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Rare Earth hypothesis
In planetary astronomy and astrobiology, the Rare Earth hypothesis argues that the emergence of complex multicellular life (metazoa) on Earth required an improbable combination of astrophysical and geological events and circumstances. The term "Rare Earth" comes from Rare Earth: Why Complex Life Is Uncommon in the Universe, the title of a book by Peter Ward, a geologist and paleontologist, and Donald Brownlee, an astronomer and astrobiologist. Their book is the source for much of this entry.
The rare earth hypothesis is the contrary of the principle of mediocrity (also called the Copernican principle), advocated by Carl Sagan and Frank Drake, among others. The principle of mediocrity concludes that the Earth is a typical rocky planet in a typical planetary system, located in an unexceptional region of a large but conventional barred-spiral galaxy. Hence it is probable that the universe teems with complex life. Ward and Brownlee argue to the contrary: planets, planetary systems, and galactic regions that are as friendly to complex life as are the Earth, the solar system, and our region of the Milky Way are probably very rare.
By concluding that complex life is uncommon, the Rare Earth hypothesis solves the Fermi paradox: "If extraterrestrial aliens are common, why aren't they obvious?"
Why complex life may be very rare
The Rare Earth hypothesis argues that the emergence of complex life required a host of fortuitous circumstances. A number of such circumstances are set out below under the following headings: galactic habitable zone, a central star and planetary system having the requisite character, the circumstellar habitable zone, the size of the planet, the advantage of a large satellite, conditions needed to assure the planet has a magnetosphere and plate tectonics, the chemistry of the lithosphere, atmosphere, and oceans, the role of "evolutionary pumps" such as massive glaciation and rare bolide impacts, and whatever led to the still mysterious Cambrian explosion of animal phyla. The emergence of intelligent life may have required yet other rare events.
In order for a small rocky planet to support complex life, Ward and Brownlee argue, the values of several variables must fall within narrow ranges. The universe is so vast that it could contain multiple Earth-like planets. But if such planets exist, they are likely to be separated from each other by many thousands of light years. Such distances may preclude communication among any intelligent species evolving on such planets, which would solve the Fermi paradox.
The galactic habitable zone
Rare Earth suggests that much of the known universe, including large parts of our galaxy, cannot support complex life; Ward and Brownlee refer to such regions as "dead zones." Those parts of a galaxy where complex life is possible make up the galactic habitable zone. This zone is primarily a function of distance from the galactic center. As that distance increases:
(1) rules out the outer reaches of a galaxy; (2) and (3) rule out galactic inner regions, globular clusters, and the spiral arms of spiral galaxies. These arms are not physical objects, but regions of a galaxy characterized by a higher rate of star formation, moving very slowly through the galaxy in a wave-like manner. As one moves from the center of a galaxy to its furthest extremity, the ability to support life rises then falls. Hence the galactic habitable zone may be ring-shaped, sandwiched between its uninhabitable center and outer reaches.
While a planetary system may enjoy a location favorable to complex life, it must also maintain that location for a span of time sufficiently long for complex life to evolve. Hence a central star with a galactic orbit that steers clear of galactic regions where radiation levels are high, such as the galactic center and the spiral arms, would appear most favourable. If the central star's galactic orbit is eccentric (eliptical or hyperbolic), it will pass through some spiral arms, but if the orbit is a near perfect circle and the orbital velocity equals the "rotational" velocity of the spiral arms, the star will drift into a spiral arm region only gradually, if at all. Therefore Rare Earth proponents conclude that a life-bearing star must have a galactic orbit that is nearly circular about the center of its galaxy. The required synchronization of the orbital velocity of a central star with the wave velocity of the spiral arms can occur only within a fairly narrow range of distances from the galactic center. This region is termed the "galactic habitable zone". Lineweaver et al  calculate that the galactic habitable zone is an annular ring 7 to 9 kiloparsecs in diameter, that includes no more than 10% of the stars in the Milky Way. Based on conservative estimates of the total number of stars in the galaxy, this could represent something like 20 to 40 billion stars. Gonzalez et al  would halve these numbers; he estimates that at most 5% of stars in the Milky Way fall in the galactic habitable zone.
