The Origin of Life

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To account for the origin of life on our earth requires solving several problems: A number of theories address each of these problems.

Abiotic Synthesis of Organic Molecules

As for the first, three scenarios have been proposed: organic molecules
  1. were synthesized from inorganic compounds in the atmosphere
  2. rained down on earth from outer space
  3. were synthesized at hydrothermal vents on the ocean floor

1. Miller's Experiment

Stanley Miller, a graduate student in biochemistry, built the apparatus shown here. He filled it with

He hypothesized that this mixture resembled the atmosphere of the early earth. (Some are not so sure.) The mixture was kept circulating by continuously boiling and then condensing the water.

The gases passed through a chamber containing two electrodes with a spark passing between them.

At the end of a week, Miller used paper chromatography to show that the flask now contained several amino acids as well as some other organic molecules.

In the years since Miller's work, many variants of his procedure have been tried. Virtually all the small molecules that are associated with life have been formed:

One difficulty with the primeval soup theory is that it is now thought that the atmosphere of the early earth was not rich in methane and ammonia — essential ingredients in Miller's experiments.

2. Molecules from outer space?

The Murchison Meteorite

Representative amino acids found in the Murchison meteorite. Six of the amino acids (blue) are found in all living things, but the others (yellow) are not normally found in living matter here on earth. The same amino acids are produced in discharge experiments like Miller's.
Glycine Glutamic acid
Alanine Isovaline
Valine Norvaline
Proline N-methylalanine
Aspartic acid N-ethylglycine
This meteorite, that fell near Murchison, Australia on 28 September 1969, turned out to contain a variety of organic molecules including:

The question is: were these molecules simply terrestrial contaminants that got into the meteorite after it fell to earth.

Probably not:

The ALH84001 meteorite

This meteorite arrived here from Mars. It contained not only a variety of organic molecules, including polycyclic aromatic hydrocarbons, but — some claim — evidence of microorganisms as well.

Furthermore, there is evidence that its interior never rose about 40° C during its fiery trip through the earth's atmosphere. Live bacteria could easily survive such a trip.

Link to a discussion of the possibility of life on Mars and more on the ALH84001 meteorite.

Organic molecules in interstellar space

Astronomers, using infrared spectroscopy, have identified a variety of organic molecules in interstellar space, including

Laboratory Synthesis of Organic Molecules Under Conditions Mimicking Outer Space

There have been several reports of producing amino acids and other organic molecules by taking a mixture of molecules known to be present in interstellar space such as: and exposing it to

Whether or not the molecules that formed terrestrial life arrived here from space, there is little doubt that organic matter continuously rains down on the earth (estimated at 30 tons per day).

3. Deep-Sea Hydrothermal Vents

Some deep-sea hydrothermal vents discharge copious amounts of hydrogen, hydrogen sulfide, and carbon dioxide at temperatures around 100°C. (These are not "black smokers".) These gases bubble up through chambers rich in iron sulfides (FeS, FeS2). These can catalyze the formation of simple organic molecules like acetate. (And life today depends on enzymes that have Fe and S atoms in their active sites.)

Assembling Polymers

Another problem is how polymers — the basis of life itself — could be assembled.

Link to a discussion of enantiomers.

This has led to a theory that early polymers were assembled on solid, mineral surfaces that protected them from degradation, and in the laboratory polypeptides and polynucleotides (RNA molecules) containing about ~50 units have been synthesized on mineral (e.g., clay) surfaces.

An RNA Beginning?

All metabolism depends on enzymes and, until recently, every enzyme has turned out to be a protein. But proteins are synthesized from information encoded in DNA and translated into mRNA. So here is a chicken-and-egg dilemma. The synthesis of DNA and RNA requires proteins. So The discovery that certain RNA molecules have enzymatic activity provides a possible solution. These RNA molecules — called ribozymes — incorporate both the features required of life:
Link to a discussion of ribozymes.

While no ribozyme in nature has yet been found that can replicate itself, ribozymes have been synthesized in the laboratory that can catalyze the assembly of short oligonucleotides into exact complements of themselves. The ribozyme serves as both

(The figure is based on the work of Green and Szostak, Science 258:1910, 1992.)

In principal, the minimal functions of life might have begun with RNA and only later did Several other bits of evidence support this notion of an original "RNA world":

Reproduction?

Perhaps the earliest form of reproduction was a simple fission of the growing aggregate into two parts — each with identical metabolic and genetic systems intact.

The First Cell?

To function, the machinery of life must be separated from its surroundings — some form of extracellular fluid (ECF). Today, plasma membranes have this function. But perhaps the tiny (~1 mm) chambers in the hydrothermal vents — with walls that permit the free passage of small molecules but not macromolecules — might have provided a place to concentrate biomolecules away from the dilute solutions in the surrounding sea water. Perhaps plasma membranes were the last essential structure to complete the first true cells. In fact, the lipid composition of the membranes of bacteria and archaeans are so different that they may have evolved independently after the metabolic and genetic systems of their ancestor ("LUCA") had been established.

The Last Universal Common Ancestor (LUCA)?

The 3 kingdoms of contemporary life — archaea, bacteria, and eukaryotes — all share many similarities of their metabolic and genetic systems [Link]. Presumably these were present in an organism (or organisms) that were ancestral to these groups: the "LUCA". Although there are not enough data at present to describe LUCA, comparative genomics and proteomics reveal a closer relationship between archaea and eukaryotes than either shares with the bacteria. (Except, of course, for the mitochondria and chloroplasts that eukaryotes gained later from bacterial endosymbionts [Link].)
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8 June 2006