After decades or centuries
of concentration, some of the shoreline puddles and pools would
have contained significant concentrations of organic polymers of
various types. Some of these tarry or gelatinous blobs would have
remained in the concentrating puddles where they formed, and others
would have splashed into mixing puddles closer to the high tide
line, and attached there.
Most of the early molecular aggregates probably
were uninteresting organic masses with no sign of life to them. However,
some would have had molecules arranged in just the right way to give
them an interesting new property- catalytic activity.
The new organic catalysts wouldn’t have done anything directly
to start life, but they would have helped to increase the amount
of ‘interesting’ chemicals in the local soup. And those
local concentrations would later, indirectly, help with the earliest
life processes.
What’s a Catalyst?
In general, a catalyst is any material that
helps make a chemical reaction go faster. It can do that by providing
an electron or a proton temporarily, by bonding to one or both of
the starting compounds to create a temporary, intermediate state,
or by holding two molecules in the correct orientation so they can
react more easily. You might think of a catalyst as a ‘dating
service’ for shy molecules that uses soft music and teensy
bottles of alcohol to help them to interact faster.
Modern amino acid catalysts are called enzymes.
Some enzymes are extremely good at a particular type of reaction,
whipping through tens of thousands of reactions per second.
The typical enzyme has a 3-D structure which
can hold two molecules in just the right places for a reaction. Frequently
the enzyme will donate an electron or proton, to reduce the energy
barrier for the reaction. Sometimes a modern enzyme will donate a
bit of energy to speed a difficult reaction. It often has grooves
or holes to feed in the raw materials, and it may shift its conformation
to help a reaction move more effectively.
An enzyme may even be part of a larger ‘pipeline’ of
several enzymes which can take raw materials in at one end, and pump
a finished product out the other.
Of course the early proteinoid blobs in our
primordial shoreline puddles were not that good. They were just random
collections of molecules not ‘designed’ for catalytic
activity. Because of that, they were a far cry from modern enzymes.
Nevertheless, by sheer accident, some of them would have had catalytic
activity.
In fact, amino acid chains are particularly
likely to be able to catalyze some reaction, simply because they
usually have chemically active side chains, and also have an overall
structure which can hold those active groups in a rigid geometry
that has a reasonable chance of acting on some sort of organic reaction.
That might mean that an aggregate could have
some active groups that would synthesize one of the amino acids reliably
from common raw materials like ammonia and cyanide (or at least perform
one step in a multiple-step reaction). A catalyze might assist the
linking of two amino acids into a longer chain, or it might produce
some other organic chemical from simpler precursors.
Early Catalysts
Since the early organic blobs were probably
composed of a wide variety of compounds, there’s no reason
that this catalysis would have been based on just amino acids. Pretty
much any molecule in a polymer blob may have contributed to the catalytic
effect.
The catalytic activity might also be helped
by mineral or clay particles. In fact, some catalysis may have occurred
in pools containing clays or minerals arranged ‘just right’ to
speed up reactions, even before the organic blobs formed.
Let’s take a look at some of the issues for prebiotic catalysts.
How Big were the Catalysts?
The proteins used in modern day life are
quite large— they are usually composed of 300 to several thousand
amino acids. Modern enzymes are often grouped into even larger assemblies
with co-factors and supporting structures that may include tens of
thousands of amino acids and other molecules.
Modern enzymes are also extremely efficient,
with regulators, inhibitors and modifiers that help coordinate their
action with the other activities in a cell.
Of course the first organic catalysts were
composed of just a random mix of compounds, so it is highly unlikely
that they would have been as efficient as modern enzymes. They were
more likely to be ox carts instead of Ferraris.
If the first enzymes were stand-alone polypeptides,
most of them probably were no larger than the functional groups in
modern enzymes-- perhaps in the range of 10 to 50 amino acids long.
If they were bound to a larger glob of random
organic material or to a mineral particle, the first catalysts may
even have consisted of single amino acids or very short polypeptide
chains.
How Efficient were the Catalysts?
Most of the random, early catalysts were
probably not very efficient.
It’s important to remember that they occurred in a random world
of random chemicals, with random enzymatic groups positioned more
or less randomly in a puddle somewhere, filled with random ingredients.
Even if a catalytic blob had its active molecules
aligned perfectly for some sort of synthesis, it still would not
have catalyzed large number of reactions, simply because its raw
materials would not be present in sufficient quantities to drive
the reaction at its optimum speed.
