The door at
the front of the courtroom opened and the judge entered. A court officer said: "All
rise," and, then, a short time later: "Please, be seated."
"You
may continue with your examination of the witness, Mr. Mayfield," Judge Arnsberger
directed. "I should remind the witness that he is still under oath."
"Dr.
Yardley, I believe," indicated the prosecutor, "you were talking about
meteorites and carbonaceous chondrites before the recess. Would you continue on with your
testimony, please."
"Actually,"
the professor stated, "I was just about to begin talking about something else when
the recess was announced. As I suggested earlier in my testimony, meteorites, comets and
interplanetary dust particles are only one approach to explaining the presence of various
kinds of hydrocarbons, both simple and complex, in the prebiotic environment of early
Earth history. The other approach, to which I will now turn, concerns the chemical
processes which are believed by evolutionary biologists to have been operating prior to,
but which eventually brought about, the advent of biological organisms.
"Serious
experimental work in the area of prebiotic chemistry has been going on for nearly
forty-five years in laboratories all over the world. Symposia and conferences dedicated to
this subject take place on a regular basis, and, in addition, there are academic journals
that publish articles dealing with virtually every facet of the prebiotic chemistry in
which life is believed to have had its origins.
"Obviously,
I cannot possibly present all of that material at this time. What I can do, however, is to
try to provide some of the broad brush strokes of the picture being painted by
researchers.
"Although
a few scientists, such as Alexander Oparin, in the Soviet Union, and J.B.S. Haldane, in
England, had been doing work on this topic during the 1930s, many people cite the
early-1950s work of Stanley Miller and Harold Urey at the University of Chicago as marking
the real beginning of serious investigation of the conditions necessary for the chemical
origins of life. They were the first to put things to the test under laboratory
conditions.
"In an
oft-cited, classic experiment, Miller gathered some gases, such as methane (CH4)
and ammonia (NH3), believed to be present in the early Archean era atmosphere,
subjected these gases to a continuous spark discharge, which was intended to simulate the
action of lightening, and examined the results after a number of days. The laboratory
procedure had generated a variety of amino acids, some of which are found in living
organisms and some which are not present in life on Earth.
"Amino
acids are complex hydrocarbons. They consist of three parts.
"One
part is a carboxyl group, having a formula of COOH. A second component is an amino group
with a formula of NH2.
"The
third aspect of the amino acid is a side chain. This varies, in a unique way, with each,
different amino acid.
"Some
16-17 years after Miller's experiment, the Murchison meteorite was found in 1969, and
scientists were able to demonstrate a number of similarities between the products of
Miller's experiment and the hydrocarbons found in the meteorite. For instance, they
discovered that the kind and quantities of amino acids found in the Miller experiment were
very, very similar to the kind and quantities of amino acids found in the meteorite.
"In any
case, by 1953, Miller had produced the first experimental evidence that natural chemical
processes could produce complex organic compounds which are fundamental to life on Earth.
Over the next forty-odd years many other experimental results would be forthcoming from
Miller and other researchers.
"In one
series of experiments, Miller and Urey discovered that roughly 10% of the carbon molecules
contained in the gases of their experimental set-up eventually were converted into known
organic compounds. Furthermore, as much as 2% of this converted carbon was involved in the
generation of amino acids within the experimental apparatus."
The
prosecutor, Mr. Mayfield, who had been listening intently to the professor, suddenly came
to life, so to speak, and said: "Dr. Yardley, earlier you had indicated that an
oxidizing atmosphere - in other words, an atmosphere composed of, say, oxygen, which
strips other compounds of hydrogen, tends to interfere with chemical processes that build
complex hydrocarbons from simple hydrocarbons. Is there a name for the sort of atmosphere
which is conducive to the generation of complex hydrocarbons from simple ones?"
"Yes,"
he replied, "the kind of atmosphere to which you are referring is known as a reducing
atmosphere. Such an atmosphere is dominated by molecules that can donate hydrogen atoms,
or, more precisely, electrons, to other substances.
