) of the growing season, as well as vegetation growth status (GS). These shifts affect hydrological processes such as evapotranspiration, soil moisture, snowmelt, and runoff.
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