H00102--00A, Front mat Genesis

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by Charles Baum


  playing a key role in the integrated network.

  Kauffman sees an important payoff in the behavior of such elabo-

  rate catalytic networks. Unlike a single self-replicating molecule, such

  vast networks of reactive molecules have the potential to increase in

  complexity and efficiency through numerous different interactions

  among molecules. The large number and variety of molecular interac-

  tions foster the emergence of new metabolic pathways and nested cycles

  of synthesis. Like a living metabolic cycle, Kauffman’s networks incor-

  porate a certain degree of sloppiness. Through such variations, the sys-

  tem can change by shifting to new, more efficient reaction pathways

  and in the process display a defining trait of life—the ability to evolve.

  THE GAME OF METABOLISM

  Kauffman’s theory provides an intuitively appealing model for the

  emergence of primordial metabolic life. For one thing, if molecules in

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  GENESIS

  a complex autocatalytic system efficiently catalyze each other, then

  there’s no need, at least at first, for a genetic mechanism. Accurate rep-

  lication of the entire system is, in effect, intrinsic to the network. At the

  same time, the system has the potential to vary and gradually evolve.

  Growth, reproduction, evolution—the autocatalytic network would

  appear to meet the minimum criteria for life.

  Kauffman’s model sounds good on paper, but there’s a dramatic

  gap between plausible theory and actual experiment. For example,

  what exactly is the chemical “A”? What is “B”? When asked, Kauffman

  shrugs and says, “That’s for the chemists to figure out.” And that’s what

  chemists have done.

  If you want to make protolife in the lab, it’s best to start by design-

  ing a simple metabolic cycle. Metabolism is a special kind of cyclical

  chemical process with two essential inputs. First you need a source of

  energy—preferably chemical energy, since that’s what all known simple

  living cells use. (Photosynthetic cells use sunlight, to be sure, but these

  advanced organisms possess layers of chemical complexity far beyond

  those of more ancient, simple cells.) Second, you need reliable supplies

  of simple molecules, such as carbon dioxide and water, to provide the

  raw materials.

  Living cells undergo chemical reactions not unlike burning, in

  which two chemicals (oxygen and some carbon-rich fuel) react and

  release energy. However, the objective in metabolism, unlike in an open

  fire, is to capture part of that released energy to make new useful mol-

  ecules that reinforce the cycle. So metabolism requires a sequence of

  chemical reactions that work in concert.

  Three basic rules govern this game of metabolism:

  Rule 1—The Cycle: Describe a cycle consisting of a sequence of

  progressively larger molecules. The largest of these molecules should

  then be able to split into two smaller molecules, both of which are also

  in the cycle. In this way you end up with two sets of molecules, where

  before there was only one set and the cycle keeps on reproducing itself.

  Rule 2—The Environment: Identify a plausible prebiotic environ-

  ment that provides a reliable supply of raw materials (i.e., small mol-

  ecules made up of carbon, nitrogen, sulfur, and other essential

  elements) and energy (preferably the chemical energy of unstable min-

  erals). Furthermore, all of the different types of molecules in the cycle

  have to be able to survive in that environment long enough to keep the

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  cycle going. Extremes in temperature, pressure, or acidity, for example,

  may stabilize some kinds of molecules, while destroying others.

  Rule 3—Continuity: An unbroken chemical history must link

  Earth’s earliest metabolic cycle with the metabolism of today’s cells.

  Deep within the metabolism of all of us, there are likely to be “fossil”

  biochemical pathways that point to life’s simpler beginnings. So any

  plausible model must conform to this “principle of continuity” and

  use molecules and energy sources that lie close to the basic metabolism

  of modern organisms.

  Experimental evidence provides the ultimate test of any chemical

  theory. Each chemical step in a hypothetical metabolic cycle is a poten-

  tial experiment, so you get bonus points if these crucial experiments

  work.

  Three influential models exemplify the metabolism game at its

  best: the “Protenoid World” of Sidney Fox, the “Thioester World” of

  Christian de Duve, and a group of related hypotheses based on the

  reverse citric acid cycle, including the elaborate “Iron–Sulfur World”

  hypothesis of Günter Wächtershäuser.

  THE PROTENOID WORLD

  The granddaddy of all metabolism-first models emerged as the brain-

  child of protein chemist Sidney Fox, who began thinking about origin-

  of-life chemistry shortly after the publication of Stanley Miller’s 1953

  paper. Fox’s career was strongly influenced by Thomas Hunt Morgan,

  a famed geneticist and a member of Fox’s Caltech thesis committee.

  “Fox,” Morgan would often remark, “all the important problems of life

  are problems of proteins.” Fox took this lesson to heart and began

  studying proteins’ role in life’s origin as a faculty member at Florida

  State University in the mid-1950s.