Modern enzymes can be incredibly efficient— but that happens
because they are in a highly controlled environment with just the
right energy sources and ‘pipelines’ to deliver raw materials.
Modern enzymes are part of complex structures which have had a few
billion years of evolution to help perfect their functionality. That
kind of effectiveness was simply not available yet, in the early
shoreline puddles.
Most of the early catalysts would have been
very inefficient, and may have managed no more than a few reactions
per second, or even fewer.
In fact, catalysts generally work in both
directions, so in a purely random world, they would have decomposed
just as many molecules as they composed.
Of course even the most sluggish of enzymes
would still have contributed its products to its local pool, albeit
more slowly than a modern enzyme. Over a long time period, they would
have helped increase the quantities of ‘interesting’ organic
compounds, both in the tidal pools and in the oceans as a whole.
How many Catalysts Were There?
It would be very useful to know roughly how
frequent catalysts would have occurred in the early organic films
and blobs of the pre-biotic Earth.
Unfortunately, there is no clear answer to
this question.
Some experiments have demonstrated catalytic
action from random assortments of compounds that were probably present
in condensing puddles— for example, combinations of proteinoids
and iron salts , simple proteinoids , and short polymers of RNA-like
compounds .
There may have been extremely large numbers
of catalytic groups in each puddle, or they may have been relatively
rare. It will take some actual simulations, or extremely good computer
models, to arrive at a better answer to this question.
Supercatalysts
By sheer chance, an occasional puddle would
have contained a combination of several organic enzymes or mineral
catalysts lined up into a ‘pipeline’ formation. Under
the right conditions, it could have taken common raw materials at
one end and spit out a finished organic molecule at the other end.
They probably would have worked similarly to modern enzyme systems,
only less efficiently. It seems possible that a good cluster of catalysts
could have produced hundreds or thousands of reactions per second.
Because of their high level of efficiency,
we’ll call such a combination of several catalysts a ‘supercatalyst’.
The relatively rare supercatalysts would
have had an important impact on the composition of the local soup,
simply because they would synthesize thousands of times more product
than the simpler, less efficient random enzymes.
In the neighborhood of a supercatalyst, there
would be a very high concentration of the output molecules, resulting
in a puddle that was much less random than the surrounding ocean.
If a supercatalyst was anchored well and
continued to act over a long time period, the compounds it produced
would have diffused or splashed to neighboring pools and puddles,
forming a concentration gradient of that chemical. The continuum
from high density to lower density may have extended for a relatively
long distance from the original source (perhaps several meters).
Energy Sources
Of course in the early soup there would not
have been any biological sources of energy to drive chemical reactions.
It takes a very sophisticated series of reactions to harness the
power from any type of chemical or electromagnetic energy, and it’s
extremely unlikely that our random catalytic blobs would have been
that clever.
However the early catalysts and supercatalysts
could still have done a good job on exothermic reactions (which release
energy rather than consuming it) or on reactions with a neutral energy
budget.
The supercatalysts may also have taken advantage
of natural energy inputs such as UV, thermal hot spots or radioactive
decay to catalyze endothermic reactions (which consume energy). In
that case, catalysts generally work in the wrong direction and catalyze
the breakdown instead of the synthesis. However, a good supercatalyst
might be able to work against the ‘energy gradient’ if
it was able to bring in the starting ingredients and then quickly
remove the end product before it had the chance to decompose. For
example, they could have done that by burying a new hydrophobic compound
in a mass of other hydrophobic materials.
How many Supercatalysts were there?
It is very difficult to guess how many supercatalysts
may have formed in the pools and puddles of the prebiotic shorelines.
There was probably a huge amount of surface
area on which they may have lodged, but there is no good way to guess
how often the right combinations of catalysts would have occurred,
and how long they would have survived in the proper positions.
In the chemical “story” that follows, we will guess that
most catalytic activity took place with the help of the relatively
rare supercatalysts, generally outstripping the activity of the regular,
less efficient catalysts, even though they were present in larger
numbers.
We’ll assume the presence of perhaps one or two supercatalysts
per square meter of shoreline, with a random distribution that would
occasionally put several of them into a single pool or puddle complex.
