Misplaced Pages

Revision as of 23:37, 11 February 2008

In the natural sciences, abiogenesis, the question of the origin of life, is the study of how life on Earth might have emerged from non-life. Scientific consensus is that abiogenesis occurred sometime between 4.4 billion years ago, when water vapor first liquefied, and 2.7 billion years ago, when the ratio of stable isotopes of carbon (C and C ), iron and sulfur points to a biogenic origin of minerals and sediments and molecular biomarkers indicate photosynthesis. This topic also includes panspermia and other exogenic theories regarding possible extra-planetary or extraterrestrial origins of life, thought to have possibly occurred sometime over the last 13.7 billion years in the evolution of the Universe since the Big Bang.

Origin of life studies is a limited field of research despite its profound impact on biology and human understanding of the natural world. Progress in this field is generally slow and sporadic, though it still draws the attention of many due to the eminence of the question being investigated. Several theories have been proposed, most notably the iron-sulfur world theory (metabolism first) and the RNA world hypothesis (genetics first).

History of the concept in science

Until the early Nineteenth Century people frequently believed in spontaneous generation of life from non-living matter.

Spontaneous generation

This section does not cite any sources. Please help improve this section by adding citations to reliable sources. Unsourced material may be challenged and removed. (January 2008) (Learn how and when to remove this message)

Classical notions of abiogenesis, now more precisely known as spontaneous generation, held that complex, living organisms are generated by decaying organic substances, e.g. that mice spontaneously appear in stored grain or maggots spontaneously appear in meat.

According to Aristotle it was a readily observable truth that aphids arise from the dew which falls on plants, fleas from putrid matter, mice from dirty hay, alligators and crocodiles from rotting logs at the bottom of bodies of water, and so forth. In the 17th century such assumptions started to be questioned; such as that by Sir Thomas Browne in his Pseudodoxia Epidemica, subtitled Enquiries into Very many Received Tenets, and Commonly Presumed Truths, of 1646, an attack on false beliefs and "vulgar errors." His conclusions were not widely accepted, e.g. his contemporary, Alexander Ross wrote: "To question this (i.e., spontaneous generation) is to question reason, sense and experience. If he doubts of this let him go to Egypt, and there he will find the fields swarming with mice, begot of the mud of Nylus, to the great calamity of the inhabitants."

In 1546 the physician Girolamo Fracastoro theorized that epidemic diseases were caused by tiny, invisible particles or "spores", which might not be living creatures, but this was not widely accepted. Next, Robert Hooke published the first drawings of a microorganism in 1665. He is also credited for naming the cell which he discovered while observing cork samples.

Then in 1676 Anthony van Leeuwenhoek discovered microorganisms that, based on his drawings and descriptions are thought to have been protozoa and bacteria. This sparked a renewal in interest in the microscopic world.

The first step was taken by the Italian Francesco Redi, who, in 1688, proved that no maggots appeared in meat when flies were prevented from laying eggs. From the seventeenth century onwards it was gradually shown that, at least in the case of all the higher and readily visible organisms, the previous sentiment regarding spontaneous generation was false. The alternative seemed to be omne vivum ex ovo: that every living thing came from a pre-existing living thing (literally, from an egg).

In 1768 Lazzaro Spallanzani proved that microbes came from the air, and could be killed by boiling. Yet it was not until 1861 that Louis Pasteur performed a series of careful experiments which proved that organisms such as bacteria and fungi do not appear in nutrient rich media of their own accord in non-living material, and which supported cell theory.

Darwin and Pasteur

By the middle of the 19th century Pasteur and others had demonstrated that living organisms did not arise spontaneously from non-living matter; the question therefore arose of how life might have come about within a naturalistic framework. In a letter to Joseph Dalton Hooker on February 1, 1871, Charles Darwin made the suggestion that the original spark of life may have begun in a "warm little pond, with all sorts of ammonia and phosphoric salts, lights, heat, electricity, etc. present, so that a protein compound was chemically formed ready to undergo still more complex changes". He went on to explain that "at the present day such matter would be instantly devoured or absorbed, which would not have been the case before living creatures were formed." In other words, the presence of life itself makes the search for the origin of life dependent on the sterile conditions of the laboratory.

Haldane and Oparin

No real progress was made until 1924 when Aleksandr Ivanovich Oparin experimentally showed that atmospheric oxygen prevented the synthesis of the organic molecules that are the necessary building blocks for the evolution of life. In his The Origin of Life on Earth, Oparin argued that a "primeval soup" of organic molecules could be created in an oxygen-less atmosphere through the action of sunlight. These would combine in ever-more complex fashions until they dissolved into a coacervate droplet. These droplets would "grow" by fusion with other droplets, and "reproduce" through fission into daughter droplets, and so have a primitive metabolism in which those factors which promote "cell integrity" survive, those that do not become extinct. Many modern theories of the origin of life still take Oparin's ideas as a starting point. Around the same time J. B. S. Haldane also suggested that the earth's pre-biotic oceans - very different from their modern counterparts - would have formed a "hot dilute soup" in which organic compounds, the building blocks of life, could have formed. This idea was called biopoiesis or biopoesis, the process of living matter evolving from self-replicating but nonliving molecules.