  He imagined a hot primordial Earth where amino acids from the

  soup dried and baked on cooling volcanic rocks. He mimicked these

  conditions in his lab, drying amino acids on a hot surface at 170°C,

  and found that his chemicals quickly polymerized into a lumpy sub-

  stance he called “protenoid.” This discovery, announced in 1958, would

  shape his checkered three-decade career in origins research.

  Fox’s protenoids displayed fascinating behavior. They acted as cata-

  lysts, though to a rather modest degree compared to the modern pro-

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  GENESIS

  tein catalysts that promote chemical reactions in every cell. When

  placed in hot water, they spontaneously turned into microbe-sized

  spheres, and sometimes these divided. He claimed that these spheres,

  though not as orderly as biological proteins, possessed a nonrandom

  structure with a permeable bilayer membrane. Increasingly, Fox sug-

  gested that the protenoids were “lifelike” and represented the key to

  life’s origins.

  Fox and a small army of students carried out experiments to bol-

  ster his origin model. Solutions of protenoids were heated and cooled

  in a cycle that produced structures he called “microspheres”—cell-like

  entities that could absorb more protenoids, grow, and divide, thus

  forming a second generation of microspheres. These self-replicating

  objects, growing from nutrients in solution and lacking any genetic

  mechanism, formed the basis of a true metabolism-first model.

  At first blush, the Protenoid World might seem to score well in the

  game of metabolism. Rule 1: The cycle is formed from widely available

  amino acids, which readily form protenoids that grow and divide. Rule

 
; 2: The environment, a volcanic setting near a tidal zone, is realistic for

  the early Earth. Rule 3: Protenoids seemed to conform to the principle

  of biological continuity, because closely related proteins are fundamen-

  tal to modern life. What’s more, experiments seemed to support each

  step of the hypothesis.

  For a time, Fox’s career thrived. Starting in 1960, he received gen-

  erous grants from NASA’s Exobiology program, which supported a va-

  riety of research projects on the origin and evolution of life. Fox’s funds

  soon exceeded $1.5 million and allowed him to establish his own Insti-

  tute of Molecular Evolution at the University of Miami in 1964. A

  steady stream of graduate students investigated protenoid properties.

  As Sidney Fox increasingly fell in love with his Protenoid World

  model, his claims became more and more extreme. The origin-of-life

  problem had been solved, he said, and protenoids are “alive in some

  primitive way.” In his 1988 book, The Emergence of Life, he even made

  the bizarre and unsubstantiated claim that his protenoid microspheres

  possessed a kind of “rudimentary consciousness.”

  As early as 1959, the mainstream origin-of-life community, led

  principally by Stanley Miller and Harold Urey, had begun distancing

  themselves from Fox’s claims. They resented what they regarded as the

  sensationalistic use of terms such as “protenoid” and “lifelike.” They

  scoffed at the idea that amino acids might have baked into anything

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  useful on a bed of lava. They questioned whether the protenoid struc-

  tures were truly nonrandom in structure. The purported lifelike be-

  haviors of microspheres were also challenged, especially the idea that

  they “replicated” in the biological sense. Equally strong was their ob-

  jection that the Protenoid World scenario ignored the knotty problem

  of genetics. How would DNA and RNA have arisen in such a world?

  Despite myriad objections to the theory, and the increasing scien-

  tific isolation of Fox, the Protenoid World was influential for at least

  two reasons. Not only did Fox develop the first comprehensive

  metabolism-first model, but he also championed the important philo-

  sophical position that origin processes might be nonrandom and

  deterministic—a view later embraced by numerous other origins

  workers. Nevertheless, by the late 1970s, Sidney Fox’s efforts had been

  marginalized, and they remained the target of jokes and derision until

  his death in 1998.

  THE THIOESTER WORLD

  The Belgian chemist Christian de Duve made his scientific name study-

  ing the structural and functional organization of cells—work that won

  him the Nobel Prize in physiology or medicine in 1974. In an oft-

  repeated pattern, he then turned his attention to the origin of life, tack-

  ling the classic question from his perspective as a cell biologist. Not

  surprisingly, that background influences his origins theory.

  De Duve takes a rather ambiguous stand in the metabolism- ver-

  sus genetics-first controversy. For him, the simplest imaginable living

  thing is a cell-like entity that has a full complement of genetic material

  to control cellular functions. But he also recognizes the futility of jump-

  starting genetics without a well-established, elaborate arsenal of chemi-

  cal reactions—what he calls “protometabolism” (as opposed to the

  more complex metabolism of modern cells). It’s really a question of

  where you place the boundary between nonliving and living systems.

  I’ve argued that the complex sequence of emergent events leading from

  geochemistry to life requires a rich taxonomy of intermediate states.

  De Duve appears to agree: His “Age of Chemistry” (protometabolism)

  precedes the “Age of Information” (genetics), which in turn precedes

  the “Age of the Protocell” (genetics and metabolism combined). Only

  then, with the merger of metabolism and genetics, does modern life

  truly emerge.

