Aby wyświetlić tę treść, wymagana jest subskrypcja JoVE. Zaloguj się lub rozpocznij bezpłatny okres próbny.
Method Article
The Miller-Urey experiment was a pioneering study regarding the abiotic synthesis of organic compounds with possible relevance to the origins of life. Simple gases were introduced into a glass apparatus and subjected to an electric discharge, simulating the effects of lightning in the primordial Earth’s atmosphere-ocean system. The experiment was conducted for one week, after which, the samples collected from it were analyzed for the chemical building blocks of life.
In 1953, Stanley Miller reported the production of biomolecules from simple gaseous starting materials, using an apparatus constructed to simulate the primordial Earth's atmosphere-ocean system. Miller introduced 200 ml of water, 100 mmHg of H2, 200 mmHg of CH4, and 200 mmHg of NH3 into the apparatus, then subjected this mixture, under reflux, to an electric discharge for a week, while the water was simultaneously heated. The purpose of this manuscript is to provide the reader with a general experimental protocol that can be used to conduct a Miller-Urey type spark discharge experiment, using a simplified 3 L reaction flask. Since the experiment involves exposing inflammable gases to a high voltage electric discharge, it is worth highlighting important steps that reduce the risk of explosion. The general procedures described in this work can be extrapolated to design and conduct a wide variety of electric discharge experiments simulating primitive planetary environments.
The nature of the origins of life on Earth remains one of the most inscrutable scientific questions. In the 1920s Russian biologist Alexander Oparin and British evolutionary biologist and geneticist John Haldane proposed the concept of a "primordial soup"1,2, describing the primitive terrestrial oceans containing organic compounds that may have facilitated chemical evolution. However, it wasn't until the 1950s when chemists began to conduct deliberate laboratory studies aimed at understanding how organic molecules could have been synthesized from simple starting materials on the early Earth. One of the first reports to this end was the synthesis of formic acid from the irradiation of aqueous CO2 solutions in 19513.
In 1952, Stanley Miller, then a graduate student at the University of Chicago, approached Harold Urey about doing an experiment to evaluate the possibility that organic compounds important for the origin of life may have been formed abiologically on the early Earth. The experiment was conducted using a custom-built glass apparatus (Figure 1A) designed to simulate the primitive Earth. Miller's experiment mimicked lightning by the action of an electric discharge on a mixture of gases representing the early atmosphere, in the presence of a liquid water reservoir, representing the early oceans. The apparatus also simulated evaporation and precipitation through the use of a heating mantle and a condenser, respectively. Specific details about the apparatus Miller used can be found elsewhere4. After a week of sparking, the contents in the flask were visibly transformed. The water turned a turbid, reddish color5 and yellow-brown material accumulated on the electrodes4. This groundbreaking work is considered to be the first deliberate, efficient synthesis of biomolecules under simulated primitive Earth conditions.
Figure 1. Comparison between the two types of apparatuses discussed in this paper. The classic apparatus used for the original Miller-Urey experiment (A) and the simplified apparatus used in the protocol outlined here (B). Click here to view larger image.
After the 1953 publication of results from Miller's classic experiment, numerous variations of the spark discharge experiment, for example using other gas mixtures, were performed to explore the plausibility of producing organic compounds important for life under a variety of possible early Earth conditions. For example, a CH4/H2O/NH3/H2S gas mixture was tested for its ability to produce the coded sulfur-containing α-amino acids, although these were not detected6. Gas chromatography-mass spectrometry (GC-MS) analysis of a CH4/NH3 mixture subjected to an electric discharge showed the synthesis of α-aminonitriles, which are amino acid precursors7. In 1972, using a simpler apparatus, first introduced by Oró8 (Figure 1B), Miller and colleagues demonstrated the synthesis of all of the coded α-amino acids9 and nonprotein amino acids10 that had been identified in the Murchison meteorite to date, by subjecting CH4, N2, and small amounts of NH3 to an electric discharge. Later, using this same simplified experimental design, gas mixtures containing H2O, N2, and CH4, CO2, or CO were sparked to study the yield of hydrogen cyanide, formaldehyde, and amino acids as a function of the oxidation state of atmospheric carbon species11.
In addition to the exploration of alternative experimental designs over the years, significant analytical advances have occurred since Miller's classic experiment, which recently aided more probing investigations of electric discharge experimental samples archived by Miller, than would have been facilitated by the techniques Miller had access to in the 1950s. Miller's volcanic experiment12, first reported in 19554, and a 1958 H2S-containing experiment13 were shown to have formed a wider variety, and greater abundances, of numerous amino acids and amines than the classic experiment, including many of which that had not been previously identified in spark discharge experiments.
The experiment described in this paper can be conducted using a variety of gas mixtures. Typically, at the very least, such experiments will contain a C-bearing gas, an N-bearing gas, and water. With some planning, almost any mixture of gases can be explored, however, it is important to consider some chemical aspects of the system. For example, the pH of the aqueous phase can have a significant impact on the chemistry that occurs there14.
The method described here has been tailored to instruct researchers how to conduct spark discharge experiments that resemble the Miller-Urey experiment using a simplified 3 L reaction vessel, as described in Miller's 1972 publications9,10. Since this experiment involves a high voltage electric arc acting on inflammable gases, it is crucial to remove O2 from the reaction flask to eliminate the risk of explosion, which can occur upon combustion of reduced carbon-bearing gases such as methane or carbon monoxide, or reaction of H2 with oxygen.
