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Bicarbonate is a key regulator but not a substrate for O2 evolution in Photosystem II
David J Vinyard1, Govindjee Govindjee2
1Department of Biological Sciences, Louisiana State University, Baton Rouge, LA, 70803, USA. dvinyard@lsu.edu.
Photosynthesis Research
|July 22, 2024
Summary
Photosystem II (PSII) uses light energy to split water and produce oxygen. Despite evidence, some theories propose bicarbonate as a source of oxygen, but experiments show no bicarbonate near the active site.
Area of Science:
- Biochemistry
- Photosynthesis
- Structural Biology
Background:
- Photosystem II (PSII) is crucial for photosynthesis, splitting water to produce oxygen (O2) and reducing plastoquinone.
- While water is the accepted source of O2, alternative hypotheses involving bicarbonate persist.
- Understanding the O2 evolution mechanism is vital for comprehending photosynthesis.
Purpose of the Study:
- To review the regulatory roles of bicarbonate in PSII activity and assembly.
- To critically evaluate the hypothesis that bicarbonate is a substrate for O2 evolution.
- To present evidence challenging the bicarbonate-based O2 evolution theory.
Main Methods:
- Review of existing literature on Photosystem II and bicarbonate.
- Analysis of biochemical, spectroscopic, and structural biology data.
- Thermodynamic evaluation of oxygen-centered bicarbonate oxidation.
Main Results:
- Bicarbonate plays regulatory roles in PSII activity and assembly.
- Biochemistry, spectroscopy, and structural biology experiments have not detected bicarbonate at the O2 evolution active site.
- Thermodynamic arguments for bicarbonate oxidation exist but do not confirm it as a substrate.
Conclusions:
- The prevailing evidence supports water as the sole source of O2 in photosynthesis.
- The hypothesis of bicarbonate as a substrate for O2 evolution is not supported by experimental data.
- Further research should focus on the established water-splitting mechanism in Photosystem II.
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