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  GENESIS

  Let’s assume, de Duve says, that some early Earth environment

  (rather vaguely specified as a “volcanic setting” in his writings) was

  rich in hydrogen sulfide gas and iron sulfide minerals, along with the

  usual cast of carbon-based molecules. One chemical consequence of

  this sketchy scenario might be the production of sulfur-containing

  molecules called thioesters, which incorporate a strong bond between

  one sulfur atom and one carbon atom—a bond that can release a lot of

  energy if broken. De Duve’s hypothesis rests on the assumption that a

  steady supply of these energy-rich thioester molecules was available on

  the ancient Earth—hence the Thioester World.

  Why focus on thioesters? For one thing, they are essential in the

  metabolism of modern cells. By breaking the strong carbon–sulfur

  bond, they can transfer energy to promote metabolic reactions, thus

  building larger molecules from smaller ones. In the Thioester World, a

  steady supply of thioesters provides the chemical energy required to

  drive protometabolism.

  Of particular import, thioesters have a propensity to bond with

  amino acids, which would have been readily available in the prebiotic

  soup. Remarkably, when placed in solution, these amino acid–thioester

  groups spontaneously assemble into peptidelike chains (de Duve calls

  them “multimers,” because they differ in some chemical details from

  true peptides). At first, the multimers thus formed would have had

  little effect on the chemical mix. But, he speculates, eventually some of

  these big molecules by chance acquired catalytic properties (reminis-

  cent of Fox’s protenoids). Gradually, as the environment became en-

  riched in chemically active multimers, an autocatalytic cycle might

  have emerged, producing, he says, “protoenzymes required for

  protometabolism.”

  The Thioester World hypothesis fits nicely with the primordial-

  soup paradigm favored by Miller and his allies. De Duve’s scenario

  relies on the environment to provide a steady input of various molecu-

  lar building blocks, including amino acids, carbohydrates, and of

  course the essential energy-rich thioesters themselves. Such a model

  metabolism, in which the first cells eat and assemble components from

  their surroundings, is said to be heterotrophic (from the Greek, “other

  nourishment”). Heterotrophs must scavenge their molecules from the

  environment.

  So how does de Duve’s Thioester World score in the game of me-

  tabolism? He certainly gets high marks for identifying a viable prebi-

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  203

  otic environment rich in plausible simple molecules. Using thioesters

  as a reliable, renewable energy source is especially attractive, because it

  echoes the action of thioesters in modern biology. But he never speci-

  fies the molecules that comprise his metabolic cycle; the chemistry is

  vague. For de Duve, protometabolism is an awkward, transient, ill-

  defined phase that is necessary to set the stage for genetics. Thioesters

>   promote the synthesis of catalytic multimers, which in turn promote

  the manufacture of a genetic molecule such as RNA. Only then does a

  well-defined biochemistry take root.

  The bottom line: de Duve’s scenario is appealing in its broad out-

  lines, but lacking in specific chemical details. And so, if you like details,

  there’s no better place to turn than Günter Wächtershäuser’s Iron–

  Sulfur World.

  15

  The Iron–Sulfur World

  You don’t mind if I brag a little, but something like this has

  never been done in the entire field.

  Günter Wächtershäuser, 1998

  In bold concept, epic sweep, and sheer mass of detailed predictions,

  Günter Wächtershäuser’s Iron–Sulfur World hypothesis for the ori-

  gin of life stands alone. Since its first presentation in 1988, this theory

  has changed the landscape of origins research by calling into question

  many of the most deeply rooted assumptions about life’s beginnings.

  Wächtershäuser (whom we first met in Chapter 8 because of his

  pleasing reliance on minerals) argues for a strikingly original metabo-

  lism-first model, based on an autotrophic (self-nourishment) model.

  Autotrophic metabolism begins with chemical simplicity. All of life’s

  essential biomolecules are manufactured in place, as needed, from the

  smallest of building blocks: carbon dioxide (CO ), water (H O), am-

  2

  2

  monia (NH ), hydrogen sulfide (H S), and so forth. All chemical syn-

  3

  2

  thesis is accomplished stepwise, just a few atoms at a time. [Plate 8]

  The contrast between heterotrophic and autotrophic existence is

  profound and represents a fundamental point of disagreement among

  origin-of-life researchers. Supporters of a heterotrophic origin argue

  that it’s much easier for a primitive cell to use the diverse molecular

  products available in the prebiotic soup rather than to make them from

  scratch. Why go to the trouble of synthesizing lots of amino acids if

  they’re already available in the environment? Modern heterotrophic

  cells are much simpler than autotrophic cells, because they don’t need

  all the complex chemical machinery to manufacture amino acids, car-

  bohydrates, lipids, and so forth. It makes sense to assume that the sim-

  pler mechanism—heterotrophy—came first.

 

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