Ask
evolutionary biologist Christopher Wills and organic chemist Jeffrey Bada,
who are studying the origin of life on earth at the University of California,
San Diego, to define life and both will answer, "an autonomous self-replicating
system that replicates imperfectly via natural selection." Key for
this pair is understanding how the abiotic or non-living world developed
into the biotic one. Co-authors of The Spark of Life: Darwin and the
Primeval Soup (2001), Wills and Bada believe life could arise only
in optimal conditions and over a significant period of time.
Between 7 and 4.6 billion years ago the earth took shape during the formation
of our solar system. The earth’s first aeon lasted between 4.6 and
3.8 billion years ago and is called the Hadean. The Hadean encompasses
800 million years of intense heat in which the earth’s core, mantle,
and crust formed. Over the next 300 million years, the planet cooled,
oceans formed, and land masses were created from volcanic eruptions and
earthquakes. Gases from the eruptions helped build an atmosphere of hydrogen,
methane, ammonia, and water vapor. Soon, ocean tides pushed onto land
and there, in tide pools, the first experiments in organic chemistry led
to life at the molecular level. The most advanced of the experiments came
when amino acids and short chains of nucleic acids accumulated to form
protoorganisms. Through natural selection, protoorganisms eventually developed
into single-celled entities, carrying instructions in their DNA and RNA
to replicate.
Recognizing life is easy: it wiggles and wanders about, it reproduces—and
seldom blushes. But ask Wills when life first occurred and he will answer,
the question is "troubling," even "infuriating." All
scientists are drawn to the unfathomable, Wills told me in a series of
interviews. In his 60s, the English-born, Canadian-raised biologist has
been teaching and researching evolution at UCSD for more than 30 years,
writing books about plagues, genes, and divers subjects. Studying the
origin of life, he says, "is so difficult that biologists have tended
to shy away from it."
Bada echoes Wills’s opinion. "When I talk to the lay public
about the origin of life, I’m talking about something that can’t
be seen even with the best microscope." The mid-western Bada, who
is also in his 60s and has taught at Scripps Institution of Oceanography
since 1970, concentrates on the chemistry of amino acids in marine environments
and on exobiology, the search for extraterrestrial life—not Klingons
but unseeable organic compounds that have evolved "in the solar system
and beyond." For the past 10 years, Bada has directed NASA’s
Specialized Center of Research and Training in Exobiology, a program whose
goal is to find "the importance of extraterrestrial input on the
primitive Earth."
And yet as impressive as their bios are, both men still face a monumental
problem. If biological evidence that developed during the Earth’s
first billion years has been ground to dust in the maws of the planet’s
tectonic plates, how can we be reasonably sure that life originated in
one particular way? The answer is, we cannot be sure—not scientifically.
We can only hypothesize.
Part of the trouble in Origin City comes from how we think about origins
as a culture. The popular (and paltry) imagination sees origins in facile
mechanistic terms, like a car equipped with an ignition switch. In her
1818 novel Frankenstein Mary Shelley never shows us Victor Frankenstein
creating the eponymous monster. Her Promethean doctor assembles his Creature
from pieces of corpses but is never seen to flip any switch. Instead,
he merely states, "After days and nights of incredible labour and
fatigue, I succeeded in discovering the cause of generation and life;
nay, more, I became myself capable of bestowing animation upon lifeless
matter." About the only science the occult-driven Frankenstein engages
in is galvanism—the 19th century conceit that beings could be helped,
even brought to life, via electric current.
The origin of life has also been "explained" as either inexplicable
or divine, limbs of the same body. The Bible and other tracts—philosophic,
spiritual, religious—argue that there’s no argument as to
how life got started: God did it (quickly not slowly), and that’s
that. Lack of evidence seems to make a purposive creation more probable.
Until the past two decades, simplistic explanations of life’s origin
have guided scientists. An agnostic Darwin ends his Origin of Species
by writing that "the Creator" breathed life "originally
into a few forms or into one." That hardly sounds like an evolutionist.