The orbit of the Sun around the center of the Milky Way is indeed almost perfectly circular, with a period of 226 Ma, one closely matching the rotational period of the galaxy. However, Masters (2002) calculates that the orbit of the Sun takes it through a spiral arm approximately every 100 million years. In contrast, the Rare Earth hypothesis predicts that the Sun, since its formation, should have passed through no spiral arm at all.
A central star of the right character
It is generally accepted by exobiologists that the central star for a life-bearing planet must be of appropriate size. Large stars emit much ultraviolet radiation, which precludes life other than underground microbes. Large stars also exist for millions, not billions, of years, after which they explode as supernovae. A supernova remnant becomes a neutron star or black hole, giving off high energy x-ray and gamma radiation. Hence the planets orbiting the large, hot or binary stars believed to give rise to supernovae do not exist long enough to allow complex life to evolve.
The terrestrial example suggests complex life requires water in the liquid state and its planet must therefore be at an appropriate distance. This is the core of the notion of the habitable zone or Goldilocks Principle . The habitable zone forms a ring around the central star. If a planet orbits its sun too closely or too far away, the surface temperature is incompatible with water being liquid (though sub-surface water, as suggested for Europa, may be possible at varying locations). Kasting et al (1993) estimate that the habitable zone for the Sun ranges from 0.95 to 1.15 astronomical units.
The habitable zone varies with the type and age of the central star. The habitable zone for a main sequence star very gradually moves out over time until the star becomes a white dwarf, at which time the habitable zone vanishes. The habitable zone is closely connected to the greenhouse warming afforded by atmospheric carbon dioxide (CO2). Even though the Earth's atmosphere contains only 350 parts per million of CO2, that trace amount suffices to raise the average surface temperature of the Earth by about 40°C from what it would otherwise be .
It is then presumed a star needs to have rocky planets within its habitable zone. While the habitable zone of hot stars, such as Sirius or Vega is wide, there are two problems:
These considerations rule out the massive and powerful stars of type F6 to O (see stellar classification).
Small red dwarf stars, on the other hand, have habitable zones with a small radius. This proximity causes one face of the planet to constantly face the star, and the other to always remain dark, a situation known as tidal lock. Tidal lock rules out axial rotation; hence one side of a planet will be extremely hot, while the other will be extremely cold. Planets within a habitable zone with a small radius are also at increased risk of solar flares (see Aurelia), which would tend to ionize the atmosphere and are otherwise inimical to complex life. Rare Earth proponents argue that this rules out the possibility of life in such systems, though some exobiologists have suggested that habitability may exist under the right circumstances. This is a central point of contention for the theory, since these K and M category stars are estimated to make up 90% of all stars.
Rare Earth proponents argue that the stellar type of central stars that are "just right" ranges from F7 to K1. Such stars are not common: G type stars such as the Sun (between the hotter F and cooler K) comprise only 5% of the stars in the Milky Way. Aged stars, such as red giants and white dwarfs, are also unlikely to support life. Red giants are common in globular clusters and elliptical galaxies. White dwarfs are mostly dying stars that have already gone through their red giant phase. The diameter of a red giant has substantially increased from its youth. If a planet was in the habitable zone during a star's youth and middle age, it will be fried when its parent star becomes a red giant (though theoretically planets at a much greater distance may become habitable).
The energy output of a star over its lifespan should only change very gradually; variable stars such as Cepheid variables, for instance, are highly unlikely to support life. If the central star's energy output suddenly decreases, even for a relatively short while, the planet's water may freeze. Conversely, if the central star's energy output temporarily increases, the oceans may evaporate, resulting in a greenhouse effect; this may preclude the oceans from reforming.
There is no known way to achieve life without complex chemistry, and such chemistry requires metals, namely elements other than hydrogen, helium, and lithium. This suggests a condition for life is a solar system rich in metals. The only known mechanism for creating and dispersing metals is a supernova explosion. The presence of metals in stars is revealed by their absorption spectrum, and studies of stellar spectra reveal that many, perhaps most, stars are poor in metals. Low metallicity characterizes the early universe, globular clusters and other stars formed when the universe was young, stars in most galaxies other than large spirals, and stars in the outer regions of all galaxies. Thus metal-rich central stars capable of supporting complex life are believed most common in the quiet suburbs of the larger spiral galaxies, regions hospitable to complex life for another reason, namely the absence of high radiation.