Early conditions

Morse and MacKenzie have suggested that oceans may have appeared first in the Hadean era, as soon as 200 million years after the Earth was formed, in a hot (100 °C) reducing environment, and that the pH of about 5.8 rose rapidly towards neutral. This has been supported by Wilde who has pushed the date of the zircon crystals found in the metamorphosed quartzite of Mount Narryer in Western Australia, previously thought to be 4.1-4.2 billion years old, to 4.404 billion years. This means that oceans and continental crust existed within 150 million years of Earth's formation. Despite this, the Hadean environment was one highly hazardous to life. Frequent collisions with large objects, up to 500 kilometres in diameter, would have been sufficient to vaporise the ocean within a few months of impact, with hot steam mixed with rock vapour leading to high altitude clouds completely covering the planet. After a few months the height of these clouds begins to decrease but the cloud base would still be elevated probably for the next thousand years after which at low altitude it starts to rain. For another two thousand years rains slowly draw down the height of the clouds, returning the oceans to their original depth only 3,000 years after the impact event. The possible Late Heavy Bombardment possibly caused by the movements in position of the Gaseous Giant planets, that pockmarked the moon, and other inner planets (Mercury, Mars, and presumably Earth and Venus), between 3.8 and 4.1 billion years would likely have sterilised the planet if life had already evolved by that time.

Examining the time interval that could have existed between devastating environmental insults by impact exceeded the timescale for establishing self-replicating protoorganisms, the interval in time when life might first have bootstrapped itself into existence can be found for different early environment. The study by Maher and Stephenson shows that if the deep marine hydrothermal setting provides a suitable site for the origin of life, abiogenesis could have happened as early as 4000 to 4200 Myr ago, whereas if it occurred at the surface of the earth abiogenesis could only have occurred between 3700 and 4000 Myr.

Other research suggests a colder start to life. Research by Stanley Miller showed the ingredients adenine and guanine require freezing conditions to synthesize, but cytosine and uracil require boiling temperatures. Based on his research he suggested a beginning of life involving freezing condition and exploding meteorites. A new article in Discover Magazine points to research by Stanley Miller indicating the formation of seven different amino acids and 11 types of nucleobases in ice when ammonia and cyanide were left in the Antarctic ice from 1972 -1997, and research by Hauke Trinks showing the formation of RNA molecules 400 bases long under freezing conditions using an RNA template, a single-strand chain of RNA that guides the formation of a new strand of RNA. As that new RNA strand grows, it adheres to the template. The explanation given for the unusual speed of these reactions at such a low tempurature is eutectic freezing. As an ice crystal forms, it stays pure: Only molecules of water join the growing crystal, while impurities like salt or cyanide are excluded. These impurities become crowded in microscopic pockets of liquid within the ice, and this crowding causes the molecules to collide more often.

Evidence of the early appearance of life comes from the Isua supercrustal belt in Western Greenland and from similar formations in nearby the Akilia Islands. Carbon entering into rock formations has a concentration of elemental δC of about -5.5, where because of a preferential biotic uptake of C, biomass has a δC of between -20 and -30. These isotopic fingerprints are preserved in the sediments, and Mojzis has used this technique to suggest that life existed on the planet already by 3.85 billion years ago. Lazcano and Miller (1994) suggest that the rapidity of the evolution of life is dictated by the rate of recirculating water through mid ocean submarine vents. Complete recirculation takes 10 million years, thus any organic compounds produced by then would be altered or destroyed by temperatures exceeding 300 °C. They estimate that the development of a 100 kilobase genome of a DNA/protein primitive heterotroph into a 7000 gene filamentous cyanobacterium would have required only 7 million years.

Current models

There is no truly "standard model" of the origin of life. But most currently accepted models build in one way or another upon a number of discoveries about the origin of molecular and cellular components for life, which are listed in a rough order of postulated emergence:

1. Plausible pre-biotic conditions result in the creation of certain basic small molecules (monomers) of life, such as amino acids. This was demonstrated in the Miller-Urey experiment by Stanley L. Miller and Harold C. Urey in 1953.
2. Phospholipids (of an appropriate length) can spontaneously form lipid bilayers, a basic component of the cell membrane.
3. The polymerization of nucleotides into random RNA molecules might have resulted in self-replicating ribozymes (RNA world hypothesis).
4. Selection pressures for catalytic efficiency and diversity result in ribozymes which catalyse peptidyl transfer (hence formation of small proteins), since oligopeptides complex with RNA to form better catalysts. Thus the first ribosome is born, and protein synthesis becomes more prevalent.
5. Proteins outcompete ribozymes in catalytic ability, and therefore become the dominant biopolymer. Nucleic acids are restricted to predominantly genomic use.

The origin of the basic biomolecules, while not settled, is less controversial than the significance and order of steps 2 and 3. The basic chemicals from which life was thought to have formed are:

1. Methane (CH₄),
2. Ammonia (NH₃),
3. Water (H₂O),
4. Hydrogen sulfide (H₂S),
5. Carbon dioxide (CO₂) or carbon monoxide (CO), and
6. Phosphate (PO₄).

Molecular oxygen (O₂) and ozone (O₃) were either rare or absent.

As of 2008, no one has yet synthesized a "protocell" using basic components which would have the necessary properties of life (the so-called "bottom-up-approach"). Without such a proof-of-principle, explanations have tended to be short on specifics. However, some researchers are working in this field, notably Steen Rasmussen at Los Alamos National Laboratory and Jack Szostak at Harvard University. Others have argued that a "top-down approach" is more feasible. One such approach, attempted by Craig Venter and others at The Institute for Genomic Research, involves engineering existing prokaryotic cells with progressively fewer genes, attempting to discern at which point the most minimal requirements for life were reached. The biologist John Desmond Bernal, coined the term Biopoesis for this process, and suggested that there were a number of clearly defined "stages" that could be recognised in explaining the origin of life.