Up to and during Darwin’s time, scientists and theologians
believed life sprung into being via spontaneous generation, which is similar
to galvanism. Frogs born of the mud they wallow in, for example. I recall
hearing the news conference, two days before the July 20, 1969 moon landing,
during which Wernher von Braun, the German rocket engineer, said that
the feat was "equal in importance to that moment in evolution
when aquatic life came crawling up on the land" (italics added).
In the 2000s, a smattering of researchers, among them Michael Behe, have
bivouacked a new anti-evolutionary camp called "intelligent design."
The group contends that evolution could not have built a system as sophisticated
as a first cell. It is, in Behe’s words, "irreducibly complex."
Any structure that exceptional had to have sprung fully formed. In short,
a miracle.
There’s nothing miraculous about the United States income tax code.
The code is a self-enabling system that no one understands except a certain
caliber of tax attorney, who alone is capable (to our benefit and peril)
of managing its recondite regulations. Even (former) Secretary of the
Treasury Paul O’Neill hires a tax accountant. The tax code can be
said to have "a life" because it is so highly complex and evolved.
In fact, its complexity is the result of its development, a 90-plus-year
accretion of more (never fewer) regulations. The tax code didn’t
happen over night and it certainly wasn’t intelligently designed.
As the tax code did in one century, life seeped into being during its
10 to 200 million-year prime. Wills has called this variable interval
no more than "a moment." But it is a moment that, in his thinking
and research, he has tried "to blur," propounding a series of
stages and a number of locales—in the molecular world and on the
earth’s surface—for creation to begin. To shape the multiple
endeavors of life—breeding, mutation, survival—only a process
is possible. Not a birth, but a very slow arrival.
***
Around 14 billions years ago, the universe originated with
the Big Bang. Seven billion years later our solar system began to form.
The materials which would become the earth accumulated: from space dust,
gases, meteorites, and comets comprising frozen gases and ice. Eventually,
the planet orbed into a sphere and its circling around the sun became
fixed by gravity.
As the planet formed, the continual volley of meteorites and the decay
of the planet’s radioactive elements created intense heat. In such
heat, heavier elements sank. The core that drew down iron and nickel was,
itself, soon bounded by a lower-density mantle. The silicates rose or
stayed on the surface and, eventually, the surface cooked up a crust.
The heat and pressure on the crust, however, was so great that it cracked
into plates. The mantle’s circulating heat, called convection currents,
pushed the plates—inches over centuries. This snail-paced but inexorable
drift would form and separate continents.
Toward the end of the Hadean period, meteorites slowly stopped bombarding
the earth. Free from assault, the crust solidified. The earth’s
atmosphere developed, coalescing at first into a smoggy concentration
of hydrogen, methane, ammonia, and water vapor, which nearly blotted out
the sun. Hydrogen, the lightest element, escaped into space, and methane
and ammonia, supplied from outgassing volcanoes, became unstable and converted
to carbon dioxide and nitrogen. Regulating the build-up and retention
of the atmosphere was the relative size of the earth and its gravity.
Had the earth been smaller, even the heaviest gasses would have leaked
into space.
Without meteor showers, the earth began to cool. In the atmosphere, water
vapor condensed and fell as rain. During a deluge that lasted more than
100,000 years, the planet’s surface depressions flooded, and global
oceans were formed. The crust, much of it now underwater, hardened as
it inched along, while in the downpour the heavier elements gravitated
to the ocean basins. The creation of the oceans was fundamental to the
onset of life.
Wills and Bada describe the early earth as a "water world,"
punctuated by emerging land areas on which "mighty tides" washed
in and out. "On islands that happened to stand athwart these massive
movements of water," they write, "the tides could easily have
swept across far wider regions than would be accessible to the tides of
today." They believe these "enormous tidal floods" may
have moved "in predictable patterns." And here, in the tidal
washing of the land’s surface, the "synthesis and sorting of
organic compounds" began.
Organic compounds, common to all living organisms, are substances that
contain carbon. Atoms of carbon most often bond with atoms of hydrogen,
nitrogen, or oxygen, and create an almost endless variety of compounds.