If a star is poor in metals, any associated planetary system is likely poor in metals as well. In order to have rocky planets like the Earth, a central star must have condensed out of a nebula that was fairly metal-rich. Only gas giant planets will condense out of a metal-poor nebula; such a nebula simply lacks the material required to form terrestrial planets.
A gas cloud capable of giving birth to a star can also give rise to gas giant (Jovian) planets like Jupiter and Saturn. But Jovian planets have no hard surface of the kind believed necessary for complex life (their satellites may have hard surfaces, though). Hence a planetary system capable of sustaining complex life must be structured more or less like the solar system, with small and rocky inner planets, and Jovian outer ones. Alternatively there can be small rocky satellites of Jovial planets.
Some planetary systems, especially their outer regions, are riddled with comets and asteroids which sometimes collide with planets. Such collisions, known as bolide impacts, have often been highly disruptive for complex life. Hence bolide impacts must be rare (but nonexistent is not necessarily best either; see below) during the billions of years required for complex life to emerge. The frequency of bolide impacts on inner planets was thought to be reduced if there are lifeless planets at the right distance from the central star, and with sufficient gravity either to attract comets and asteroids to themselves or to eject them from the planetary system.
Uncertainty over Jupiter
Thanks to its gravitational force, a gas giant ejects the debris from planet formation into the equivalent of the Kuiper belt and Oort cloud. Hence a gas giant was thought to protect the inner rocky planets from asteroid bombardment. Recent computer simulations suggest that the situation may be more complex than this, however, with gas giants both protecting from and contributing to asteroid bombardment; Jupiter appears to cause about as many asteroid impacts as it prevents and replacing Jupiter with a Saturn-sized body would actually increase the bombardment.
Disruption of orbit
A gas giant must not be too close to a body upon which life is developing, unless that body is one of its moons. Close placement of gas giant(s) could disrupt the orbit of a potential life-bearing planet, either directly or by drifting into the habitable zone.
Newtonian dynamics can produce chaotic planetary orbits, especially in a system having large planets at high orbital eccentricity 
The need for stable orbits rules out planetary systems resembling those that have been discovered in recent years (extra-solar systems consisting of large planets with close orbits, known as hot Jupiters). It is believed that hot Jupiters formed much further from their parent stars than they are now, and have migrated inwards to their current orbits. In the process, they would have catastrophically disrupted the orbits of any planets in the habitable zone. 
A planetary system capable of supporting complex life may need to include at least one large outer planet. But planetary systems with too many Jovian planets, or with a single one that is too large, are likely to be unstable, in which case the likely fate of a rocky inner planet able to support life is either to plunge into its central star or to be ejected into interstellar space.
Size of planet
(Lissauer 1999, as summarized by Conway Morris 2003: 92; also see Comins 1993). A planet that is too small cannot hold much of an atmosphere. Hence the surface temperature becomes more variable and the average temperature drops. Water will either freeze, boil away, or decompose under the action of UV radiation; in any event, substantial and long-lasting oceans become impossible. A small planet will also tend to have a rough surface, with large mountains and deep canyons. The core will cool faster, and plate tectonics will either not last as long as they would on a larger planet or may not occur at all.
If a planet's size is such that its gravitational field substantially exceeds the Earth's, it will attract more bolides to itself. The stronger the gravitational field, the harder it is for mountains and continents to form. In the limit, such a planet would probably be covered with an ocean, in which case the lack of exposed rocks would rule out the feedback mechanism, described below, regulating atmospheric CO2.
The Moon is unusual because:
The giant impact theory hypothesizes that the Moon results from the impact of a Mars-sized body with the very young Earth. This giant impact also gave the Earth its axis tilt and velocity of rotation . Rapid rotation reduces the daily variation in temperature and makes photosynthesis viable. The Rare Earth hypothesis further argues that the axis tilt cannot be too large or too small (relative to the orbital plane). A planet with a large tilt will experience extreme seasonal variations in climate, unfriendly to complex life. A planet with little or no tilt will lack the stimulus to evolution that climate variation provides. In this view, the Earth's tilt is "just right". A large satellite can also act as a gyroscope, stabilising the planet's tilt; without this effect the tilt will be chaotic, presumably also causing difficulties for developing life forms.
If the Earth had no Moon, the ocean tides resulting solely from the Sun's gravity would be very modest. A large satellite gives rise to tidal pools, which may be essential for the formation of complex life.