• Stage 1: The origin of biological monomers
• Stage 2: The origin of biological polymers
• Stage 3: The evolution from molecules to cell

Bernal suggested that Darwinian evolution may have commenced early, some time between Stage 1 and 2.

Origin of organic molecules

There are three sources of organic molecules on the early Earth:

1. organic synthesis by other energy sources (such as ultraviolet light or electrical discharges) (eg.Miller's Experiments).
2. delivery by extraterrestrial objects (eg Carbonaceous chondrites);
3. organic synthesis driven by impact shocks.

Recently estimates of these sources suggest that the heavy bombardment before 3.5 Gyr ago within the early atmosphere made available quantities of organics comparable to those produced by other energy sources.

Miller's experiments

In 1953 a graduate student, Stanley Miller, and his professor, Harold Urey, performed an experiment that proved organic molecules could have spontaneously formed on Early Earth from inorganic precursors. The now-famous “Miller-Urey experiment” used a highly reduced mixture of gases - methane, ammonia and hydrogen – to form basic organic monomers, such as amino acids. Whether the mixture of gases used in the Miller-Urey experiment truly reflects the atmospheric content of Early Earth is a controversial topic. Other less reducing gases produce a lower yield and variety. It was once thought that appreciable amounts of molecular oxygen were present in the prebiotic atmosphere, which would have essentially prevented the formation of organic molecules; however, the current scientific consensus is that such was not the case. See Oxygen Catastrophe.

Simple organic molecules are, of course, a long way from a fully functional self-replicating life form. But in an environment with no pre-existing life these molecules may have accumulated and provided a rich environment for chemical evolution ("soup theory"). On the other hand, the spontaneous formation of complex polymers from abiotically generated monomers under these conditions is not at all a straightforward process. Besides the necessary basic organic monomers, compounds that would have prohibited the formation of polymers were formed in high concentration during the experiments.

It can be argued that the most crucial challenge unanswered by this theory is how the relatively simple organic building blocks polymerise and form more complex structures, interacting in consistent ways to form a protocell. For example, in an aqueous environment hydrolysis of oligomers/polymers into their constituent monomers would be favored over the condensation of individual monomers into polymers. Also, the Miller experiment produces many substances that would undergo cross-reactions with the amino acids or terminate the peptide chain.

Fox's experiments

In the 1950s and 1960s Sidney W. Fox, studied the spontaneous formation of peptide structures under conditions that might plausibly have existed early in Earth's history. He demonstrated that amino acids could spontaneously form small peptides. These amino acids and small peptides could be encouraged to form closed spherical membranes, called microspheres.

Eigen's hypothesis

In the early 1970s the problem of the origin of life was approached by Manfred Eigen and Peter Schuster of the Max Planck Institute for Biophysical Chemistry. They examined the transient stages between the molecular chaos and a self replicating hypercycle in a prebiotic soup.

In a hypercycle, the information storing system (possibly RNA) produces an enzyme, which catalyzes the formation of another information system, in sequence until the product of the last aids in the formation of the first information system. Mathematically treated, hypercycles could create quasispecies, which through natural selection entered into a form of Darwinian evolution. A boost to hypercycle theory was the discovery that RNA, in certain circumstances forms itself into ribozymes, capable of catalyzing their own chemical reactions. However, these reactions are limited to self-excisions (in which a longer RNA molecule becomes shorter), and much rarer small additions that are incapable of coding for any useful protein. The hypercycle theory is further degraded since the hypothetical RNA would require the existence of complex biochemicals such as nucleotides which are not formed under the conditions proposed by the Miller-Urey experiment.

Wächtershäuser's hypothesis

Another possible answer to this polymerization conundrum was provided in 1980s by Günter Wächtershäuser, in his iron-sulfur world theory. In this theory, he postulated the evolution of (bio)chemical pathways as fundamentals of the evolution of life. Moreover, he presented a consistent system of tracing today's biochemistry back to ancestral reactions that provide alternative pathways to the synthesis of organic building blocks from simple gaseous compounds.

In contrast to the classical Miller experiments, which depend on external sources of energy (such as simulated lightning or UV irradiation), "Wächtershäuser systems" come with a built-in source of energy, sulfides of iron and other minerals (e.g. pyrite). The energy released from redox reactions of these metal sulfides is not only available for the synthesis of organic molecules, but also for the formation of oligomers and polymers. It is therefore hypothesized that such systems may be able to evolve into autocatalytic sets of self-replicating, metabolically active entities that would predate the life forms known today.

The experiment produced a relatively small yield of dipeptides (0.4% to 12.4%) and a smaller yield of tripeptides (0.10%) but the authors also noted that: "under these same conditions dipeptides hydrolysed rapidly."

Radioactive beach theory

Zachary Adam at the University of Washington, Seattle, claims that stronger tidal processes from a much closer moon may have concentrated radioactive grains of uranium and other radioactive elements at the high water mark on primordial beaches where they may have been responsible for generating life's building blocks. According to computer models reported in Astrobiology, vol 7 p 852, a desposit of such radioactive materials could show the same self-sustaining nuclear reaction as that found in the Oklo uranium ore seam in Gabon. Such radioactive beach sand provides sufficient energy to generate organic molecules, such as amino acids and sugars from acetonitrile in water. Radioactive monazite also releases soluble phosphate into regions between sand-grains, making it biologically "accessible". Thus amino acids, sugars and soluble phosphates can all be simultaneously produced, according to Adam. Radioactive actinides, then in greater concentrations, could have formed part of organo-metallic complexes. These complexes could have been important early catalysts to living processes.