Amino acids are organic compounds, which, when linked, form proteins.
Twenty amino acids are found in living organisms. Just as amino acids
build proteins, nucleobases—another kind of organic compound—build
the large molecules DNA and RNA.
Scientists speculate that organic compounds may have originated in the
oceans, from outer space, or in an oil slick that once covered the earth.
Organic compounds may have arisen from hydrothermal vents, or undersea
openings, where the crust is thin and superheated water produces chemical
reactions. They may have ridden in on particles of cosmic dust, which
have been showering the planet throughout its existence. We know today
that organic compounds piggyback to earth on meteorites. A meteorite that
fell near Murchison, Australia, in 1969, contained several of the building
blocks of life, including amino acids and some of the nucleobases in DNA
and RNA. It is these meteor-moored compounds that Bada has explored on
this planet and plans to investigate in 2011 when soil and rock samples
are returned from Mars. Bada, who has helped design the module that will
retrieve those samples, hopes to uncover evidence of simple molecules
on Mars that may have contributed to the building blocks of life on earth.
The third source of organic compounds may have been a planet-wide oil
slick several meters thick. "The most abundant component," Wills
and Bada write, "must have been tarry material," which, "tended
to coagulate into gooey lumps or films." They describe the surface
of the earth as "one giant Exxon Valdez disaster."
The slick "could have been like a giant time-release capsule, continuously
supplying adenine and amino acids to the oceans of the early Earth."
Eventually, the oil would have "congealed into tar and then been
broken down slowly by sunlight." But the ocean would have retained
the organic compounds created in the tar.
Whether synthesized here or flown in from elsewhere, this grand stew of
organic material was cooked during what’s called the prebiotic
period, a post-Hadean time some 200 million years long.
Could
it be that finding the right balance among the oceans, the island chains,
the atmosphere, and the size and gravity of the earth was necessary for
life to begin? Wills and Bada say this may be part of the equation. They
cite the Gaia hypothesis, formulated in 1975 by British chemist
James Lovelock and American biologist Lynn Margulis, and named for the
Greek goddess of the earth. Gaia suggests that earth is a biosphere where
carbon-rich sediments and a carbon-cycling system regulate the temperature.
"Variations on the Gaia theme," write Wills and Bada, "may
account for the Earth’s apparent ability to keep to a narrow range
of temperatures as the Sun has gradually warmed over the last four billion
years." But this hypothesis only works with "living organisms":
Protoorganisms had to evolve before the earth became self-regulating.
Indeed, for millions of years, the first life-creating system, in order
to reach some level of organization, had to battle a severely inhospitable
terrestrial environment.
***
As collaborators, Christopher Wills and Jeffrey Bada are working in what
may be a golden age of life sciences at UCSD. The campus has nurtured
a host of chemists and biologists who continue to hothouse new ideas about
life and its origins. The most celebrated pair of UCSD biochemists are
Stanley Miller and Harold Urey (Miller died in 2007; Urey in 1981). Under
Urey’s tutelage, Miller, while a graduate student at the University
of Chicago in 1953, synthesized amino acids by replicating the supposed
prebiotic conditions of the earth—several gasses (hydrogen, ammonia,
methane), a little water, an electrical charge, and no oxygen—in
a bi-level rigging of glass flasks. Having taught at UCSD since 1958,
Miller has, among other things, worked on dating the origin of life within
a 10-million-year time-frame. (The Spark of Life is dedicated
to Miller.) Nobel laureate and double helix codiscoverer Francis Crick
researched genes at the Salk Institute until his death in 2004. Also at
Salk is Sydney Brenner, who discovered, with Crick and others, messenger
RNA, a genetic strand that orders the amino acids in proteins. Still another
Salk veteran was Leslie Orgel (died in 2007), who made nucleic acid polymers
and is researching a "first gene" that copied itself before
complex protein catalysts evolved. And Gustaf Arrhenius of Scripps Institution
of Oceanography, having collected carbon isotope evidence from rocks in
Greenland, claims that life has existed for 3.8 billion years.