The exact density is not critical, and it
could range a couple of orders of magnitude in either direction and
still provide a plausible level of chemical action for the following
chapters.
Self-Replicators
During prebiotic times, a very interesting class of catalysts
may have developed, with the ability
to roduce more of themselves by catalytic
action. For example, a very simple
self-replicator might consist of
a protein built from just one amino
acid, that was capable of synthesizing
that same amino acid from precursors.
A self-replicating molecule or group
of molecules would have the potential
for positive feedback, creating
large numbers of similar molecules
(if conditions were favorable).
Scientists
have developed a good number of self-replicating
molecules and molecular systems ,
but it has been difficult to develop an effective
transition from these simple
chemical
systems to more life-like processes.
In this book, we will examine a more
specific chemical pathway that bridges
the gap between ‘primordial
soup’ and life. However self-replicating systems may have
provided some areas with an abundant supply of some types of raw
materials, similar to the action of supercatalysts. In that sense,
they may have aided the development of life, even if they didn’t
participate directly in that development.
Catalytic Chemistry
Before we move on to biogenesis, it will
be useful to look more closely at some basic aspects of proteinoid
catalysis, since it has a bearing on the biochemistry that we’ll
discuss in the later chapters of this book.
Protein Folding
Amino acid polymers form a long linear chain
of linked amino acids. However the chains are very flexible— that
is because each bond between atoms in the chain make a very sharp
bend (109°), and most of the bonds are able to rotate freely.
The result is a molecular chain that acts much like a string of beads— capable
of stretching out into a long chain, or clumping up into a compact
blob.
As a polypeptide chain increases in length,
the newly created part of the chain responds to attractions and repulsions
from the remainder of the chain, and moves into a position that depends
on the specific sequence of amino acids. Positively charged molecules
attract to negatively charged ones, and hydrophobic molecules are
attracted to hydrophobic portions of the chain.
The chain also develops secondary folding
such as an ‘alpha helix’ (like a corkscrew) or a flat ‘beta
sheet’. Those large folded structures can then interact and
bond into larger tertiary structures.
Active Groups
Many of the amino acids include side chains
which can assist in a chemical reaction. For example, they might
have a positive or negative charge, or they may be able to accept
or donate an electron or proton.
When secondary and tertiary folding of a
polypeptide causes the active portions of several amino acids to
fit close together, the result is an ‘active group’ or ‘active
site’. The different amino acids each contribute their part
to the overall catalytic effect.
For example many modern enzymes have a serine,
histidine and aspartate in close proximity.
The three molecules work together to donate
an electron temporarily, which helps the
enzyme to hydrolyze other molecules (e.g.
when cutting amino acids free from a protein
chain).
Besides the amino acids, many other organic
molecules can also form active groups which
are useful in enzyme systems. For example,
the purines and pyrimidines that are components
of RNA and DNA have catalytic properties
that are similar to the amino acids. The
biggest difference is that their chains are
much less ‘bendy’, so it’s
not quite so easy to position them close
together.
Positioning
For the active groups in an enzyme to work
properly, they need to be positioned in the
right places so they can interact chemically
with the incoming raw materials.
In polypeptides, that happens when the amino
acid chain loops around in 3-D space, with
some parts of the chain linked to each other
rigidly via sulfur bridges, hydrogen bonding
or hydrophobic attraction. Those rigid portions
hold the active groups into the proper places
for catalysis.
Frequently other molecules in an enzyme will
guide and position the raw materials into
the right location for a reaction, and/or
guide reaction products away from the enzyme.
On a larger scale, many enzymes also contain
a hole, slot or groove that helps control
the diffusion and flow of reaction ingredients
and products.
Coenzymes and Ions
Some organic compounds are extremely active
chemically. They frequently act as a ‘coenzyme’ that
works along with a regular enzyme. Some modern
coenzymes are ATP (which stores energy),
nicotinamide, or NAD (electron carrier),
riboflavin, or FAD (for oxidation and reduction
reactions) and Coenzyme A (which provides
and accepts acetyl groups in synthetic reactions).
Many metal ions also assist with enzyme action— including
calcium, magnesium, iron, copper and zinc.
Most of these compounds were probably present
in the prebiotic soup, and would have occasionally
assisted the early enzymes in their action
.