John Parnell of the University of Aberdeen suggests that such a process could provide part of the "crucible of life" on any early wet rocky planet, so long as the planet is large enough to have generated a system of plate tectonics which brings radioactive minerals to the surface. As the early Earth is believed to have many smaller "platelets" it would provide a suitable environment for such processes.

Homochirality

Some process in chemical evolution must account for the origin of homochirality, i.e. all building blocks in living organisms having the same "handedness" (amino acids being left-handed, nucleic acid sugars (ribose and deoxyribose) being right-handed, and chiral phosphoglycerides). Chiral molecules can be synthesized, but in the absence of a chiral source or a chiral catalyst are formed in a 50/50 mixture of both enantiomers. This is called a racemic mixture. Clark has suggested that homochirality may have started in space, as the studies of the amino acids on the Murchison meteorite showed L-analine to be more than twice as frequent as its D form, and L-glutamic acid was more than 3 times prevalent than its D counterpart. It is suggested that polarised light has the power to destroy one enantiomer within the proto-planetary disk. Noyes showed that beta decay caused the breakdown of D-leucine, in a racemic mixture, and that the presence of C, present in larger amounts in organic chemicals in the early Earth environment, could have been the cause. Once established, chirality would be selected for.

Self-organization and replication

This section needs expansion. You can help by adding to it.

While features of self-organization and self-replication are often considered the hallmark of living systems, there are many instances of abiotic molecules exhibiting such characteristics under proper conditions. For example Martin and Russel show that physical compartmentation by cell membranes from the environment and self-organization of self-contained redox reactions are the most conserved attributes of living things, and they argue therefore that inorganic matter with such attributes would be life's most likely last common ancestor.

From organic molecules to protocells

The question "How do simple organic molecules form a protocell?" is largely unanswered but there are many hypotheses. Some of these postulate the early appearance of nucleic acids ("genes-first") whereas others postulate the evolution of biochemical reactions and pathways first ("metabolism-first"). Recently, trends are emerging to create hybrid models that combine aspects of both.

"Genes first" models: the RNA world

The RNA world hypothesis suggests that relatively short RNA molecules could have spontaneously formed that were capable of catalyzing their own continuing replication. It is difficult to gauge the probability of this formation. A number of theories of modes of formation have been put forward. Early cell membranes could have formed spontaneously from proteinoids, protein-like molecules that are produced when amino acid solutions are heated - when present at the correct concentration in aqueous solution, these form microspheres which are observed to behave similarly to membrane-enclosed compartments. Other possibilities include systems of chemical reactions taking place within clay substrates or on the surface of pyrite rocks. Factors supportive of an important role for RNA in early life include its ability to act both to store information and catalyse chemical reactions (as a ribozyme); its many important roles as an intermediate in the expression and maintenance of the genetic information (in the form of DNA) in modern organisms; and the ease of chemical synthesis of at least the components of the molecule under conditions approximating the early Earth. Relatively short RNA molecules which can duplicate others have been artificially produced in the lab.

Researches have pointed out difficulties for the abiogenic synthesis of nucleotides from cytosine and uracil. Cytosine has a half-life of 19 days at 100°C and 17,000 years in freezing water. Larralde et al, say that "the generally accepted prebiotic synthesis of ribose, the formose reaction, yields numerous sugars without any selectivity." and they conclude that their "results suggest that the backbone of the first genetic material could not have contained ribose or other sugars because of their instability." The ester linkage of ribose and phosphoric acid in RNA is known to be prone to hydrolysis.

A slightly different version of this hypothesis is that a different type of nucleic acid, such as PNA, TNA or GNA, was the first one to emerge as a self-reproducing molecule, to be replaced by RNA only later.

"Metabolism first" models: iron-sulfur world and others

Several models reject the idea of the self-replication of a "naked-gene" and postulate the emergence of a primitive metabolism which could provide an environment for the later emergence of RNA replication.

One of the earliest incarnations of this idea was put forward in 1924 with Aleksandr Ivanovich Oparin's notion of primitive self-replicating vesicles which predated the discovery of the structure of DNA. More recent variants in the 1980s and 1990s include Günter Wächtershäuser's iron-sulfur world theory and models introduced by Christian de Duve based on the chemistry of thioesters. More abstract and theoretical arguments for the plausibility of the emergence of metabolism without the presence of genes include a mathematical model introduced by Freeman Dyson in the early 1980s and Stuart Kauffman's notion of collectively autocatalytic sets, discussed later in that decade.

However, the idea that a closed metabolic cycle, such as the reductive citric acid cycle, could form spontaneously (proposed by Günter Wächtershäuser) remains unsupported. According to Leslie Orgel, a leader in origin-of-life studies for the past several decades, there is reason to believe the assertion will remain so. In an article entitled "Self-Organizing Biochemical Cycles", Orgel summarizes his analysis of the proposal by stating, "There is at present no reason to expect that multistep cycles such as the reductive citric acid cycle will self-organize on the surface of FeS/FeS2 or some other mineral." It is possible that another type of metabolic pathway was used at the beginning of life. For example, instead of the reductive citric acid cycle, the "open" acetyl-CoA pathway (another one of the four recognised ways of carbon dioxide fixation in nature today) would be even more compatible with the idea of self-organisation on a metal sulfide surface. The key enzyme of this pathway, carbon monoxide dehydrogenase/acetyl-CoA synthase harbours mixed nickel-iron-sulfur clusters in its reaction centers and catalyses the formation of acetyl-CoA (which may be regarded as a modern form of acetyl-thiol) in a single step.

