Tokyo Tech research: Kinetic analysis questions chemistry proposed for the origin of life


Some will claim this as proof of ‘life’ emerging from primordial slime – or maybe returning to it

Tokyo Institute of Technology research: Kinetic analysis questions chemistry proposed for the origin of life

(Tokyo, 28 July 2016) Kinetic and thermodynamic considerations reported by researchers at the Tokyo Institute of Technology suggest that thioesters at the heart of many theories on the origin of life are unlikely primordial contributors. The research is reported in Scientific Reports, 21 July 2016.

How life emerged from a primordial soup of simple chemicals remains unknown. However, scientists have proposed several possible schemes for the origin of life, many of which rely on chemistry involving thioesters such as thioacetic acid (TAA) and methylathioacetate (MTA). Now results of kinetic and thermodynamic considerations reported by Kuhan Chandru and his colleagues at the Tokyo Institute of Technology (Earth-Life Science Institute: ELSI), question the likelihood of these schemes.

Many of the reactions that form biological matter require enzymes that would not have existed in prebiotic times. However, the high temperatures in hydrothermal vents can overcome reaction barriers without the need for enzymes, making them widely considered likely sites for the origin of life. With this in mind, Chandru along with colleagues led by Jim Cleaves – a researcher affiliated with Tokyo Institute of Technology in Japan and the Institute for Advanced Study in Princeton – studied the reaction kinetics in the conditions found in hydrothermal vents.

The researchers used nuclear magnetic resonance (NMR) to study the reversible hydrolysis of TAA and MTA in a range of possible pH, temperature and concentration conditions common to hydrothermal settings. They conclude that “TAA and MTA differ significantly in terms of their stability and reactivity as a function of pH and temperature, though both are implausible prebiotic reagents for different reasons in different contexts.”

The researchers also add that the results suggest “estimates of the ubiquity of suitable environments for the origin of life in and beyond our solar system may be somewhat overestimated, if these compounds are indeed crucial for jumpstarting early metabolism.”


The role of temperature

Chemical reactions can involve the release (exothermal) or absorption (endothermal) of energy. Many of the reactions that produce organic matter in organisms are highly endothermal. They are achieved in living organisms despite the presence of a large energy barrier to product formation thanks to enzymes, which provide a pathway with a lower energy barrier. In prebiotic Earth such enzymes would not be available so very high temperatures, like those found in hydrothermal vents, may have been needed.

TAA and MTA hydrolyze to form acids and thiols. While this reaction is reversible, the equilibrium concentrations of TAA and MTA in the conditions that exist in hydrothermal vents are extremely low for schemes that base the origin of life on these chemicals.

The role of concentration

The exact conditions during the emergence of life on primordial Earth are unknown. However, what is known of the ancient oceans during the Archaen period (~4-2.5 x 109 years ago, when life is thought to have begun) constrain concentrations of hydrogen ions (that is, pH) as well as iron, carbon and sulphur to levels similar to those found in hydrothermal vents. These concentrations are all problematic for the generation of TAA and MTA.

The origin of reactants

The product of the hydrolysis reactions is acetic acid. Isotopic measurements to date all point to biological origins of the acetic acid that exists in hydrothermal vents, which leaves questions over its existence in the primordial conditions present during the emergence of life.


Kuhan Chandru1, Alexis Gilbert1, Christopher Butch1, Masashi Aono1, H. James Cleaves II1,2,3,4*, The Abiotic Chemistry of Thiolated Acetate Derivatives and the Origin of Life, Scientific Reports 6, on line 21 July 2016

Earth-Life Science Institute, Tokyo Institute of Technology, 2-12-IE-1 Ookayama, Meguro-ku, Tokyo 152-8551, Japan
Institute for Advanced Study, Princeton, NJ 08540
Blue Marble Space Institute of Science, 1515 Gallatin St. NW, Washington, DC 20011
Center for Chemical Evolution, Georgia Institute of Technology, Atlanta, GA 30332

*To whom correspondence should be addressed

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