"Methane
and ammonia, the gases used in Miller's experiment, are both considered to be relatively
good reducing agents. This means they tend to be involved in chemical reactions involving,
to simplify things somewhat, the donation of some of their hydrogen atoms or electrons,
which then interact with other hydrocarbon compounds to help make possible, under the
appropriate conditions, the formation of even more complex hydrocarbon molecules.
"In one
sense, all organic compounds are actually different gradations of reduced forms of carbon.
Generally speaking, this is due largely, although not necessarily always, to the presence
of hydrogen in such compounds.
"Creating
different kinds of reducing atmospheres under experimental conditions, investigators were
able to produce a variety of amino acids. Glycine, valine, alanine, proline, glutamic acid
and aspartic acid all have been generated through different kinds of electric discharge
experiments.
"In
another experiment, when sunlight was passed through a solution of paraformaldehyde (CH2O)3,
ammonia (NH3), and ferric chloride, the amino acids asparagine and serine were
produced. On the other hand, when solid ammonium carbonate was exposed to high doses of
gamma rays, small quantities of the amino acid glycine, along with formic acid (HCOOH),
resulted.
"In
1961, another scientist, Juan Oro wondered if amino acids could be generated under
laboratory conditions if one used chemical processes which were even simpler than those
involved in Miller's earlier experiments. Previous experiments had proven that if one
exposed a mixture of hydrogen, nitrogen and carbon monoxide gases to a spark discharge,
the reaction would yield hydrogen cyanide (HCN), which is a very reactive intermediate
compound.
"Oro
combined hydrogen cyanide with ammonia (NH3) and water (H2O). This
chemical reaction produced a number of different amino acids, just as the Miller
experiment had.
"In
addition, among the product residues of his experiment, Oro discovered something else.
This molecule was a purine, a nitrogen-containing base of considerable importance.
"The
particular purine found by Oro is known as adenine. This molecule is one of two purine
bases having a general formula of C5H4N4, and three
pyrimidine bases, each of which has a general formula of C4H4N2.
When any of these are combined with either of the pentose sugars, ribose or deoxyribose,
together with a phosphate group, then, RNA or DNA is produced.
"Adenine
is also one of the components of adenosine triphosphate. This latter molecule is one of
the fundamental energy-providing compounds in most organisms.
"In
addition to adenine, a number of other useful products could be produced by means of
reactions involving hydrogen cyanide. These products included a variety of intermediate
precursor molecules that constitute steps on the way to purine- or pyrimidine-formation,
and the products of the reactions included, as well, a number of pyrimidine base molecules
which are found in the nucleic acids of some, but not all, living organisms.
"Subsequent
experiments demonstrated the possibility of generating, through natural chemical
processes, the other nucleic acid bases- namely, uracil, cytosine, guanine and thymine,
that are found in the vast majority of organisms on Earth. These reactions also started
with hydrogen cyanide (HCN), but they required, as well, the presence of two other simple
carbon compounds: cyanogen (C2N2) and cyanoacetylene (HC3N),
which are believed to have been present on the prebiotic Earth.
"Still
other experiments were able to demonstrate that the pentose sugar, ribose, an important
component of RNA, could be produced quite easily. This chemical process merely involved a
series of spontaneous reactions involving molecules of formaldehyde CH2O.
"Again
and again, scientists were showing, experimentally, the possibility of starting with
simple compounds and combining them to produce complex hydrocarbons. More importantly,
these products were not just arbitrary molecules, but, rather, they were fundamental
building blocks of compounds, such as proteins and nucleic acids, that are crucial to the
life process.
"Researchers
felt their laboratory experiments were recreating the conditions of prebiotic Earth and
demonstrating that chemical reactions important to the origins of life would occur
spontaneously. The whole process was relatively simple and straightforward.
"Initially,
for example, atmospheric gases, such as methane and ammonia, would react together to
generate a variety of simple hydrocarbons, like hydrogen cyanide and molecules known as
aldehydes, which are compounds that contain a CHO group - such as formaldehyde (CH2O).