A large satellite also increases the likelihood of plate tectonics through the effect of tidal forces on the planet's crust. The impact that formed the Moon may also have initiated plate tectonics, without which the continental crust would cover the entire planet, leaving no room for oceanic crust. It is possible that the large scale mantle convection needed to drive plate tectonics could not have emerged in the absence of crustal inhomogeneity. However, plate tectonics existed on Mars in past, without such a mechanism to initiate it. 
If a giant impact is the only way for a rocky inner planet to acquire a large satellite, any planet in the circumstellar habitable zone will need to form as a double planet in order that there be an impacting object sufficiently massive to give rise in due course to a large satellite. An impacting object of this nature is not necessarily improbable. Recent work by Edward Belbruno and J. Richard Gott of Princeton University suggests that a suitable impacting body could form in a planet's trojan points (L4 or L5).
A magnetosphere protects the biosphere from solar wind and cosmic rays, which are harmful to life. The magnetosphere results from a massive conductive planetary core made of solid and molten iron, acting as a dynamo. The iron is molten in part because of heat given off by the decay of radioactive elements. If complex life can exist only on the surface of a planet surrounded by a magnetosphere, then complex life requires a planet whose interior contains radioactive elements (such as uranium 238, thorium 232, and potassium 40). Moreover, these elements must have half lives long enough to sustain the magnetosphere for a time span long enough for complex life to evolve.
This is the most original part of Ward and Brownlee's analysis (however this section owes much to Webb 2002: 180-84). They argue that in order for a rocky planet to support animal life, its crust must experience plate tectonics. That is, the lithosphere must consist of large crustal plates that, along certain margins, are continuously created from fluid matter carried from the deep interior in convection cells. Along other margins, called subduction zones, these crustal plates are reabsorbed into the planet's interior.
A planet will not experience plate tectonics unless its chemical composition allows it. The only known long lasting source of the required heat is radioactive decay occurring deep in the planet's interior. Continents must also be made up of less dense granitic rocks that "float" on underlying more dense basaltic rock. Taylor  emphasizes that subduction zones (an essential part of plate tectonics) require the lubricating action of ample water; on Earth, such zones exist only at the bottom of oceans.
A large satellite also increases the likelihood of plate tectonics through the effect of tidal forces on the planet's crust. The impact that formed the Moon may also have initiated plate tectonics, without which the continental crust would cover the entire planet, leaving no room for oceanic crust. At present, it is not known whether the organization of the large scale mantle convection needed to drive plate tectonics could develop in the absence of crustal inhomogeneity.
The reasons why convection-driven plate tectonics promotes the development of complex life include the following. Plate tectonics:
By drawing heat from the interior to the surface, convection driven plate tectonics assures that if a planet has a core of molten iron, that core keeps moving. That motion means that the core of the earth acts like a dynamo, generating a magnetic field.
If the atmosphere contains too few greenhouse gases, the planet slides into a permanent ice age. Too much greenhouse gas, and the temperature becomes too high for complex life (many proteins denature at temperatures well short of the boiling point of water), and eventually the oceans turn to water vapor. One of the primary greenhouse gases in the Earth's atmosphere is carbon dioxide, CO2. It appears that plate tectonics play an important role in a complex feedback system (for details, see Ward and Brownlee) that stabilizes the Earth's temperature. Atmospheric CO2 combines with rainwater to form dilute carbonic acid. This acid interacts with surface rocks to form calcium carbonate, CaCO3, which is eventually deposited on the ocean bottom and carried into the Earth's interior at subduction zones. Thus CO2 is removed from the atmosphere. The high temperatures and pressures within the Earth's mantle transform CaCO3 into CO2 and CaO. This subterranean CO2 is eventually returned to the atmosphere via volcanism.
Feedback occurs because a rise in atmospheric CO2 results in higher temperatures via the greenhouse effect, and more rainfall, and more acid rainwater. Hence the rate at which CO2 is removed from the atmosphere rises. When atmospheric CO2 falls, the rate at which it is removed from the atmosphere declines. Plate tectonics exposes and buries rocks in a way that automatically regulates the CO2 content of the atmosphere. The result has been an Earth with a more or less steady surface temperature, even though the sun's energy output is believed to be about 25% greater now than it was when the Earth was young. Absent this recycling of atmospheric carbon, the expected lifetime of the biosphere would not exceed a few million years. Ice ages, by covering much of a planet's rocks and by reducing rainfall, interfere with this feedback process.
