Photosynthetic and Respiratory Acclimation of Understory Shrubs in Response to in situ Experimental Warming of a Wet Tropical Forest

Kelsey R. Carter, Tana E. Wood, Sasha C. Reed, Elsa C. Schwartz, Madeline B. Reinsel, Xi Yang, Molly A. Cavaleri

Research output: Contribution to journalArticlepeer-review

23 Scopus citations

Abstract

Despite the importance of tropical forests to global carbon balance, our understanding of how tropical plant physiology will respond to climate warming is limited. In addition, the contribution of tropical forest understories to global carbon cycling is predicted to increase with rising temperatures, however, in situ warming studies of tropical forest plants to date focus only on upper canopies. We present results of an in situ field-scale +4°C understory infrared warming experiment in Puerto Rico (Tropical Responses to Altered Climate Experiment; TRACE). We investigated gas exchange responses of two common understory shrubs, Psychotria brachiata and Piper glabrescens, after exposure to 4 and 8 months warming. We assessed physiological acclimation in two ways: (1) by comparing plot-level physiological responses in heated versus control treatments before and after warming, and (2) by examining physiological responses of individual plants to variation in environmental drivers across all plots, seasons, and treatments. P. brachiata has the capacity to up-regulate (i.e., acclimate) photosynthesis through broadened thermal niche and up-regulation of photosynthetic temperature optimum (Topt) with warmer temperatures. P. glabrescens, however, did not upregulate any photosynthetic parameter, but rather experienced declines in the rate of photosynthesis at the optimum temperature (Aopt), corresponding with lower stomatal conductance under warmer daily temperatures. Contrary to expectation, neither species showed strong evidence for respiratory acclimation. P. brachiata down-regulated basal respiration with warmer daily temperatures during the drier winter months only. P. glabrescens showed no evidence of respiratory acclimation. Unexpectedly, soil moisture, was the strongest environmental driver of daily physiological temperature responses, not vegetation temperature. Topt increased, while photosynthesis and basal respiration declined as soils dried, suggesting that drier conditions negatively affected carbon uptake for both species. Overall, P. brachiata, an early successional shrub, showed higher acclimation potential to daily temperature variations, potentially mitigating negative effects of chronic warming. The negative photosynthetic response to warming experienced by P. glabrescens, a mid-successional shrub, suggests that this species may not be able to as successfully tolerate future, warmer temperatures. These results highlight the importance of considering species when assessing climate change and relay the importance of soil moisture on plant function in large-scale warming experiments.

Original languageEnglish
Article number576320
JournalFrontiers in Forests and Global Change
Volume3
DOIs
StatePublished - Sep 30 2020
Externally publishedYes

Funding

We are very grateful to TRACE project managers Aura M. Alonso-Rodríguez and Megan Berberich for their logistical support. We are also grateful to Kaylie Butts, Benjamin Miller, Talia Anderson, Jamarys Torres, GraceAnna Schilz, Jack Zwart, and Brian Peacock for their excellent field and lab assistance. Reviewers gave critical feedback on an earlier manuscript version that we believe greatly enhanced the quality. We also thank Robert Froese, Andrew Burton, and Sarah Green for thoughtful discussions. A previous version of this manuscript was included in a Ph.D. dissertation (Carter, 2019). Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the United States Government. Funding. This research was funded by U.S. Department of Energy award numbers DE-SC-0012000, DE-SC-0011806, 89243018S-SC-000014, and DE-SC-0018942 awarded to MC, TW, and SR. This research was also funded by the National Science Foundation award DEB-1754713. SR was also supported by the U.S. Geological Survey Ecosystem Mission Area. The USDA Forest Service’s International Institute of Tropical Forestry (IITF) and University of Puerto Rico-Río Piedras provided additional support. All research at IITF is done in collaboration with the University of Puerto Rico. ES was also funded by Michigan Technological University Ecosystem Science Center and a Summer Undergraduate Research Fellowship. KC was also funded by Michigan Technological Finishing Fellowship and Michigan Tech Ecosystem Science Center. This research was funded by U.S. Department of Energy award numbers DE-SC-0012000, DE-SC-0011806, 89243018S-SC-000014, and DE-SC-0018942 awarded to MC, TW, and SR. This research was also funded by the National Science Foundation award DEB-1754713. SR was also supported by the U.S. Geological Survey Ecosystem Mission Area. The USDA Forest Service’s International Institute of Tropical Forestry (IITF) and University of Puerto Rico-Río Piedras provided additional support. All research at IITF is done in collaboration with the University of Puerto Rico. ES was also funded by Michigan Technological University Ecosystem Science Center and a Summer Undergraduate Research Fellowship. KC was also funded by Michigan Technological Finishing Fellowship and Michigan Tech Ecosystem Science Center.

Keywords

  • TRACE
  • experimental warming
  • photosynthesis
  • respiration
  • stomatal traits
  • thermal acclimation
  • tropical forests

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