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大气中的 CO 通过生物源多胺捕获,并可能作为底物转移到 Rubisco 进行羧化反应。

Atmospheric CO captured by biogenic polyamines is transferred as a possible substrate to Rubisco for the carboxylation reaction.

机构信息

Kitasato University School of Marine Biosciences, 1-15-1 Kitasato, Minami, Sagamihara, Kanagawa, 252-0373, Japan.

Biological Laboratory, Center for Natural Sciences, College of Liberal Arts and Sciences, Kitasato University, 1-15-1 Kitasato, Minami, Sagamihara, Kanagawa, 252-0373, Japan.

出版信息

Sci Rep. 2018 Dec 7;8(1):17724. doi: 10.1038/s41598-018-35641-8.

Abstract

Biogenic polyamines are involved in a wide range of plant cellular processes, including cell division, morphogenesis and stress responses. However, the exact roles of biogenic polyamines are not well understood. We recently reported that biogenic polyamines that have multiple amino groups can react with CO and accelerate calcium carbonate formation in seawater. The ability of biogenic polyamines to capture atmospheric CO prompted us to examine their roles in photosynthesis. Here, we demonstrated that atmospheric CO captured by biogenic polyamines is a candidate substrate for the carboxylation reaction of ribulose 1,5-bisphosphate carboxylase/oxygenase (Rubisco), which is an enzyme involved in the first major step of carbon fixation during photosynthesis, and that biogenic polyamines can accelerate the carboxylation reaction of this enzyme because of their specific affinity for CO. Moreover, the results of our nuclear magnetic resonance (NMR) analysis showed that putrescine, which is the most common biogenic polyamine, reacts with atmospheric CO and promotes the formation of carbamate derivatives and bicarbonate in aqueous environments. A sufficient amount of CO is well known to be produced by carbonic anhydrase from bicarbonate in vivo. The present study indicates that CO would be also produced by the equilibrium reaction from carbonate produced by biogenic polyamines and would be used as a substrate of Rubisco, too. Our results may suggest a new photosynthetic research strategy that involves CO-concentrating mechanisms and also possibly constitutes a potential tool for reducing atmospheric CO levels and, consequently, global warming.

摘要

生物源多胺参与广泛的植物细胞过程,包括细胞分裂、形态发生和应激反应。然而,生物源多胺的确切作用尚不清楚。我们最近报道,具有多个氨基的生物源多胺可以与 CO 反应,加速海水中碳酸钙的形成。生物源多胺捕捉大气 CO 的能力促使我们研究它们在光合作用中的作用。在这里,我们证明生物源多胺捕获的大气 CO 是核酮糖 1,5-二磷酸羧化酶/加氧酶(Rubisco)羧化反应的候选底物,Rubisco 是光合作用中固定碳的第一步的主要酶,并且生物源多胺可以通过其对 CO 的特异性亲和力来加速该酶的羧化反应。此外,我们的核磁共振(NMR)分析结果表明,腐胺,是最常见的生物源多胺,与大气 CO 反应,并促进氨基甲酸盐衍生物和碳酸氢盐在水相环境中的形成。在体内,碳酸酐酶可将碳酸氢盐转化为大量 CO。本研究表明,CO 也可以通过生物源多胺产生的碳酸盐的平衡反应产生,并作为 Rubisco 的底物。我们的研究结果可能提示了一种新的光合作用研究策略,涉及 CO 浓缩机制,并且可能构成了降低大气 CO 水平、进而缓解全球变暖的潜在工具。

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