Each of these scientists has struggled with Wills’s "infuriating"
question about the origin of life: How did organic molecules "come
together" to make a protoorganism?
Some scientists, like Leslie Orgel, argue that one day there appeared
a "naked gene on the beach," which had already fully formed
in the oceans or on "the surface of some mineral particles."
It’s been proposed that this gene, Wills and Bada write, "was
capable of making copies of itself from the building blocks supplied by
the primordial soup. . . . The genetic material grew in size and complexity,
coding for more and more compounds, with which it surrounded itself."
Wills and Bada, however, discount this theory. They believe "a limited
amount of organization" had to have "appeared in the molecular
world" before genes developed.
Another idea is that life sprung into action in what Bada portrays as
a "self-sustained little chemical factory." The enclosed factory
would have been composed of only metabolizing molecules. But Bada disagrees
that such an isolated structure could have advanced and labels the idea,
"life as we don’t know it."
Wills and Bada contend that the molecular precursors of a first self-replicating
entity rooted themselves on the shores of a vast percolating ocean-soup.
For millions of years, organic compounds had gathered in the soup. The
compounds were then splashed for millions of more years onto the intertidal
zones of the emerging land masses. There, in the tidal zones, formed what
Wills calls an "ill-smelling residue," a mineral-rich "organic
scum." This scum would have settled in nooks and crannies on the
rocky shore.
As more and more molecules aggregated in the scum, organic compounds would
have begun to produce more complex groups. For example, write Wills and
Bada, "in those early tidal flats, wherever amino acids and sugars
were concentrated," a "brownish polymer," or repeating
chain of a simple molecular group, would have formed. The "accumulating
sugars could have provided some sort of protective function—perhaps
by producing a slimy impervious layer that would have repelled water as
tides and waves periodically swept by." Such a layer might have separated
groups of molecules.
One kind of protective layer that Wills and Bada believe developed early
on was a two-dimensional-like membrane. This membrane wasn’t like
the lipid or water-insoluble surface that houses a cell today. It was
a barrier between one group of molecules and another. Bada describes the
membrane as "sticky yet discrete," allowing for simple separation,
and Wills elaborates. These membranes were probably "made of a silky
material that floated about in the primitive soup. They would have had
[the equivalent of] an inside and an outside, across which charged differences
could be generated. [This would have led] to the charging up of these
molecules." Perhaps the membrane’s surface was composed of
one-half an amino acid that is negatively charged, which then attracts—to
interact or bond with—a surface of positively charged aminos. Charged
molecules may have combined and grown into energy-rich compounds that
became sources of food for other compounds.
With the mix of ocean surf and the deposit of more and more organic molecules
in the tide pools, "billions of tiny experiments" in life-making
got going. Wills and Bada hold that tidal action, an agent itself of constant
change, is essential to these experiments because on and within the scum
favorable and unfavorable aggregates of molecules began to be sorted.
Usually we associate a sorting-out process of favorable and unfavorable—the
fit and the less fit—with evolution. But Wills and Bada suggest
that "the sorting-out capability could somehow [have been] decoupled
from the reproductive capability" before life began, in what they
describe as "the molecular equivalent of birth and death." They
believe the stronger molecules stuck to the rocks and "lived"
while the weaker molecules got washed into the ocean and "died."
Initially, there was a simple piling-on of molecules. In the piles, however,
"different collections of molecules would have clung to different
types of particles" on the rocky surfaces, eventually "becoming
stratified according to their sizes and chemical properties."
These different collections, still being sorted out, resided in what Wills
and Bada call a "molecular ecosystem." Supported by this ecosystem,
a given robust collection of molecules may have been able to accomplish
several things at once: attract, with its stickiness and its charged surfaces,
other molecules coming in with the tides; absorb energy from sunlight
that would aid its development; and protect its expanding aggregate from
the ultraviolet light that would normally fry anything exposed.