It is difficult to imagine how an aquatic species would smelt and shape metal ores or manipulate electricity (sea water is a fair electrical conductor thanks to its dissolved minerals). Hence it is likely that intelligent life with technology can only evolve on dry land; plate tectonics assures that a planet with ample water also has dry land. More generally, a planet with mountains, islands, and continents gives rise to more microclimates and evolutionary niches, which present evolution with more challenges. Hence plate tectonics promote biodiversity.
While plate tectonics appear to have helped complex life to evolve on Earth, how essential plate tectonics are for complex life in general, and the rarity of planets with plate tectonics, are both not well understood at present. The only object in the solar system other than the Earth believed to experience plate tectonics now is the Galilean moon Europa.
Chemistry of the atmosphere
Carbon-based biochemistry clearly requires a large supply of atmospheric carbon dioxide and crustal carbon (in the form of carbonate compounds); however large amounts of carbon would give rise to a runaway greenhouse effect. Atmospheric oxygen is necessary to support the metabolism of Earthly animals and hence intelligent life. Hence something like photosynthesis had to evolve to shift the atmosphere from a reducing one to an oxidizing one.
Central stars invariably emit ultraviolet (UV) radiation. UV radiation whose wavelength falls in the range of 260-90 nm is efficiently absorbed by nucleic acids and proteins, and hence is lethal for all forms of terrestrial life. Fortunately, ozone efficiently absorbs UV radiation in the range 200-300 nm, and atmospheric oxygen is the building block for ozone. Hence a planet with complex life living on dry land must have an ozone layer in its upper atmosphere. Oxygen first appeared in the atmosphere when UV radiation in the range 100-200 nm broke water down into its atomic components. Once there was enough of an ozone layer to permit photosynthetic microbes to evolve on the planet's surface, the oxygen content of the atmosphere gradually rose through photosynthesis, and is believed to have reached its present (or even higher) level during the Cambrian era. Hence an atmosphere sufficiently rich in oxygen may have been a necessary condition for the Cambrian explosion.
Even if conditions on a planet's surface allow water in the liquid phase, we cannot conclude that there will in fact be any water present. The inner planets in our solar system were formed with little water. Much of the water in the oceans is believed to have been brought to Earth by the icy asteroid impacts during the early bombardment phase about 4.5 Ga. The oceans play a crucial role in moderating the seasonal swings in the Earth's temperature. The high specific heat of water enables oceans to warm slowly during the summer and then to give up their summer heat over the following winter. Too much water, on the other hand, leads to a planet with little or no land, and hence no weathering mechanism for regulating the carbon dioxide content of the atmosphere.
The evolution of life on Earth includes two very important and unexpected leaps, the emergence of:
The earliest unambiguous fossil evidence of multicellular life is the Ediacaran biota, about 580 Ma. Hence the better part of 2 billion years elapsed between the first and the second leaps. Meanwhile, only about 400 million years were required in order for the first multicellular animals (sponges and Ediacaran biota) to evolve into dinosaurs.
Curiously, both of these evolutionary transitions came hard on the heels of extended periods of glaciation so extensive that it is suspected that the earth was covered with ice, either entirely or over all but a narrow band about the Equator. This much ice cover would have raised the Earth's albedo to such an extent that the Earth's average temperature may have fallen to about -50°C. The thick ice covering almost all oceans ruled out any interactions between the oceans and the atmosphere. The continents were either covered with ice, or consisted of bare rock devoid of life. This scenario has been named Snowball Earth.
During such periods of catastrophic glaciation, life probably retreated to a narrow band near the equator, and to places warmed by tectonic activity, such as hydrothermal vents on the ocean floor, and volcanoes. Fortunately, glaciation interferes neither with plate tectonics nor with the resulting vulcanism. A hypothesized eventual rise in vulcanism increased atmospheric levels of greenhouse gases, which led to a dramatic increase in temperature and the end of the two apparent snowball earth episodes.
