Abstract

Although studies about the origin of life are a frontier in science and a number of effective approaches have been developed, drawbacks still exist. Examples include: (1) simulation of chemical evolution experiments (which were demonstrated for the first time by Stanley Miller); (2) approaches tracing back the most primitive life-like systems (on the basis of investigations of present organisms); and (3) constructive approaches for making life-like systems (on the basis of molecular biology), such as in vitro construction of the RNA world. Naturally, simulation experiments of chemical evolution under plausible ancient Earth environments have been recognized as a potentially fruitful approach. Nevertheless, simulation experiments seem not to be sufficient for identifying the scenario from molecules to life. This is because primitive Earth environments are still not clearly defined and a number of possibilities should be taken into account. In addition, such environments frequently comprise extreme conditions when compared to the environments of present organisms. Therefore, we need to realize the importance of accurate and convenient experimental approaches that use practical research tools, which are resistant to high temperature and pressure, to facilitate chemical evolution studies. This review summarizes improvements made in such experimental approaches over the last two decades, focusing primarily on our hydrothermal microflow reactor technology. Microflow reactor systems are a powerful tool for performing simulation experiments in diverse simulated hydrothermal Earth conditions in order to measure the kinetics of formation and degradation and the interactions of biopolymers.

Highlights

  • A number of investigations regarding the origin of life have been carried out based on experiments that simulate primitive Earth conditions in order to determine the main prebiotic materials and reactions that contributed to the formation of primitive life-like systems

  • The goal of the system is for the residence time and heat-up time to be accurately controlled to a millisecond time scale at very high temperatures, possibly over the critical point of water, rather than running simulations of a realistic hydrothermal vent system, in which the circulation time scale through the vent systems frequently reaches several years

  • The present paper has described briefly the history and background leading up to the development of hydrothermal microflow reactor systems useful for origin-of-life studies

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Summary

Introduction

A number of investigations regarding the origin of life have been carried out based on experiments that simulate primitive Earth conditions in order to determine the main prebiotic materials and reactions that contributed to the formation of primitive life-like systems. Simulation experiments involve attempts to construct life-like systems in laboratories, such as in vitro selection of functional RNA [27,28,29,30,31,32,33,34] and artificial cells [35,36] These simulation experimental data enable a scenario about the origin of life to be drawn up accurately. The traditional experimental approaches of biochemistry and molecular biology are not useful for such simulation experiments with extreme conditions Because of this situation, the development of experimental techniques for chemical evolution is essential for facilitating origin-of-life studies. The first objective of scientists in this field, including our group, is to focus on the development of research tools for chemical evolution

Importance of Hydrothermal Systems in Relation to the RNA World Hypothesis
Hydrothermal Flow System
Details of the Mechanical Characteristics of the Flow System
Kinetic Measurements by the Flow System
In situ Measurement of Absorption Spectra
Mineral-Mediated Hydrothermal System
High-Throughput Modifications
Degradation and Formation of Biomolecules
Interaction of Biomolecules under Hydrothermal Conditions
Chemical Evolution of Biomolecules under Hydrothermal Conditions
Conclusions

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