Bubble Theory

Waves breaking on the shore create a delicate foam composed of bubbles. Winds sweeping across the ocean have a tendency to drive things to shore, much like driftwood collecting on the beach. It is possible that organic molecules were concentrated on the shorelines in much the same way. Shallow coastal waters also tend to be warmer, further concentrating the molecules through evaporation. While bubbles composed mostly of water burst quickly, water containing amphiphiles forms much more stable bubbles, lending more time to the particular bubble to perform these crucial experiments.

Amphiphiles are oily compounds containing a hydrophilic head on one or both ends of a hydrophobic molecule. Some amphiphiles have the tendency to spontaneously form membranes in water. A spherically closed membrane contains water and is a hypothetical precursor to the modern cell membrane. If a protein came along that increased the integrity of its parent bubble, then that bubble had an advantage, and was placed at the top of the natural selection waiting list. Primitive reproduction can be envisioned when the bubbles burst, releasing the results of the experiment into the surrounding medium. Once enough of the 'right stuff' was released into the medium, the development of the first prokaryotes, eukaryotes, and multicellular organisms could be achieved.

Similarly, bubbles formed entirely out of protein-like molecules, called microspheres, will form spontaneously under the right conditions. But they are not a likely precursor to the modern cell membrane, as cell membranes are composed primarily of lipid compounds rather than amino-acid compounds (for types of membrane spheres associated with abiogenesis, see protobionts, micelle, coacervate).

A recent model by Fernando and Rowe suggests that the enclosure of an autocatalytic non-enzymatic metabolism within protocells may have been one way of avoiding the side-reaction problem that is typical of metabolism first models.

Other models

Autocatalysis

British ethologist Richard Dawkins wrote about autocatalysis as a potential explanation for the origin of life in his 2004 book The Ancestor's Tale. Autocatalysts are substances which catalyze the production of themselves, and therefore have the property of being a simple molecular replicator. In his book, Dawkins cites experiments performed by Julius Rebek and his colleagues at the Scripps Research Institute in California in which they combined amino adenosine and pentafluorophenyl ester with the autocatalyst amino adenosine triacid ester (AATE). One system from the experiment contained variants of AATE which catalysed the synthesis of themselves. This experiment demonstrated the possibility that autocatalysts could exhibit competition within a population of entities with heredity, which could be interpreted as a rudimentary form of natural selection.

Clay theory

A model for the origin of life based on clay was forwarded by Dr A. Graham Cairns-Smith of the University of Glasgow in 1985 and adopted as a plausible illustration by several other scientists, including Richard Dawkins. Clay theory postulates that complex organic molecules arose gradually on a pre-existing, non-organic replication platform -- silicate crystals in solution. Complexity in companion molecules developed as a function of selection pressures on types of clay crystal is then exapted to serve the replication of organic molecules independently of their silicate "launch stage". It is, truly, "life from a rock."

Cairns-Smith is a staunch critic of other models of chemical evolution. However, he admits, that like many models of the origin of life, his own also has its shortcomings (Horgan 1991).

In 2007, Kahr and colleagues reported their experiments to examine the idea that crystals can act as a source of transferable information, using crystals of potassium hydrogen phthalate. "Mother" crystals with imperfections were cleaved and used as seeds to grow "daughter" crystals from solution. They then examined the distribution of imperfections in the crystal system and found that the imperfections in the mother crystals were indeed reproduced in the daughters. The daughter crystals had many additional imperfections. For a gene-like behavior the additional imperfections should be much less than the parent ones, thus Kahr concludes that the crystals "were not faithful enough to store and transfer information form one generation to the next".

"Deep-hot biosphere" model of Gold

The discovery of nanobes (filamental structures that are smaller than bacteria, but that may contain DNA in deep rocks) in the late 1990s has been informally linked with led to a controversial theory put forward by Thomas Gold in the 1970s that life first developed not on the surface of the Earth, but several kilometers below the surface.

It is now reasonably well established that microbial life is plentiful at shallow depths in the Earth (up to five kilometers below the surface) in the form of extremophile archaea, rather than the better-known eubacteria (which live in more accessible conditions). It is claimed that discovery of microbial life below the surface of another body in our solar system would lend significant credence to this theory. Thomas Gold also asserted that a trickle of food from a deep, unreachable, source is needed for survival because life arising in a puddle of organic material is likely to consume all of its food and become extinct. Gold's theory is that that flow of food is due to out-gassing of primordial methane from the Earth's mantle ; more conventional explanations of the food supply of deep microbes (away from sedimentary carbon compounds) is that the organisms subsist on hydrogen released by an interaction between water and (reduced) iron compounds in rocks

"Primitive" extraterrestrial life

An alternative to Earthly abiogenesis is the hypothesis that primitive life may have originally formed extraterrestrially, either in space or on a nearby planet (Mars). (Note that exogenesis is related to, but not the same as, the notion of panspermia). A supporter of this theory is Francis Crick.

Organic compounds are relatively common in space, especially in the outer solar system where volatiles are not evaporated by solar heating. Comets are encrusted by outer layers of dark material, thought to be a tar-like substance composed of complex organic material formed from simple carbon compounds after reactions initiated mostly by irradiation by ultraviolet light. It is supposed that a rain of material from comets could have brought significant quantities of such complex organic molecules to Earth.

An alternative but related hypothesis, proposed to explain the presence of life on Earth so soon after the planet had cooled down, with apparently very little time for prebiotic evolution, is that life formed first on early Mars. Due to its smaller size Mars cooled before Earth (a difference of hundreds of millions of years), allowing prebiotic processes there while Earth was still too hot. Life was then transported to the cooled Earth when crustal material was blasted off Mars by asteroid and comet impacts. Mars continued to cool faster and eventually became hostile to the continued evolution or even existence of life (it lost its atmosphere due to low volcanism), Earth is following the same fate as Mars, but at a slower rate.