Conformation Changes
Many polypeptides can ‘flip’ into
more than one stable conformation. That usually
happens when there is a particularly flexible
section of the polypeptide chain, along with
secondary or tertiary structures that are
not firmly bound by other parts of the polypeptide.
When there is a conformational change, part
of an amino acid change will ‘pop’ from
one position to another (as in the shaded
portion below).
Having different conformational states might
act as an ‘on-off’ switch to
control the action of the enzyme— for
example, by shifting part of the active group
away from its neighbors to stop it action.
A conformational change might also help a
chemical reaction to proceed— for example,
by nudging a molecule into place, or by ejecting
the finished product so new raw materials
can attach to the active groups.
We’ll talk later about the role played
by conformational changes in our first self-replicating
molecules. They will also be important in
many of the subsequent reactions.
Enzymes and Substrates
The best enzymes in the prebiotic puddles
were probably attached in one place so they
didn’t move too much— either
by bonding to a mineral substrate, or by
attaching covalently to a fairly rigid blob
of organic material.
That kind of fixed location would be particularly
vital for a successful supercatalyst, which
would need several proteins or coenzymes
to be located close to each other, in order
to have efficient catalytic action.
If there were hydrocarbons in the early soup,
the oil-water junction of tar balls or simple
membranes would also have provided a place
to anchor polypeptides that contained sequences
of hydrophobic amino acids which would have
sunk into the hydrocarbons. Living organisms
frequently will ‘anchor’ enzymes
in the oil/water junction of a membrane,
to help hold them in a specific position.
However, the same thing could have happened
even before there was life, as long as there
were globs of oil or tar to which the catalysts
could attach.
Chirality
Organic catalysts do something very interesting
to their chemical products— they produce
molecules with just one type of spatial orientation,
or chirality. That is very different from
more general organic reactions, which produce
a racemic mix of all possible chiral forms.
That change happens because the polypeptide
catalysts ‘hold’ the reacting
molecules in a specific orientation.
Of course in the long run, all possible enantiomers
would still have been be produced in the
soup, since there would have been just as
many catalysts producing levo-rotary amino
acids as dextro-rotary ones.
But in the neighborhood of a supercatalyst,
we can expect that there would have been
a higher local concentration of levo-rotary
or dextro-rotary molecules— depending
on the chiral form that happened to be produced
by the local catalysts.
Backbone Chains
So far we have talked mostly about catalysts
made from amino acid chains, but there is
a second class of molecular chains that can
also act catalytically. We’ll call
them backbone chains, since they are built
from organic compounds that bind to each
other more rigidly than amino acids, resulting
in polymers that are much less ‘bendy’.
The backbone chains usually form a straight
and rigid molecule or a helix, rather than
a blob as amino acids do.
Organic molecules that contain both aromatic
rings and polar groups are one type of backbone
molecule. In a water solution they tend to ‘stack’ with
the aromatic rings in parallel plates that
are hydrophobically bonded. It’s similar
to a stack of plates in a cabinet, and very
similar to graphite’s chemical structure.
Purines and pyrimidines in particular have
a ring structure that is very eager to bind
into helical chains.
Sugars such as glucose and ribose also can
bond covalently and form long, fairly linear
polymers (an extreme example is cellulose,
the most common structural chemical found
on earth today). Their rigidity comes from
their ring structure and high degree of polarity,
which tends to prevent much rotation at each
bond. However sugars are usually not very
catalytic on their own, since they don’t
have as much variety in their side chains,
as is found in the amino acids, purines and
pyrimidines.
Backbones and Catalysts
Could backbone chain molecules have acted
as catalysts in the early prebiotic world?
Sure. Most of the purines, pyrimidines and
other aromatic molecules contain chemically
active parts on their molecules, similar
to those in the amino acids. The aromatic
rings themselves are often good at accepting
and donating electrons. So as long as the
chain molecules were held in the right positions,
they could have contributed to enzyme activity
just as easily as amino acids.
The backbone chains would not have been so
effective when it came positioning several
active molecules close together— the
chains are rigid enough that it wouldn’t
have been easy for them to loop back around
to the same place as where they started.
But short lengths of backbone chain could
have attached to a proteinoid blob and assisted
in catalysis just as well as any amino acid.
Backbones as Structures
Backbone chains might have also served a
structural role in supercatalysts. If a short
chain happened to become imbedded in with
groups of polypeptides or other compounds,
it might have occasionally created a stable
supercatalyst by positioning smaller enzymes
into a fixed position. That’s where
the ‘backbone’ part comes in.