***
We are now almost ready for the arrival. But, due to further complex development
of the first living organism, it may be easier to describe the newborn
before analyzing its composition. Wills and Bada adopted the term protobiont,
used by the Russian biochemist Aleksandr Oparin in his 1926 The Origin
of Life, to describe the first self-replicating entity in the molecular
ecosystem. The protobiont has several characteristics: it is an organized
collection of molecules; it can multiply "inside the complex, slimy
layers of molecules" that cling to the rocks; and it carries rudimentary
genetic information. The genes both house the protobiont’s hereditary
characteristics and transmit instructions for self-duplication.
Wills and Bada believe that the protobionts made a "skeleton,"
or platform, out of a group of molecules. The platform secured itself
by selecting (and affixing) the architecturally strongest organic compounds
from the primitive soup. To illustrate this link between protobiont and
environment, Wills offers—from much further up the evolutionary
ladder—the sea snail. With the calcium carbonate molecules of seawater
a snail builds a shell, a structure or platform within which it can survive.
"The ability to build the shell is coded in the snail’s genes,"
he says, "but the shell itself isn’t." The shell’s
materials must come from "outside the organism to enable the organism
to complete itself." In this way, the protobiont needed the village
of its environment in order to be raised.
The protobiont may have also contained what Wills and Bada describe as
a "fragment of genetic material [which was] made up of a short piece
of nucleic acid or a similar molecule." Whatever that genetic material
was, it was like DNA, the nucleic acid common to almost all life today.
We recall that DNA’s structure, the familiar spiraling double helix,
is also like a zipper. The sides of the zipper interlock, linking nucleobases
into base pairs: adenine with thymine, guanine with cytosine. The human
genome is built of 3.2 billion base pairs; the tiny bacterium, mycoplasma,
has 500,000 base pairs. Bada believes the first entity’s structure
contained just 30 to 50 base pairs. That was "the minimal size needed
to store information in this molecule. And, remember, it’s the sequence
of the bases that stores the information." As more bases linked,
the entity would have had more data to copy and more opportunity to mutate.
What information might have been stored first in the entity’s code?
Wills and Bada write that the "most primitive distinction that the
early genetic code must have made was between water-loving and water-hating
amino acids." If a molecule was coded to "love water,"
then it would have readily received organic compounds from the soup. If
a molecule was coded to "hate water," then it would have built
up a structure to repel water, helping the entity survive some of the
ocean’s pummeling action on the shores. As we have seen before,
the two kinds of molecules may have allowed the entity to do two life-enhancing
things simultaneously - grow and protect its growth.
One final sorting-out process remains - what Wills and Bada call, imperfect
replication. It’s essential to remember that our knowledge of prebiotic
chemistry is, as Wills laments, "full of so many missing steps [that]
it’s difficult to see how these steps might have happened."
It must have taken billions of chances for each step to occur - for cosmic
dust, hydrothermal vents, and a planet-wide oil slick to seed the primeval
soup with organic compounds; for ocean tides to begin pummeling the shores;
for organic compounds to stick and polymerize in the scum; for the protobiont
to develop fledgling nucleic bases that would remember bits and pieces
of themselves across a generation. The final step necessary for self-replication
would have been for the protobiont to evolve from copying a small part
of itself to copying enough of itself that it passed on a living and autonomous
organism.
"Life can’t get anywhere," Wills says, "if organisms
make exact copies of themselves." In order to get somewhere—that
is, to survive the severity of its environment—the protobiont was
forced to adapt. The primary source of adaptation for the protobiont came
through mistakes made while its genetic information was passed on. We
may grasp the theory of the protobiont, Wills says, by looking at "the
process of DNA replication itself. DNA is comprised of two strands that
spiral, or grow, with each other in the double helix. Suppose you have
a sequence of pairs that is A T. If the self-replicating DNA makes a mistake
and puts a G in place of the T, you have A G, or a mutation. In this way,
organisms acquire mutations and natural selection sorts these mutations
out. Humans," he continues, "are very good at repairing our
mistakes. We have all kinds of machines in the cell that repair mistakes.