Neither hypothesis actually answers the question of how life first originated, but merely shifts it to another planet or a comet. However, the advantage of an extraterrestrial origin of primitive life is that life is not required to have evolved on each planet it occurs on, but rather in a single location, and then spread about the galaxy to other star systems via cometary and/or meteorite impact. Evidence to support the plausibility of the concept is scant, but it finds support in recent study of Martian meteorites found in Antarctica and in studies of extremophile microbes. Additional support comes from a recent discovery of a bacterial ecosytem whose energy source is radioactivity.

The Lipid World

There is a theory that ascribes the first self-replicating object to be lipid-like. It is known that phospholipids spontaneously form bilayers in water - the same structure as in cell membranes. These molecules were not present on early earth, however other amphiphilic long chain molecules also form membranes. Furthermore, these bodies may expand (by insertion of additional lipids), and under excessive expansion may undergo spontaneous splitting which preserves the same size and composition of lipids in the two progenies. The main idea in this theory is that the molecular composition of the lipid bodies is the preliminary way for information storage, and evolution led to the appearance of polymer entities such as RNA or DNA that may store information favorably. Still, no biochemical mechanism has been offered to support the Lipid World theory.

The Polyphosphate model

The problem with most scenarios of abiogenesis is that the thermodynamic equilibrium of amino acid versus peptides is in the direction of separate amino acids. What has been missing is some force that drives polymerization. The resolution of this problem may well be in the properties of polyphosphates. Polyphosphates are formed by polymerization of ordinary monophosphate ions PO₄ by ultraviolet light. Polyphosphates cause polymerization of amino acids into peptides. Ample ultraviolet light must have existed in the early oceans. The key issue seems to be that calcium reacts with soluble phosphate to form insoluble calcium phosphate (apatite), so some plausible mechanism must be found to keep free calcium ions from solution.

PAH world hypothesis

Other sources of complex molecules have been postulated, including extraterrestrial stellar or interstellar origin. For example, from spectral analyses, organic molecules are known to be present in comets and meteorites. In 2004, a team detected traces of polycyclic aromatic hydrocarbons (PAH's) in a nebula. Those are the most complex molecules so far found in space. The use of PAH's has also been proposed as a precursor to the RNA world in the PAH world hypothesis.

Multiple genesis

Different forms of life may have appeared quasi-simultaneously in the early history of Earth. The other forms may be extinct, leaving distinctive fossils through their different biochemistry (e.g., using arsenic instead of phosphorus), survive as extremophiles, or simply be unnoticed through their being analoguous to organisms of the current life tree. Hartman for example combines a number of theories together, by proposing that

The first organisms were self-replicating iron-rich clays which fixed carbon dioxide into oxalic and other dicarboxylic acids. This system of replicating clays and their metabolic phenotype then evolved into the sulfide rich region of the hotspring acquiring the ability to fix nitrogen. Finally phosphate was incorporated into the evolving system which allowed the synthesis of nucleotides and phospholipids. If biosynthesis recapitulates biopoesis, then the synthesis of amino acids preceded the synthesis of the purine and pyrimidine bases. Furthermore the polymerization of the amino acid thioesters into polypeptides preceded the directed polymerization of amino acid esters by polynucleotides.

See also

• Important publications in origin of life
• Astrochemistry
• Biogenesis
• Drake equation
• History of Earth
• Mimivirus
• Planetary habitability
• Rare Earth hypothesis
• Common descent
• Zeolites
• Origin of the world's oceans
• Mediocrity principle
• Autocatalytic reactions and order creation

References

• Brooks, J (1973). Origins and Development of Living Systems. Academic Press. p. 359. ISBN 0-12-135740-6. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
• De Duve, Christian (1996). Vital Dust: The Origin and Evolution of Life on Earth. Basic Books. ISBN 0-465-09045-1. {{cite book}}: Cite has empty unknown parameter: |1= (help); Unknown parameter |month= ignored (help)
• Fernando CT, Rowe, J (2007). "Natural selection in chemical evolution". Journal of Theoretical Biology. 247: 152–67.{{cite journal}}: CS1 maint: multiple names: authors list (link)
• Horgan, J (1991). "In the beginning". Scientific American. 264: 100–109. (Cited on p. 108).
• Huber, C. and Wächterhäuser, G., (1998). "Peptides by activation of amino acids with CO on (Ni,Fe)S surfaces: implications for the origin of life". Science. 281: 670–672.{{cite journal}}: CS1 maint: extra punctuation (link) CS1 maint: multiple names: authors list (link) (Cited on p. 108).
• Martin, W. and Russell M.J. (2002). "On the origins of cells: a hypothesis for the evolutionary transitions from abiotic geochemistry to chemoautotrophic prokaryotes, and from prokaryotes to nucleated cells". Philosophical Transactions of the Royal Society: Biological sciences. 358: 59–85.
• Russell MJ, Hall AJ, Cairns-Smith AG, Braterman PS (1988). "Submarine hot springs and the origin of life". Nature. 336: 117.{{cite journal}}: CS1 maint: multiple names: authors list (link)
• JW Schopf; et al. (2002). "Laser-Raman imagery of Earth's earliest fossils". Nature. 416: 73–76. PMID 11882894. {{cite journal}}: Explicit use of et al. in: |author= (help)
• Maynard Smith, John (2000-03-16). The Origins of Life: From the Birth of Life to the Origin of Language. Oxford Paperbacks. ISBN 0-19-286209-X. {{cite book}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
• Hazen, Robert M. (2005). Genesis: The Scientific Quest for Life's Origins. Joseph Henry Press. ISBN 0-309-09432-1. {{cite book}}: Unknown parameter |month= ignored (help)
• Morowitz, Harold J. (1992) "Beginnings of Cellular Life: Metabolism Recapitulates Biogenesis". Yale University Press. ISBN 0-300-05483-1

