Photosynthetic optimum temperature plays a minor role in the increase of terrestrial carbon uptake from 2000 to 2019

Research output: Contribution to journalResearch articleContributedpeer-review

Contributors

  • Chongyang Xu - , Hebrew University of Jerusalem (Author)
  • Hongyan Liu - , Peking University (Author)
  • Dan Yakir - , Weizmann Institute of Science (Author)
  • Boyi Liang - , Beijing Forestry University (Author)
  • Xinrong Zhu - , Peking University (Author)
  • Yu Zhou - , ETH Zurich (Author)
  • Luca Belelli Marchesini - , Istituto Agrario San Michele all'Adige (Edmund Mach Foundation) (Author)
  • Damien Bonal - , Université de Lorraine (Author)
  • Nina Buchmann - , ETH Zurich (Author)
  • Christian Brümmer - , Johann Heinrich von Thunen Institute (Author)
  • Jamie Cleverly - , James Cook University Queensland (Author)
  • Siwen Feng - , Huafeng Meteorological Media Group (Author)
  • Mika Korkiakoski - , Finnish Meteorological Institute (Author)
  • Michael J. Liddell - , James Cook University Queensland (Author)
  • Matthias Mauder - , Chair of Meteorology (Author)
  • Leonardo Montagnani - , Free University of Bozen-Bolzano (Author)
  • Andrej Varlagin - , Russian Academy of Sciences (Author)
  • Luca Vitale - , National Research Council of Italy (CNR) (Author)
  • Songhan Wang - , Nanjing Agricultural University (Author)
  • William Woodgate - , University of Queensland, Commonwealth Scientific & Industrial Research Organisation (CSIRO) (Author)
  • José M. Grünzweig - , Hebrew University of Jerusalem (Author)

Abstract

Gross primary productivity (GPP; ecosystem-level photosynthesis) represents the largest terrestrial carbon flux and is highly sensitive to temperature. Despite global warming, the trends and controlling factors of optimum temperature ((Formula presented) ) and maximum rates of GPP ((Formula presented) ) remain uncertain. We investigated the drivers of (Formula presented) and (Formula presented) trends during 2000–2019 using global observations of ground-based eddy covariance and satellite-based sun-induced chlorophyll fluorescence. Although (Formula presented) increased worldwide, (Formula presented) increased only in tropical and temperate regions but remained unchanged globally and in arid and cold regions. Thermal acclimation via shifting (Formula presented) was constrained by atmospheric and soil dryness, explaining less than 20% of the global (Formula presented) rise. In contrast, (Formula presented) trends were more strongly driven by stomatal regulation improving water-use efficiency and by enhanced canopy development under dryness constraints. These findings challenge the expectation that thermal acclimation is central to projecting GPP under warming and highlight dynamic physiological-structural shifts that sustain terrestrial carbon uptake.

Details

Original languageEnglish
Article number101703
JournalOne Earth
Volume9
Issue number5
Publication statusPublished - 15 May 2026
Peer-reviewedYes

Keywords

Keywords

  • canopy development, carbon uptake, eddy-covariance measurements, global warming, intrinsic water-use efficiency, optimum temperature for gross primary productivity, SIF, solar-induced chlorophyll fluorescence, thermal acclimation