Photosynthetic Performance of Tidally Flooded Spartina Alterniflora Salt Marshes

Lishen Mao, Deepak R. Mishra, Peter A. Hawman, Caroline R. Narron, Jessica L. O’Connell, David L. Cotten

Research output: Contribution to journalArticlepeer-review

5 Scopus citations

Abstract

Spartina alterniflora has a distinct flood-adapted morphology, and its physiological responses are likely to vary with differences in tidal submergence. To understand these responses, we examined the impacts of tidal inundation on the efficiency of Photosystem II (φPSII) photochemistry and leaf-level photosynthesis at different canopy heights through a combination of in situ chlorophyll fluorescence (ChlF), incident photosynthetically active radiation, and tide levels. Our result showed small declines (7%–8.3%) in φPSII for air-exposed leaves when the bottom canopies were tidally submerged. Submerged leaves produced large reductions (30.3%–41%) in φPSII. Our results suggest that when submerged, PSII reaction centers in S. alterniflora leaves are still active and able to transfer electrons, but only at ∼20% of the typical daily rate. We attribute this reduction in φPSII to the decrease in the fraction of “open” PSII reaction centers (10% of the total) and the stomatal conductance rate caused by the tidal submergence. To our knowledge, this flooding induced leaf-level reduction of φPSII for S. alterniflora in field settings has not been reported before. Our findings suggest that canopy-level φPSII is dependent on the proportion of submerged versus emerged leaves and highlight the complexities involved in estimating the photosynthetic efficiency of tidal marshes.

Original languageEnglish
Article numbere2022JG007161
JournalJournal of Geophysical Research: Biogeosciences
Volume128
Issue number3
DOIs
StatePublished - Mar 2023

Funding

This project was supported by NASA Carbon Cycle Science Grant (#NNX17AI76G) and the Georgia Coastal Ecosystems LTER's National Science Foundation funding (OCE-1237140 and OCE-1832178). This is contribution 1111 of the University of Georgia Marine Institute. The authors would like to thank Dontrece Smith, Jacob Shalack, Alyssa Peterson, John Williams, and Elise Diehl for their assistance in field transportation, field data collection, and sensor maintenance at the GCE-LTER site. The authors would like to thank Wade Sheldon, and Adam Sapp for data management at the GCE-LTER site. The authors also thank Dr. Hailong Huang for his help in the first deployment and testing of the PAM fluorometry. This project was supported by NASA Carbon Cycle Science Grant (#NNX17AI76G) and the Georgia Coastal Ecosystems LTER's National Science Foundation funding (OCE‐1237140 and OCE‐1832178). This is contribution 1111 of the University of Georgia Marine Institute. The authors would like to thank Dontrece Smith, Jacob Shalack, Alyssa Peterson, John Williams, and Elise Diehl for their assistance in field transportation, field data collection, and sensor maintenance at the GCE‐LTER site. The authors would like to thank Wade Sheldon, and Adam Sapp for data management at the GCE‐LTER site. The authors also thank Dr. Hailong Huang for his help in the first deployment and testing of the PAM fluorometry.

FundersFunder number
NASA Carbon Cycle Science17AI76G
University of Georgia Marine Institute
Wade Sheldon
National Science FoundationOCE‐1237140, OCE‐1832178

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