As a consequence, we don’t have anywhere near the number of mutations
per unit time as the bacteria does."
Early on, the protobionts were, like bacteria, mutating at a very high
rate. In fact, before the protobiont became a living organism, different
sections of its genetic code, Wills says, must have "replicated extremely
imperfectly." At first the protobiont retained a very small percentage
of its precursor’s genes, which would not have specified "all
the information needed for a living organism." To retain more genes,
the protobiont may have evolved a better self-replicating system in which
it reduced the number of its mistakes. But once the protobiont had stabilized
its rate of mistakes, and enough genetic information was being copied
to "secure" its autonomy, then, as Wills and Bada write, this
"would have represented the first stirrings of life."
***
How long did it take for the protobiont to arrive? If protobionts were
bacteria-like in their mutative proliferation, wouldn’t that have
meant an extremely long time to evolve? Wills says no. In fact, he believes
life got going in less than 10 million years. He cites three reasons.
One is an idea developed by Stanley Miller. Miller has written that "life
must have arisen in 10 million years or less based on the known rate of
decomposition of organic compounds." In this inferno, organic molecules
"died" when, returned to the ocean, they were sucked through
the hydrothermal vents in the deep-sea trenches every 10 million years.
Second is that, at the molecular level, chemical reactions take place
very quickly. Combine this rapidity with the third reason: the growing
shoreline space of the young planet. While the protobiont was using its
10 million years to form and replicate, it also formed and replicated
in several billion places—those tiny terrestrial niches
where organic scum collected. If incipient life had only one chance in
a million billion chances in one locale, the likelihood of its developing
is very slim. But if that one chance had a million billion molecular eco-systems
within which to experiment, the odds are much better. Quite good, in fact.
Enough to cause Bada to say that there were probably "multiple origins
of life."
Let’s say that life originated around 3.8 billion years ago and
then took tens of millions of years to reach full autonomy or, as Wills
says, "be on its way." As it did, there would have been massive
amounts of decomposed organic compounds—those with "imperfect"
characteristics—available to "feed" it. On one hand that’s
a lot of feed; on the other hand, that’s a lot of dying, an area
which scientists, like doctors, seldom discuss. Why is unclear. Perhaps
it’s because decomposition is seldom studied under the biologist’s
microscope. Living matter attracts the majority of their scrutiny. But
the importance (not to mention the amount) of decomposition to the evolution
of life is prodigious.
Consider this oblique angle. Estimates suggest that the structure of DNA
was fixed more than 3 billion years ago. This includes the DNA of our
common ancestor in the bacterial realm. So what were the chances that
deoxyribonucleic acid developed its very particular sequence? In The
Fifth Miracle: The Search for the Origin and Meaning of Life (2000),
Paul Davies collects several metaphors to try to explain the unlikelihood
of life developing on earth as it did. Among them is a quotation from
the British astronomer Fred Hoyle who "likened the odds against the
spontaneous assembly of life to those for a whirlwind sweeping through
a junkyard and producing a fully functioning Boeing 747." The possible
combinations of billions and billions of interacting molecules to make
DNA are, as British zoologist Richard Dawkins is fond of intoning about
evolutionary possibilities in general, unimaginable but not incalculable.
DNA "against all odds" sounds fantasy-headed, like a George
Lucas movie. But, despite the relentlessness of earth’s geology,
DNA beat the odds. We know from the paleobiochemical record that virtually
all organisms—the estimate is greater than 99 percent—have
died out. We know that all protobionts have been annihilated by plate
tectonics. Hence, the self-maintaining biomolecule that came after the
protobiont was, up to that date, the most improbable entity to have gotten
that far. And still, no matter which organism got through, there is an
abyss between the one that made it and all those others that didn’t,
all those molecules that were recycled, all those mutations that dropped
off the turnip truck. Such loss is evolution’s stamp. To overproduce
the very many so the very few survive.