Shoreline pools that included a catalyst
which created rigid chain-forming molecules
such as purines or pyrimidines, may have
seen a slightly higher frequency of catalysis
in general, if the chains helped to hold
together random groups of polypeptides and
other compounds that might have enzymatic
action. But there was nothing remotely like
positive feedback yet.
Note that these early chains would not have
had any genetic role— they would simply
have been ‘interesting’ compounds
that might occasionally act a structure or
catalyst in the random blobs of the time.
Later on, we’ll see that the backbone
chains probably played increasingly important
roles in prebiotic chemistry, eventually
culminating in the elegant double helix structure
that is our primary subject. But it will
take quite a while until we get there.
Templates
So far we have talked about ‘traditional’ catalysts,
which could have aided in dehydrogenation
reactions and synthesis in the early soup.
But there is another way that larger compounds
may have formed in the prebiotic world— by
way of ‘templates’.
A template is a mineral or organic surface
which encourages the formation of long-chain
molecules by positioning individual molecules
so it is easier for them to bond together.
If specific binding areas within the template
had an affinity for specific compounds, the
polymer might end up with a similar sequence,
each time a new set of components bound to
the template and a polymer emerged.
Mineral Templates
One of the most common of the potential templates
is clay— a decomposition product of
micas and feldspars. Structurally, it is
generally in the form of flat plates of silica
interspersed with calcium, aluminum and magnesium
ions and water molecules.
In experiments under simulated prebiotic
conditions, montmorillonite clay was shown
to act as a template that produced relatively
longer chains of RNA from single nucleotides.
Although the RNA chains were not always linked
by the standard 3’,5’ bonds,
they still could have acted as an early form
of genetic chain.
Many clays and minerals also have catalytic
activity, and their structure may have acted
as a template for other polymerizations as
well.
Polypeptide Templates
One possible source of templating in prebiotic
puddles would be crystals of very short chain
amino acid sequences—frequently dimers
or trimers such as phenylalanine-phenylalanine
or cysteine-phenylalanine-phenylalanine.
They may have formed during the repeated
wetting and drying cycles in the condensing
pools.
Some of these polymers may have formed into
fibers or tubes that could have served as
an environment where RNA strands could have
bonded, and developed in a relatively protected
environment.
Template Results
What kinds of larger compounds would have
been created by a template? Well, it depends
entirely on the compounds that were in highest
concentration in the soup near the template.
If there was a preponderance of amino acids,
the template might produce polypeptides or
small proteins. If there were many nucleic
acids with sufficient ribose sugars and phosphate,
it might produce RNA or DNA sequences.
Templates would be more efficient if they
were in an area where a small number of supercatalysts
had already created a local concentration
of just a few raw materials. In that case
the ‘slots’ in the template would
frequently be filled with the same molecules,
and a more consistent end product would result.
There would not be any selective advantage
for larger compounds created from a template— but
the presence of multiple copies of the same
compounds does make prebiotic evolution more ‘interesting’.
As we’ll see later, it may have played
a role in the next steps in chemical evolution.
Chemical Selection and Evolution
Any catalysts that formed in the early soup
had no way of reproducing or passing their
structure along to grandchildren. That means
that Darwinian natural selection and evolution
would not have taken place.
Nevertheless, we can expect that some limited
selective forces would start to come into
play even in this early and extremely random
organic world. We’ll call it ‘chemical
evolution’, since it may have helped
provide higher concentrations of chemicals
used in later pre-biotic reactions, even
when there was no true evolution going on.
These selective forces would work best in
the limited environs of just a few puddles
or pools.
Survival of the Survivors
The simplest selective force in the soup
would be simple chemical survival of compounds.
A compound that was quickly broken down by
UV, water, heat or other environmental conditions
would simply not remain present in very large
quantities. More stable compounds would stick
around longer, and gradually increase in
concentration.
Likewise, compounds that were easily formed
from other compounds that were already in
abundant supply would have become more common.
That synthesis might happen from a simple
inorganic reaction a la the Miller-Urey experiment,
or it might be accelerated by whatever organic
or inorganic catalysts were present.
If there was some particular catalyst that
was easy to form, then it probably appeared
more often in the ocean and the puddles,
and any of its reaction products would also
have become more common.
