Primordial Photoredox Catalyst
Nitrogen-Doped Graphite Catalyzes Reactions to Give Early Biomolecules
(c) Wiley-VCH
Between three and four billion years ago, on primordial Earth, the first biomolecules were being formed prior to an explosion of life. These early chemical reactions, however, required catalysts. Xinchen Wang and a team of researchers from Fuzhou University in China have discovered that the primordial atmosphere itself could have served as a source for these catalysts.
Using methane and ammonia gases, which were most likely present in the hot gas mixture shrouding the world in the Archean age, the team used chemical vapor deposition to produce nitrogenous carbon compounds as possible catalysts. They found that, in a reaction chamber, molecules condensed out of an ammonia and methane plasma onto a surface, quickly growing to form a solid nitrogenous carbon polymer similar to nitrogen-doped graphite.
As the team observed, the irregularly incorporated nitrogen atoms gave this polymer catalytically active sites and an electron structure that enabled it to be excited by light. The researchers then turned to proving the extent to which the substance could reduce or oxidize other substances under the effect of light.
One of the most significant reactions on early Earth may have been imine formation. Imines, also referred to as Schiff bases, are a dehydrogenated form of amines, compounds composed of carbon, nitrogen, and hydrogen. Many chemists assume that, on primordial Earth, imines may have served in the formation of the first hereditary molecules of ribonucleic acid (RNA). Wang and his team could show that their plasma-generated catalyst can convert amines to imines using nothing other than sunlight.
The team says that carbon nitride-based photocatalysts, such as the plasma-generated substance, could have lasted for millions of years and produced important chemical intermediates. In addition, they could also have served as a source of carbon- and nitrogen-containing compounds. By demonstrating that it is possible to produce such a catalyst using only the gases and conditions present in the atmosphere of early Earth, the study sheds new light on the possible evolutionary path taken by biomolecules.
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