Photosynthetic capacity in middle-aged larch and spruce acclimates independently to experimental warming and elevated CO2

Mirindi Eric Dusenge, Jeffrey M. Warren, Peter B. Reich, Eric J. Ward, Bridget K. Murphy, Artur Stefanski, Raimundo Bermudez, Marisol Cruz, David A. McLennan, Anthony W. King, Rebecca A. Montgomery, Paul J. Hanson, Danielle A. Way

Research output: Contribution to journalArticlepeer-review

6 Scopus citations

Abstract

Photosynthetic acclimation to both warming and elevated CO2 of boreal trees remains a key uncertainty in modelling the response of photosynthesis to future climates. We investigated the impact of increased growth temperature and elevated CO2 on photosynthetic capacity (Vcmax and Jmax) in mature trees of two North American boreal conifers, tamarack and black spruce. We show that Vcmax and Jmax at a standard temperature of 25°C did not change with warming, while Vcmax and Jmax at their thermal optima (Topt) and growth temperature (Tg) increased. Moreover, Vcmax and Jmax at either 25°C, Topt or Tg decreased with elevated CO2. The Jmax/Vcmax ratio decreased with warming when assessed at both Topt and Tg but did not significantly vary at 25°C. The Jmax/Vcmax increased with elevated CO2 at either reference temperature. We found no significant interaction between warming and elevated CO2 on all traits. If this lack of interaction between warming and elevated CO2 on the Vcmax, Jmax and Jmax/Vcmax ratio is a general trend, it would have significant implications for improving photosynthesis representation in vegetation models. However, future research is required to investigate the widespread nature of this response in a larger number of species and biomes.

Original languageEnglish
Pages (from-to)4886-4902
Number of pages17
JournalPlant Cell and Environment
Volume47
Issue number12
DOIs
StatePublished - Dec 2024

Funding

Research was sponsored by the Biological and Environmental Research Program in the Office of Science, U.S. Department of Energy managed by UT- Battelle, LLC, for the U.S. Department of Energy under contract DEAC05-00OR22725. M.E.D., J.M.W., E.J.W., D.A.M., A.W.K. and P.J.H. were supported under this contract. E.J.W. also acknowledges support from USGS Climate Research and Development Program. P.B.R., A.S., R.B., and R.A.M acknowledge funding support by the U.S. NSF Biological Integration Institutes grant DBI-2021898. D.A.W. acknowledges funding from the NSERC Discovery and Strategic programs (RGPIN/04677-2019 and STPGP/521445-2018), the Research School of Biology at the Australian National University, and the U.S. Department of Energy contract No. DE-SC0012704 to Brookhaven National Laboratory. Notice: This manuscript has been authored by UT-Battelle, LLC, under contract DE-AC05-00OR22725 with the US Department of Energy (DOE). The US government retains and the publisher, by accepting the article for publication, acknowledges that the US government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for US government purposes. DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan (http://energy.gov/downloads/doe-public-access-plan). The DOI link for the data set used in this paper can be accessed at https://doi.org/10.25581/spruce.056/1455138 (Dusenge, Ward, et al., 2020) and https://doi.org/10.6084/m9.figshare.23685984.v2. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Research was sponsored by the Biological and Environmental Research Program in the Office of Science, U.S. Department of Energy managed by UT‐ Battelle, LLC, for the U.S. Department of Energy under contract DEAC05‐00OR22725. M.E.D., J.M.W., E.J.W., D.A.M., A.W.K. and P.J.H. were supported under this contract. E.J.W. also acknowledges support from USGS Climate Research and Development Program. P.B.R., A.S., R.B., and R.A.M acknowledge funding support by the U.S. NSF Biological Integration Institutes grant DBI‐2021898. D.A.W. acknowledges funding from the NSERC Discovery and Strategic programs (RGPIN/04677‐2019 and STPGP/521445‐2018), the Research School of Biology at the Australian National University, and the U.S. Department of Energy contract No. DE‐SC0012704 to Brookhaven National Laboratory. Notice: This manuscript has been authored by UT‐Battelle, LLC, under contract DE‐AC05‐00OR22725 with the US Department of Energy (DOE). The US government retains and the publisher, by accepting the article for publication, acknowledges that the US government retains a nonexclusive, paid‐up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript, or allow others to do so, for US government purposes. DOE will provide public access to these results of federally sponsored research in accordance with the DOE Public Access Plan ( http://energy.gov/downloads/doe-public-access-plan ). The DOI link for the data set used in this paper can be accessed at https://doi.org/10.25581/spruce.056/1455138 (Dusenge, Ward, et al., 2020) and https://doi.org/10.6084/m9.figshare.23685984.v2 . Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.

Keywords

  • SPRUCE project
  • acclimation
  • black spruce
  • boreal conifers
  • tamarack
  • temperature

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