The first Snowball Earth episode, the Huronian glaciation, began about 2.4 Ga, shortly after the appearance of the oldest known eukaryotic unicellular organisms. The second episode, the Cryogenian period, lasted from 850 Ma to 635 Ma, ending about 50 Ma before the emergence of the Ediacaran biota. It is an open question what role, if any, these ice ages played in triggering the emergence of complex life. In any event, when the glaciation ended, life eventually sprang back with renewed vigor and diversity. The Cambrian explosion began 542 Ma, in which representatives of all currently extant (and some now extinct) animal phyla suddenly appear in the fossil record. Just how or why the Cambrian explosion came about is still not understood, but it is likely to have resulted from one or more "evolutionary pumps."
More modest glaciations are also associated with rapid evolutionary change. The rapid evolution of hominids, which culminated in the appearance of homo sapiens about 200 ka, coincides with the oscillating Quarternary ice age that began about 1.5 Ma. Moreover, the agricultural revolution, when homo sapiens emerged as an aggressive discoverer of technology, began shortly after the last glacial retreat, around 12 ka.
The impact of a sufficiently massive asteroid or comet can act as an evolutionary pump. The evolution of complex life requires long periods of tranquility. Frequent impacts from large bolides, while not incompatible with the emergence and survival of microbes, make it unlikely that complex life will emerge and survive. Rare bolide impacts, however, while making many forms of complex life extinct, on balance appear to act as evolutionary pumps. A small number of mass-extinction events may be required to give evolution the chance to explore radical new approaches to the challenges of the environment, rather than remain trapped in a suboptimal local maximum.
A case in point is the asteroid impact that created the Chicxulub Crater, believed to have triggered the Cretaceous-Tertiary extinction event, when an estimated 70% of extant metazoans species, including all dinosaurs, became extinct.
Inertial interchange event
There is ample evidence that the rate of continental drift during the Cambrian explosion was unusually high. In fact, continents moved from Arctic to equatorial locations, and vice versa, in 15 million years or less. Kirschvink et al  have proposed the following controversial explanation: a 90° change in the Earth's axis of rotation resulting from an imbalance in the distribution of continental masses relative to the axis. The result was huge changes in climates, ocean currents, and so on, occurring in a very short time and affecting the entire Earth. They named their explanation the "inertial interchange event." This scenario is not yet received science, but if such an event took place then it is a very unlikely occurrence, and if such an event was required for the evolution of animal life more complex than sponges and coral reefs, then we have yet another reason why complex life will be rare in the universe.
Microbes may be common
Multicellular life does not include most microbes. The Rare Earth hypothesis permits microbial life to be far more common than complex life. This part of the hypothesis builds on the discovery, since 1980 or so, of extremophilic microorganisms that thrive in unusually hot, cold, dark, high pressure, salty, or acid conditions. Examples of such locations include rocks several kilometers under the surface of the Earth, hydrothermal vents on the ocean floor, and deep in Antarctic ice, as revealed by drilled ice cores. Some of these organisms are prokaryotes called Archaea that can gain energy from inorganic chemical reactions and do not require sunlight. Some of these extremophile Archaea also require an ambient temperature exceeding 80°C, and thrive in temperatures exceeding 100°C. Such conditions could well have been common deep in the oceans of the young Earth.
Evidence of single-celled microorganisms has been found in rocks dated about 3.5 Ga; hence these forms of life did not take very long to evolve, once the Earth's surface had cooled sufficiently. The domain Archaea suggests that microbial life can emerge fairly quickly in a much broader range of environments than those compatible with complex life. Hence the universe could well teem with simple microbes. Under the Rare Earth hypothesis, only eukaryotic, multicellular, animal, and intelligent life are rare, in that order.
Rare Earth equation
The following discussion is adapted from Cramer . The Rare Earth equation is Ward and Brownlee's riposte to the Drake equation. It calculates N, the number of Earth-like planets in the Milky Way having complex life forms, as:
We assume . The Rare Earth hypothesis can then be viewed as asserting that the product of the other nine Rare Earth equation factors listed below, which are all fractions, is no greater than 10-10 and could plausibly be as small as 10-12. In the latter case, N could be as small as 0 or 1. Ward and Brownlee do not actually calculate the value of N, because the numerical values of quite a few of the factors below can only be conjectured. They cannot be estimated simply because we have but one data point: the Earth, a rocky planet orbiting a G2 star in a quiet suburb of a large barred spiral galaxy, and the home of the only intelligent species we know, namely ourselves.
