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Atmospheric UV synthesis of aldehydes and oxidant from CO2, CO and H2O initiating the first ancestral metabolism

This study demonstrates that atmospheric UV irradiation of CO₂, CO, and H₂O on the early Earth or Mars can spontaneously generate a self-sustaining "Primitive Respiration Cycle" of aldehydes, organic acids, and amino acids, offering a plausible non-enzymatic pathway bridging geochemistry and the emergence of ancestral metabolism.

Original authors: Yuichiro Ueno, Xiaofeng Zang, Yuta Asakura, Andy Fong, Waka Kawade, Kenta Isoda, Tetsuya Yokoyama, Norio Kitadai

Published 2026-08-27
📖 5 min read🧠 Deep dive

Original authors: Yuichiro Ueno, Xiaofeng Zang, Yuta Asakura, Andy Fong, Waka Kawade, Kenta Isoda, Tetsuya Yokoyama, Norio Kitadai

Original paper licensed under CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/). This is an AI-generated explanation of the paper below. It is not written or endorsed by the authors. For technical accuracy, refer to the original paper. Read full disclaimer

Before life could begin, the Earth needed a way to turn simple, lifeless gases into the complex building blocks of biology. Scientists have long debated how this transition happened, focusing on two main possibilities: either genetic molecules like RNA appeared first, or a network of chemical reactions that we now call metabolism came first. In both scenarios, the starting point is the same: the early atmosphere was filled with carbon dioxide, carbon monoxide, and water vapor. The question is how sunlight could have acted on these ingredients to create the sugars, acids, and proteins necessary for life. For decades, researchers knew that sunlight could turn carbon monoxide and water into formaldehyde, a simple sugar-like molecule. However, it was unclear if this process could generate the rich variety of chemicals needed to kickstart a living system, or if the harsh, oxidizing environment of the early Earth would simply destroy these fragile molecules before they could do anything useful.

A team of researchers led by Yuichiro Ueno at the Institute of Science Tokyo has now demonstrated that this atmospheric chemistry is far more productive and complex than previously thought. By simulating the conditions of the early Earth's atmosphere in a glass flask, they showed that sunlight does not just make formaldehyde; it creates a whole family of small aldehydes, including acetaldehyde and glyoxal. When these gases dissolve into water, they do not simply sit there or break down. Instead, they begin to react with one another in a self-sustaining cycle that mimics the core processes of modern biological respiration. The study, published in a revised version for the journal PEPS, suggests that a primitive form of metabolism could have emerged spontaneously from the interaction of sunlight, water, and carbon gases, providing a stable chemical foundation for life to eventually take hold.

The experiment began by filling a glass vessel with carbon monoxide, carbon dioxide, and water vapor, then exposing the mixture to ultraviolet light that mimicked the intense sunlight of the early Earth. The researchers watched what happened as the light broke apart water molecules, creating highly reactive fragments that attacked the carbon gases. They found that the process produced not only the expected formaldehyde but also significant amounts of acetaldehyde and glyoxal. These molecules are crucial because they serve as the starting points for building larger, more complex structures. The team then tracked how these gases behaved once they dissolved into the liquid water at the bottom of the flask. In the water, the chemistry became even more dynamic. The dissolved aldehydes reacted to form hydroxy aldehydes, which are the precursors to sugars, as well as various acids like glycolic acid and lactic acid.

What makes this discovery particularly striking is the behavior of the system over time. The researchers observed that while the sunlight produced powerful oxidants that could destroy organic molecules, a specific set of chemicals managed to survive and even regenerate themselves. The system operated through a cycle of condensation, where small molecules joined together to form larger ones; oxidation, where they gained oxygen to become acids; and decarboxylation, where they lost a carbon atom to return to a smaller form. This cycle allowed specific molecules, such as glycolaldehyde and acetaldehyde, to be recycled continuously. The authors call this the Primitive Respiration Cycle. It functions like a chemical engine that keeps a specific set of molecules in circulation, protecting them from being completely broken down into carbon dioxide, as long as the atmosphere continues to supply fresh aldehydes.

The study also explored what happened when ammonia was introduced into this mixture, simulating the presence of nitrogen in the early environment. The results were equally compelling. The existing network of carbon-based molecules reacted with the ammonia to produce amino acids, the building blocks of proteins, as well as heterocyclic nitrogen compounds. These nitrogen rings are structurally similar to coenzymes, which are essential helpers in modern biological metabolism. The researchers found that the system naturally selected for specific types of amino acids, particularly those that are used by life today, while producing fewer of the alternative forms. This suggests that the chemical environment itself could have acted as a filter, favoring the molecules that would eventually become part of living cells.

The researchers are careful to note that this does not prove that life started exactly this way, but it provides a plausible and robust mechanism for how the first metabolic networks could have formed. The system they observed is self-organizing, meaning it creates its own order without the need for enzymes or genetic instructions. It relies entirely on the physical laws of chemistry and the energy provided by the sun. The study rules out the idea that formaldehyde was the only significant product of atmospheric photochemistry, showing instead that a diverse soup of reactive molecules was inevitable. It also challenges the notion that the oxidizing nature of the early atmosphere would have prevented the accumulation of organic matter; instead, the study shows that the same oxidants that threaten to destroy these molecules are also the very drivers that keep the cycle turning.

In the end, the work paints a picture of a prebiotic Earth where the atmosphere and the oceans were engaged in a continuous chemical conversation. Sunlight drove the conversion of simple gases into a complex mixture of organics, which then settled into the water to form a stable, recycling network. This network could have persisted for long periods, accumulating the necessary ingredients for life. When the right conditions arose, such as the availability of phosphates or the formation of compartments, this chemical system could have transitioned into the enzymatic and genetic systems we recognize as life. The findings suggest that the blueprint for metabolism was not a rare accident but a natural consequence of the chemistry of a planet bathed in sunlight, waiting for the next step in evolution to begin.

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