The photosynthetic oxygen evolution does not exclude the important role and contribution of bicarbonate photolysis

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Acta Geochimica Pub Date : 2023-10-31 DOI:10.1007/s11631-023-00649-z
Yanyou Wu, Shaogang Guo
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Abstract

Photosynthesis is the most important biochemical reaction on Earth. It has co-evolved and developed with the Earth, driving the biogeochemical cycle of all elements on the planet and serving as the only chemical process in nature that can convert light energy into chemical energy. Some heavy oxygen isotopic (18O) labeling experiments have “conclusively” demonstrated that the oxygen released by photosynthesis comes only from water and are written into textbooks. However, it is not difficult to find that bicarbonate has never been excluded from the direct substrate of photosynthesis from beginning to end during the history of photosynthesis research. No convincing mechanism can be used to explain photosynthetic oxygen evolution solely from water photolysis. The bicarbonate effect, the Dole effect, the thermodynamic convenience of bicarbonate photolysis, the crystal structure characteristics of photosystem II, and the reinterpretation of heavy oxygen isotopic labeling (18O) experiments all indicate that the photosynthetic oxygen evolution does not exclude the important role and contribution of bicarbonate photolysis. The recently proposed view that bicarbonate photolysis is the premise of water photolysis, bicarbonate photolysis and water photolysis work together with a 1:1 (mol/mol) stoichiometric relationship, and the stoichiometric relationship between oxygen and carbon dioxide released during photosynthetic oxygen evolution is also 1:1, has excellent applicability and objectivity, which can logically and reasonably explain the precise coordination between light and dark reactions during photosynthesis, the bicarbonate effect, the Dole effect, the Kok cycle and the neutrality of water and carbon in nature. This is of great significance for constructing the bionic artificial photosynthetic reactors and scientifically answering the question of the source of elemental stoichiometric relationships in nature.

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光合作用的氧气进化并不排除碳酸氢盐光解的重要作用和贡献
光合作用是地球上最重要的生化反应。它与地球共同进化和发展,推动着地球上所有元素的生物地球化学循环,是自然界中唯一能将光能转化为化学能的化学过程。一些重氧同位素(18O)标记实验 "确凿 "地证明光合作用释放的氧气只来自于水,并被写进了教科书。然而,我们不难发现,在光合作用的研究史上,碳酸氢盐自始至终从未被排除在光合作用的直接底物之外。没有一种令人信服的机制可以用来解释光合作用中氧气的进化完全来自于水的光解。碳酸氢盐效应、多尔效应、碳酸氢盐光解的热力学便利性、光合系统 II 的晶体结构特征以及重氧同位素标记(18O)实验的重新解释都表明,光合作用氧进化并不排除碳酸氢盐光解的重要作用和贡献。最近提出的碳酸氢盐光解是水光解的前提,碳酸氢盐光解和水光解以 1:1(摩尔/摩尔)的化学计量关系共同作用,光合作用氧进化过程中释放的氧气和二氧化碳的化学计量关系也是 1:1,具有很好的适用性和客观性,可以从逻辑上合理解释光合作用过程中光反应和暗反应的精确配合、碳酸氢盐效应、多尔效应、科克循环以及自然界中水和碳的中性。这对于建造仿生人工光合反应器和科学回答自然界元素化学计量关系的来源问题具有重要意义。
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来源期刊
Acta Geochimica
Acta Geochimica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
2.80
自引率
6.20%
发文量
1134
期刊介绍: Acta Geochimica serves as the international forum for essential research on geochemistry, the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth‘s crust, its oceans and the entire Solar System, as well as a number of processes including mantle convection, the formation of planets and the origins of granite and basalt. The journal focuses on, but is not limited to the following aspects: • Cosmochemistry • Mantle Geochemistry • Ore-deposit Geochemistry • Organic Geochemistry • Environmental Geochemistry • Computational Geochemistry • Isotope Geochemistry • NanoGeochemistry All research articles published in this journal have undergone rigorous peer review. In addition to original research articles, Acta Geochimica publishes reviews and short communications, aiming to rapidly disseminate the research results of timely interest, and comprehensive reviews of emerging topics in all the areas of geochemistry.
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