Next, the products of the first round of reactions- namely, aldehydes, hydrogen cyanide
and ammonia, would enter into a second round of chemical interactions which would result
in such intermediary products as amino nitriles. These products, in turn, would react with
the water of the ocean to produce ammonia and amino acids, like glycine.
"People
such as Sidney Fox were able to discover, experimentally, alternative methods for the
prebiotic generation of various kinds of amino acids - methods which were different from
the ones outlined by Miller and Oro. When Fox heated urea [CO(NH2)2]
and malic acid (C4H6O5) at temperatures of 150 degrees
Celsius, he was able to obtain aspartic acid.
"Fox
also was able to construct chains of amino acids through a process of thermal
copolymerization or cooking. He referred to these chains of amino acids as 'protenoids'
because they had certain structural similarities to the proteins found in living
organisms.
"The
recipe for thermal copolymerization of amino acids is fairly simple. One starts with some
quantity of a given amino acid, such as glutamic acid.
"One
places this quantity of amino acids in an oil bath and heats it at 170 degrees Celsius for
an hour. When the timer goes off after an hour, one blends in a finely ground mixture of
other kinds of amino acids.
"One
heats this new mixture for an additional three hours at the same temperature as before. In
addition, one heats it in an atmosphere of carbon dioxide.
"When
the mixture has cooked for the requisite period of time, one allows it to cool under
controlled conditions. When it is ready, one can examine the residue of this process and
find polymerized or chemically linked sequences of amino acids of varying length and
composition.
"Many
of the protenoid polymer chains consisted of up to 100 amino acids. The nature of the
bonds linking the amino acids varied in character, but some peptide linkages, the kind
which occur in proteins in living organisms, were observed among these bonds.
"The
thermal copolymerization process is capable of providing yields, by weight, of up to
fifteen percent of the total mixture. These portions are considered by evolutionary
biologists to be quite ample yields, although most of the rest of us may feel them to be
too small to share with friends for a late night snack.
"There
are variations on the foregoing recipe. Glutamine, another of the amino acids occurring in
living organisms, is substituted for glutamic acid. Phosphoric acid is also added.
"In
addition, one skips the step of pre-heating prior to the adding of other ground-up amino
acids. Everything else stays, more or less, the same, yielding roughly similar results as
before.
"One
can play around with parameters such as the temperature and time, at which and for which,
respectively, the mixture is cooked. One also can alter the ratios of the reactants and/or
phosphoric acid to be used in the process.
"Experiments
focusing on the manipulation of these variables have permitted protenoids with different
kinds of character to be produced. For example, one can increase the percentage of neutral
and basic amino acids that were incorporated into the polymerized chain.
"In
1977, a scientist by the name of Usher, demonstrated that when one used relatively low
temperatures, one could generate phosphodiester bonds between the phosphate and ribose
sugar portions of nucleic acids. This is an important step in generating fully functional
DNA and RNA molecules.
"In
1978 Juan Oro showed, experimentally, that if one heated fatty acids, an important
building block of lipids, and then dried them in the presence of phosphate and glycerol,
one could synthesize simple phospholipids. Phospholipids are fundamental to the formation
of cell membranes in most living organisms.
"Stanley
Miller has synthesized a compound under prebiotic conditions which is known as
pantetheine. This molecule has been observed to link amino acids in some organisms.
"Many
of the compounds produced in these kinds of experiment are quite soluble in water.
Researchers have hypothesized that these molecules, at one point or another, probably
would have gone into solution in the ocean, and, later, they would have become part of
more concentrated solutions when washed, by winds and tides, into the margins of marine
lagoons, tidal pools and other intertidal regions, from which water was being evaporated.
"This
process of enhanced concentrations through evaporation is thought to be important by many
researchers since, quite frequently, the presence of water seems to inhibit the process of
polymerization or chaining of, say, molecules. Sidney Fox, along with other scientists,
has found, for example, that in order to bring about the polymerization of amino acids,
the conditions within the experimental apparatus should be anhydrous, that is, done in the
absence of water."