Survival of the Cell Makers
Any random clusters with enzyme activity
in the pre-biotic world would have always
been in danger of decomposition. They might
be zapped with radiation, digested by a proteolytic
enzyme, baked into oblivion in a thermal
vent or hot spring, or dehydrated by the
sun and then blown by the wind onto dry land.
Enzymes that produced some kind of protective
shell material would have enjoyed increased
longevity, simply because they’d be
surrounded by sacrificial material.
New enzymes would have been created randomly,
and since any mucus or membrane producers
would stick around for longer, over time
there would be a gradual increase in the
number of enzymes producing protective materials
(and also an increase in protective compounds
in the soup itself).
It’s possible that a poly-phospho-ribose
gel may have been formed by the occasional
random enzyme, providing a convenient source
of raw material for later RNA or DNA synthesis.
Proteins Catalyzing Amino Acids
A more significant form of chemical evolution
would result if a catalyst produced compounds
that were a part of its own makeup. It’s
a situation that has much potential for positive
feedback loops.
The extreme example would be a polymer of
just one amino acid that happened to be a
catalyst that could synthesize its own amino
acid. It would create a local concentration
of its own raw materials, which would occasionally
by sheer random chance produce another copy
of itself (assuming there were concentration
and dehydration reactions going on).
Of course, most protein enzymes require the
presence of several amino acids, and it’s
unlikely that effective enzymes could be
created from pure polymers of a single amino
acid .
However the same selective force also applies
to slightly more complex polypeptide enzymes
composed of a small number of amino acids.
For example, imagine a shoreline puddle that
included a few supercatalysts that transformed
precursors into two or three of the amino
acids that built the catalysts. The result
would have been high concentrations of those
components, which probably would have splashed
and spilled into neighboring pools and created
local concentrations in them as well.
Then imagine a short polypeptide condensing
from those two or three ingredients that
happened to be a catalyst that helped condense
amino acids into polypeptides.
With no direction, many of those polypeptides
would be non-functional, but a very small
percentage of them would have the exact same
sequence as the first condensing polypeptide.
For example, if it was built from two amino
acids and was 20 amino acids in length, then
one out of 220 of its products (about one
in a million) would have an identical sequence.
That means that there would have been a low-efficiency
replication of that protein. Even more interesting,
there would be a neighborhood with a huge
number of other short polypeptide chains
composed of the same components— some
of which might have other interesting properties.
Given the billions of possible pools this
is not a completely implausible event. If
the catalysts were firmly attached in the
pools, they might have proceeded to create
a reasonably large number of enzyme progeny
over the course of their lifetime.
Of course such simple self-replication is
not life— it has no genetic material
to respond to selective forces, so it has
no way to pass any beneficial properties
along to the next generation. It’s
not even anything that leads directly to
life forms in any meaningful way. But it
would have created local concentrations of
an amino acid and an enzyme that might be
used in actual pre-life forms later on .
Where is the RNA?
Because RNA is capable of catalytic activity
, many exobiologists now support the ‘RNA
world’ theory— which assumes
that RNA served two different roles in prebiotic
chemistry, as catalyst and as information
storage.
The RNA world would have started with the
gradual formation of RNA chains that were
able to catalyze the formation of their own
raw materials and assembly into longer chains.
Eventually, DNA and proteins would then gradually
taken over and supplanted the RNA-based life
because of their greater efficiency.
An RNA world may certainly have been possible,
and it does elegantly solve the ‘chicken
and egg’ problem for DNA and proteins
(more or less by answering that the first
thing was ‘salamanders’).
However the RNA world theory also has some
serious weaknesses— perhaps the most
serious is that RNA forms a rather rigid
chain that is not that great at catalysis.
RNA enzymes also require the use of complementary
pairing to hold the active groups in position,
and in a world of random purines and pyrimidines,
it seems unlikely that would happen very
often.
What we will focus on instead is a different
path that has the advantage of evolving in
smaller, less improbable steps from simpler
compounds. It’s more of a coevolution
of proteins and backbone chains, which may
or may not have been RNA at the start.
As we’ll see later, there are some
intriguing clues in modern biochemistry that
the RNA world may actually have occurred
one or more times in the early Earth, but
we’ll fit it into a larger picture
of biochemical evolution, instead of making
it the primary vehicle for early evolution.
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