External links

• Template:PDFlink
• "SELF-REPLICATION: Even peptides do it" by Stuart A. Kauffman (web archive version as original page no longer accessible)
• Origins of Life website including papers, resources, by Dr. Michael Russell at the U. of Glasgow
• Possible Connections Between Interstellar Chemistry and the Origin of Life on the Earth
• Scientists Find Clues That Life Began in Deep Space — NASA Astrobiology Institute
• Self-organizing biochemical cycles — by Leslie Orgel
• How Life Began: New Research Suggests Simple Approach
• Primordial Soup's On: Scientists Repeat Evolution's Most Famous Experiment - an article in Scientific American. March 28, 2007
• Illustrations from Evolution (textbook)

Additional reading

• Buehler, Lukas K. (2000-2005) The physico-chemical basis of life, http://www.whatislife.com/about.html accessed 27 October 2005.
• Pitsch, S. Krishnamurthy, R. Arrhenius, G. (2000). Concentration of simple aldehydes by sulfite-containing double-layer hydroxide minerals: implications for biopoesis. Helvetica chimica acta. Sep-Oct. 83(9):2398-411.
• Hartman, H. (1998). Photosynthesis and the origin of life. Orig Life Evol Biosph. Oct. 28(4-6):515-21.
• Things Come to Life by Henry Harris (2002) ISBN 0-19-851538-3
• Arrhenius, G. Sales, B. Mojzsis, S. Lee, T. (1997). Entropy and charge in molecular evolution--the case of phosphate. J Theor Biol. Aug 21. 187(4):503-22.
• NASA Astrobiology Institute: Earth's Early Environment and Life
• NASA Specialized Center of Research and Training in Exobiology: Gustaf O. Arrhenius