***
Christopher Wills says that perhaps the fiercest of the ongoing arguments
among origin-of-life researchers is whether an origin theory can be tested
in the lab. This fascinates him because, he says, "Every other science
is approachable in the lab, why not the origin." The success of Stanley
Miller’s 1953 experiment is precisely what attracted an array of
scientists to study life’s onset. By the middle of this century,
Wills believes, biochemists will in a series of headline-grabbing experiments
create life, and, thereafter, such experiments by high school kids will
be common. Wills imagine the biology teacher’s challenger to her
students, "‘Let’s see who can be the first in the class
to make life.’ I have a hunch it’s going to be far easier
than we think." And yet, he stresses, it has to be "ineluctably"
proven, so that people will accept the molecular ab ovo view.
To create life in the lab will be a momentous occurrence for two reasons:
first, because it may permanently alter the creationist view that God
is the only author; and second, because replication may be less complicated
than we thought since even high school kids will be able to do it.
Wills, of course, is not claiming that the mystery of creation will be
solved with such experiments; the exact conditions that gave rise to life
on the early earth are neither knowable nor reproducible. So what will
the lab-based synthesis of self-replicating organic compounds prove?
According to Loren Eiseley, a naturalist and author of The Immense Journey
(1957), not much. A demonstrable origin, for Eiseley, "suffers from
the defect of explaining nothing, even if it should prove true. It does
not elucidate the nature of life." Eiseley is pushed not so much
by the complexity of origin science as he is by "the loneliness of
a man who knows he will not live to see the mystery solved, and who, furthermore,
has come to believe that it will not be solved when the first humanly
synthesized particle begins . . . to multiply itself in some unknown solution."
For Eiseley the origin’s incredibly lucky conditions "will
never come again." And it’s this never coming again that broods
the egg. We—all creatures—are doomed to sit on what he calls
"the egg of night."
To illustrate the quandary, Eiseley writes, "My memory holds the
past, and yet paradoxically knows, at the same time, that the past is
gone and will never come again." Humans may be able to recognize
that the irreversibility of their own pasts resonates with the irreversibility
of life’s beginning. But, if DNA’s existence coincides almost
with that beginning, does DNA hold its past in the same way that an individual’s
memory holds its past? Is part of the genetic code of any biomolecule
a key for deciphering that biomolecule’s past? Or does the code
only give instructions for replication, that is, what will be?
It is possible that DNA has "remembered" its past, that a genetic
sequence may contain the origin’s right splash of atmospheric and
terrestrial conditions. But that sequence may have mutated through the
aeons as well as been buried and re-buried, ad infinitum. The origin of
life that may be locked in DNA appears to us like a million Rosetta stones,
concealed under a few billion years of planetary evolution.
No doubt a "knowable" origin has been entombed by what Paul
Davies calls "the carnage of natural selection." What seems
truly irreducible about the first biomolecule is that carnage is not only
programmed into its DNA—the overproduction and death of "too
many" organisms so that the very few survive—but that carnage
has been in motion so long that it has made the origin of that biomolecule
more inscrutable than it may be. Carnage also suggests the immense amount
of failure that is necessary to create and sustain life. The rate of mutation’s
failure to replicate life is many times that of the rate of mutation’s
success in continuing life. While the number of species alive today is
a few million, the number of extinct species, according to calculations
done in 1952 by paleontologist George Gaylord Simpson, is 500,000,000.
With such odds, no wonder every species and every bacteria tries every
trick in the book to ward off the hangman.
Merrily we mutate. Mercifully we die. Is that it? Mutation and death,
carnage and renewal, annihilation and rebirth—ultimately achieving
a kind of platitudinal purposelessness? All entities, whether they do
or don’t replicate, have to die with or without ascribing themselves
a purpose. Life may have no purpose because the "autonomous self-replicating
system" that drives the living bestows little more to do, in the
grand scheme, than accomplish the next round of autonomous and imperfect
self-replication. Is that purposeless? I don’t know. I do know that
because I’m drawn to summer’s resplendence out my window,
to the feathery top of a Eucalyptus bending in a coastal breeze, I think
(and it may only be my code) that the irredeemable fact of our
origin means very little.
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