Prebiotic Metabolism: Production by Mineral Photoelectrochemistry of α-Ketocarboxylic Acids in the Reductive Tricarboxylic Acid Cycle

被引:62
作者
Guzman, Marcelo I. [1 ]
Martin, Scot T. [1 ]
机构
[1] Harvard Univ, Dept Earth & Planetary Sci, Sch Engn & Appl Sci, Cambridge, MA 02138 USA
关键词
Origin of life; Prebiotic chemistry; Photoelectrochemistry; Zinc sulfide; Reductive tricarboxylic acid cycle; Pyruvate; Lactate; alpha-Ketoglutarate; Photooxidation; Photoreduction; INTERMEDIARY METABOLISM; ORIGIN; EVOLUTION; LIFE;
D O I
10.1089/ast.2009.0356
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
A reductive tricarboxylic acid (rTCA) cycle could have fixed carbon dioxide as biochemically useful energy-storage molecules on early Earth. Nonenzymatic chemical pathways for some steps of the rTCA cycle, however, such as the production of the alpha-ketocarboxylic acids pyruvate and a-ketoglutarate, remain a challenging problem for the viability of the proposed prebiotic cycle. As a class of compounds, alpha-ketocarboxylic acids have high free energies of formation that disfavor their production. We report herein the production of pyruvate from lactate and of alpha-ketoglutarate from pyruvate in the millimolar concentration range as promoted by ZnS mineral photoelectrochemistry. Pyruvate is produced from the photooxidation of lactate with 70% yield and a quantum efficiency of 0.009 at 15 degrees C across the wavelength range of 200-400 nm. The produced pyruvate undergoes photoreductive back reaction to lactate at a 30% yield and with a quantum efficiency of 0.0024. Pyruvate alternatively continues in photooxidative forward reaction to alpha-ketoglutarate with a 50% yield and a quantum efficiency of 0.0036. The remaining 20% of the carbon follows side reactions that produce isocitrate, glutarate, and succinate. Small amounts of acetate are also produced. The results of this study suggest that alpha-ketocarboxylic acids produced by mineral photoelectrochemistry could have participated in a viable enzyme-free cycle for carbon fixation in an environment where light, sulfide minerals, carbon dioxide, and other organic compounds interacted on prebiotic Earth.
引用
收藏
页码:833 / 842
页数:10
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