Notes

1. "Is this life? ABC Science Online". Retrieved 2007-07-10.
2. Simon A. Wilde, John W. Valley, William H. Peck and Colin M. Graham, Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago, Nature 409, 175-178 (2001) doi:10.1038/35051550
3. "www.journals.royalsoc.ac.uk/content/01273731t4683245/". Retrieved 2007-07-10.
4. "geology.geoscienceworld.org/cgi/content/abstract/34/3/153". Retrieved 2007-07-10.
5. "www.journals.royalsoc.ac.uk/content/887701846v502u58/". Retrieved 2007-07-10.
6. "www.journals.royalsoc.ac.uk/content/814615517u5757r6/". Retrieved 2007-07-10.
7. "map.gsfc.nasa.gov/m_mm/mr_age.html". Retrieved 2007-07-10.
8. Chapter 6, last section in Alberts B, Johnson A, Lewis J, Raff M, Roberts K and Walter P, Molecular Biology of the Cell, 4th Edition, Routledge, March, 2002, ISBN 0-8153-3218-1.
9. First life on Earth windmillministries.org, Retrieved on- 2008-01-18
10. "It is often said that all the conditions for the first production of a living organism are now present, which could ever have been present. But if (and oh! what a big if!) we could conceive in some warm little pond, with all sorts of ammonia and phosphoric salts, light, heat, electricity, &c., present, that a proteine compound was chemically formed ready to undergo still more complex changes, at the present day such matter would be instantly devoured or absorbed, which would not have been the case before living creatures were formed." written in 1871, published in Darwin, Francis, ed. 1887. The life and letters of Charles Darwin, including an autobiographical chapter. London: John Murray. Volume 3. p. 18
11. Oparin, A. I. (1968), The Origin and Development of Life (NASA TTF-488). Washington: D.C.L GPO,1968
12. Oparin, A. I. The Origin of Life. New York: Dover (1952)
13. Bryson, Bill (2003) A Short History of Nearly Everything pp. 300-302; ISBN 0-552-99704-8
14. Morse, J.W. and MacKenzie, F.T. (1998). "Hadean Ocean Carbonate chemistry." In: Aquatic Geochemistry 4: 301–319
15. Wilde, S.A. et al (2001), "Evidence from detrital zircons for the existence of continental crust and oceans 4.4 Gyr ago", "Nature"409 pp.175-178
16. Sleep, N.H. et al (1989) "Annihilation of ecosystems by large asteroid impacts on early Earth" "Nature"342, pp139-142
17. Maher, Kevin A. and Stephenson, David J (19880 "Impact frustration of the origin of life" (Nature. Vol. 331, pp. 612-614. 18 Feb. 1988)
18. Michael P. Robertson and Stanley L. Miller, "An Efficient Prebiotic Synthesis of Cytosine and Uracil," Nature 375 (1995), pp. 772-774
19. J.L. Bada, C. Bigham, and S.L. Miller, "Impact Melting of Frozen Oceans on the Early Earth: Implications for the Origin of Life," Proceedings of the National Academy of Sciences, USA 91 (February 1994), pp. 1248-1250
20. Levy, M (2000). "Prebiotic synthesis of adenine and amino acids under Europa-like conditions". Icarus. 145 (2): 609–13. PMID 11543508. Retrieved 2008-02-11. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help); Unknown parameter |month= ignored (help)
21. Trinks, Hauke (2005). "Ice And The Origin Of Life". Origins of Life and Evolution of the Biosphere. 35 (5): 429–445. doi:10.1007. Retrieved 2008-02-11. {{cite journal}}: Check |doi= value (help); Unknown parameter |coauthors= ignored (|author= suggested) (help); Unknown parameter |month= ignored (help)
22. Discover Magazine article Did Life Evolve in Ice? published February 2008
23. Mojzis, S.J. et al (1996), "Evidence for life on earth before 3,800 million years ago", "Nature" 384 pp.55-59
24. Lazcano A, and S.L. Miller (1994) "How long did it take for life to begin and evolve to cyanobacteria"" "Journal of Molecular Evolution" 39 pp.546-554
25. Chyba, Christopher and Sagan, Carl (1992),"Endogenous production, exogenous delivery and impact-shock synthesis of organic molecules: an inventory for the origins of life" (Nature 355, 125 - 132 (09 January 1992))
26. Experiments on origin of organic molecules Nitro.biosci.arizona.edu, Retrieved on- 2008-13-01
27. Manfred Eigen and Peter Schuster: The Hypercycle: A principle of natural self-organization, 1979, Springer ISBN 0-387-09293-5
28. origin of life thebioreview.com Retrieved on- 2008-01-14
29. Huber, C. and Wächterhäuser, G., (1998). "Peptides by activation of amino acids with CO on (Ni,Fe)S surfaces: implications for the origin of life". Science 281: 670–672.
30. Dartnell, Lewis "Life's a beach on planet Earth" in New Scientist 12 January 2008
31. Noyes, H. Pierre; Bonner, William A.; and Tomlin, J. A. (1977), "On the origin of biological chirality via natural beta-decay" (Origins of Life and Evolution of Biospheres, Volume 8, Number 1 / April, 1977)
32. Clark, S. (1999), "Polarised starlight and the handedness of Life" (American Scientist 97, pp336-343)
33. Martin, William; and Russel, Michael J (2003), "On the origins of cells: a hypothesis for the evolutionary transitions from abiotic geochemistry to chemoautotrophic prokaryotes, and from prokaryotes to nucleated cells " (Philosophiocal Transactions of the Royal Society, Volume 358, Number 1429/January 29, 2003)
34. W. K. Johnston, P. J. Unrau, M. S. Lawrence, M. E. Glasner and D. P. BartelRNA-Catalyzed RNA Polymerization: Accurate and General RNA-Templated Primer Extension, Science 292, 1319 (2001)
35. L. Orgel, The origin of life on earth. Scientific American. 271 (4) p. 81, 1994.
36. Matthew Levy and Stanley L. Miller, The stability of the RNA bases: Implications for the origin of life, Proceedings of the National Academy of Science USA 95, 7933–7938 (1998)
37. Larralde R, Robertson M P, Miller S L. Proc Natl Acad Sci USA. 1995;92:8158–8160.
38. Lindahl T. Nature (London). 1993;362:709–715.
39. Orgel, Leslie (Nov 2000). "A Simpler Nucleic Acid". Science 290 (5495): 1306 - 1307
40. Nelson, K.E., Levy, M., and Miller, S.L. Peptide nucleic acids rather than RNA may have been the first genetic molecule (2000) Proc. Natl. Acad. Sci. USA 97, 3868–3871.
41. PNAS, vol. 97, no. 23, November 7 2000, p12503-12507
42. "The Cell: Evolution of the First Organism" by Joseph Panno
43. "www.cogs.susx.ac.uk/users/ctf20/dphil_2005/publications.htm". Retrieved 2007-07-10.
44. Genetic Takeover: And the Mineral Origins of Life ISBN 0-521-23312-7
45. Test of Cairns-Smiths crystals-as-genes hypothesis, Theresa Bullard, John Freudenthal, Serine Avagyan and Bart Kahr, Faraday Discuss., 2007, DOI: 10.1039/b616612c
46. Caroline Moore (16 July 2007). "Crystals as genes?". Chemical Science.
47. ^ Nanobes- Intro microscopy-uk.org, Retrieved on- 2008-01-14
48. "http://www.newscientist.com/channel/life/evolution/dn2844". Retrieved 2007-07-10. {{cite web}}: External link in |title= (help)
49. Lin, Li-Hung (2006). "Long-Term Sustainability of a High-Energy, Low-Diversity Crustal Biome". Science. 314: 479–482. doi:10.1126/science.1127376. 5798. {{cite journal}}: |access-date= requires |url= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help); Unknown parameter |month= ignored (help)
50. "ool.weizmann.ac.il/". Retrieved 2007-07-10.
51. "www.pubmedcentral.nih.gov/articlerender.fcgi?artid=528972". Retrieved 2007-07-10.
52. "www.science.siu.edu/microbiology/micr425/425Notes/14-OriginLife.html". Retrieved 2007-07-10.
53. Discovery of Blue Fluorescence by Polycyclic Aromatic Hydrocarbon Molecules in the Red Rectangle. A. N. Witt, et al
54. Battersby, S. (2004). Space molecules point to organic origins. Retrieved January 11, 2004 from http://www.newscientist.com/news/news.jsp?id=ns99994552
55. Are Aliens Among Us? In pursuit of evidence that life arose on Earth more than once, scientists are searching for microbes that are radically different from all known organisms Scientific American. 19 November 2007
56. artman, Hyman (1998) "Photosynthesis and the Origin of Life" (Origins of Life and Evolution of Biospheres, Volume 28, Numbers 4-6 / October, 1998)

• Biology theories
• Origin of life