There are additional details that should be kept in mind when preparing to conduct the experiment discussed here. First, whenever working with glass vacuum lines and pressurized gases, there exists the inherent danger of both implosion and over-pressuring. Therefore, safety glasses must be worn at all times. Second, the experiment is typically conducted at less than atmospheric pressure. This minimizes the risk of over-pressuring the manifold and reaction flask. Glassware may be rated at or above atmospheric pressure, however, pressures above 1 atm are not recommended. Pressures may increase in these experiments as water-insoluble H2 is liberated from reduced gases (such as CH4 and NH3). Over-pressuring can lead to seal leakage, which can allow atmospheric O2 to enter the reaction flask, making it possible to induce combustion, resulting in an explosion. Third, it should be borne in mind that modification of this protocol to conduct variations of the experiment requires careful planning to ensure unsafe conditions are not created. Fourth, it is highly recommended that the prospective experimenter read through the entire protocol carefully several times prior to attempting this experiment to be sure he or she is familiar with potential pitfalls and that all necessary hardware is available and in place. Lastly, conducting experiments involving combustible gases require compliance with the experimenter's host institution's Environmental Health and Safety departmental guidelines. Please observe these recommendations before proceeding with any experiments. All steps detailed in the protocol here are in compliance with the authors' host institutional Environmental Health and Safety guidelines.
1. Setting Up a Manifold/Vacuum System
2. Preparation of Reaction Flask
3. Introduction of Gaseous NH3
4. Introduction of CH4
5. Introduction of Further Gases (e.g. N2)
6. Beginning the Experiment
7. End of Experiment
8. Collecting Liquid Sample
9. Cleaning the Apparatus
10. Sample Analysis
Note: When preparing samples for analysis, the use of an acid hydrolysis protocol such as has been described in detail elsewhere15, is useful for obtaining more amino acids. Hydrolysis of a portion of the recovered sample provides the opportunity to analyze both free amino acids as well as their acid-labile precursors that are synthesized under abiotic conditions.
The products synthesized in electric discharge experiments can be quite complex, and there are numerous analytical approaches that can be used to study them. Some of the more commonly used techniques in the literature for analyzing amino acids are discussed here. Chromatographic and mass spectrometric methods are highly informative techniques for analyzing the complex chemical mixtures produced by Miller-Urey type spark discharge experiments. Amino acid analyses can be conducted using o-phthaldialdehyde/N-acetyl...
Numerous steps in the protocol described here are critical for conducting Miller-Urey type experiments safely and correctly. First, all glassware and sample handling tools that will come in contact with the reaction flask or sample need to be sterilized. Sterilization is achieved by thoroughly rinsing the items in question with ultrapure water (18.2 MΩ cm, <5 ppb TOC) and then wrapping them in aluminum foil, prior to pyrolyzing at 500 °C in air for at least 3 hr. Once the equipment has been pyrolyzed and while prepa...
The authors declare no competing financial interests.
This work was jointly supported by the NSF and NASA Astrobiology Program, under the NSF Center for Chemical Evolution, CHE-1004570, and the Goddard Center for Astrobiology. E.T.P. would like to acknowledge additional funding provided by the NASA Planetary Biology Internship Program. The authors also want to thank Dr. Asiri Galhena for invaluable help in setting up the initial laboratory facilities.
Name | Company | Catalog Number | Comments |
Glass Plugs for Manifold | Chemglass | CG-983-01 | |
High Vacuum Grease | Apiezon | N/A | Type M/N |
Silicon High Vacuum Grease | Dow Corning | 1597418 | |
Teflon PFA Tubing | McMaster-Carr | 51805K54 | |
Ultra-Torr Vacuum Fittings | Swagelok | SS-4-UT-6 | |
Dry Scroll Vacuum Pump | Edwards | A72401905 | |
U-Tube Manometer | Alta-Robbins | 100SS | |
Tungsten Electrodes | Diamond Ground Products | TH2-1/16 | 2% thoriated |
Methanol | Alfa Aesar | N/A | Ultrapure HPLC Grade |
Teflon-Coated Magnetic Stir Bar | McMaster-Carr | 5678K127 | |
Gaseous NH3 | Airgas | AMAHLB | 99.99% purity |
Gaseous CH4 | Airgas | ME UHP300 | 99.99% purity |
Gaseous N2 | Airgas | NI UHP300 | 99.999% purity |
Tesla Coil | Electro-Technic Products | 15001 | Model BD-50E |
24 hr Plug-in Basic Timer | General Electric Company | 15119 | |
Cleaning Detergent | Alconox | 1104 | |
Toluene | Thermo Fisher Scientific | N/A | Optima Grade |
Luna Phenyl-Hexyl HPLC Column | Phenomenex | 00G-4257-E0 | Brand: Luna |
Formic Acid | Sigma-Alrich | F0507 | Used to make 50 mM ammonium formate |
Zapytaj o uprawnienia na użycie tekstu lub obrazów z tego artykułu JoVE
Zapytaj o uprawnieniaThis article has been published
Video Coming Soon
Copyright © 2025 MyJoVE Corporation. Wszelkie prawa zastrzeżone