The Rare Earth equation, unlike the Drake equation, does not factor the probability that complex life evolves into intelligent life that discovers technology. (Keep in mind that Ward and Brownlee are not evolutionary biologists.) Barrow and Tipler  review the consensus among such biologists that the evolutionary path from primitive Cambrian chordates, e.g. Pikaia, to homo sapiens was a highly improbable event. For example, the large brains of humans have marked adaptive disadvantages, requiring as they do an expensive metabolism, a long gestation period, and a childhood lasting more than 25% of the average total life span. Other improbable features of humans include:
Books that advocate the Rare Earth hypothesis, listed in order of increasing difficulty, include:
Criticisms of the Rare earth Hypothesis take various forms.
Planets outside the Solar System
The main objection to the Rare Earth hypothesis is that it is based on a single observation, namely the Earth and its lifeforms. Current scientific instrumentation and search techniques, such as Doppler shift, cannot detect most extrasolar planets of a size and mass similar to the Earth's. Extrasolar planets detected to date are predominantly of Jupiter-mass or larger, which thus renders detectable their effect on the motion of their parent star. Therefore, as of 2006, there is no data on how common Earth-like planets are in the Milky Way. However, on April 24, 2007 astronomers announced the possible discovery of a rocky planet lying in the habitable zone of a main sequence star, Gliese 581 c. Likewise, there is no evidence of extraterrestrial complex life. Although the hypothesis discusses a number of conditions appearing to favor the emergence and development of life under "Earth-like" conditions, the validity of the hypothesis remains open until other Earth-like worlds are found, or the scientific community formally concludes that they are indeed truly rare.
Central to the Rare Earth hypothesis is the following claim about evolutionary biology: while microbes of some sort could well be common in the universe, complex life is unlikely to be. Yet to date, the only evolutionary biologist to speak to the hypothesis at any length is Simon Conway Morris (2003). The hypothesis concludes, more or less, that complex life is rare because it can evolve only on the surface of an Earth-like planet or on a suitable satellite of a planet. Some biologists, such as Jack Cohen, believe this assumption too restrictive and unimaginative; they see it as a form of circular reasoning (see Alternative biochemistry, a speculative biochemistry of alien life forms). Earth-like planets may indeed be very rare, but non carbon-based complex life could possibly emerge in other environments.
According to Darling, the Rare Earth hypothesis is neither hypothesis nor prediction, but merely a description of how life arose on Earth. In his view Ward and Brownlee have done nothing more than select the factors that best suit their case.
There are very many planets. This inevitably will include some Earth-like planets.
Physics and Cosmology
The earth may be rare without being unique. Alternatively planets like Earth may not be rare. Astronomers, Cosmologists and other Physicists also criticize the Rare Earth hypothesis. If the suggestions below are true other places in the universe or multiverse are likely to feature complex life or inevitably feature complex life.
In an infinitely large Multiverse there will be infinitely many copies of the Earth.
Many-Worlds quantum mechanicsThe Many worlds interpretation would yield at least one earth-like planet in some time-lines or worlds. In this context a time line means a world or parallel universe. See Multiverses (Ellis, Koechner and Stoeger sense) This applies even in a universe where the probability of forming even a single one were low.
The Big bang is believed to have roughly started 13.6 billion years ago. The Solar System formed about 4.6 billion years ago. During the 9 billion years between the formation of the Universe and the formation of the Solar System uncountably many copies of the universe developed. The development of at least one Solar System among all these copies of the universe should be expected. Similarly, during the 4.6 billion years ago since the Solar System and the Earth developed, copies of the Earth have been increasing exponentially. It is unsurprising that at least one copy of the Earth developed to form intelligent life.
If the Rare Earth hypothesis, and the Many worlds interpretation are both true, then intelligent observers are guaranteed even if the Rare Earth Equation is close to zero. But, such Earths would almost always be alone, answering the Fermi Paradox. The Rare Earth hypothesis may not be true as explained above.
The Many worlds interpretation alone cannot so easily explain the apparently Fine-tuned universe. In most versions of Many worlds the physical constants of all the “many worlds” are the same.
Other aspects of the Rare Earth hypothesis have come under attack. The hypothesis:
Lack of hard evidence
An advanced species could alter its environment
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Rare_Earth_hypothesis". A list of authors is available in Wikipedia.|