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Circumstellar habitable zone




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Circumstellar habitable zone

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“Goldilocks zone” redirects here. For the planet originally nicknamed “Goldilocks”, see 70 Virginis b. For the more general Goldilocks principle, see Goldilocks principle.
“Habitable zone” redirects here. For the galactic zone, see Galactic habitable zone.
“Comfort zone (astronomy)” redirects here. For other uses, see Comfort zone (disambiguation).

An example of a system based on stellar luminosityfor predicting the location of the habitable zone around various types of stars. Planet sizes, star sizes, orbit lengths, and habitable zone sizes are not to scale.

In astronomy and astrobiology, the circumstellar habitable zone (CHZ), or simply the habitable zone, is the range of orbits around a star within which a planetary surfacecan support liquid water given sufficient atmospheric pressure.[1][2] The bounds of the CHZ are based on Earth‘s position in the Solar System and the amount of radiant energyit receives from the Sun. Due to the importance of liquid water to Earth’s biosphere, the nature of the CHZ and the objects within it may be instrumental in determining the scope and distribution of Earth-like extraterrestrial life and intelligence.

The habitable zone is also called the Goldilocks zone, a metaphor of the children’s fairy tale of “Goldilocks and the Three Bears“, in which a little girl chooses from sets of three items, ignoring the ones that are too extreme (large or small, hot or cold, etc.), and settling on the one in the middle, which is “just right”.

Since the concept was first presented in 1953,[3] many stars have been confirmed to possess a CHZ planet, including some systems that consist of multiple CHZ planets.[4]Most such planets, being super-Earths or gas giants, are more massive than Earth, because such planets are easier to detect. On November 4, 2013, astronomers reported, based on Kepler data, that there could be as many as 40 billion Earth-sizedplanets orbiting in the habitable zones of Sun-like stars and red dwarfs in the Milky Way.[5][6] 11 billion of these may be orbiting Sun-like stars.[7]Proxima Centauri b, located about 4.2 light-years (1.3 parsecs) from Earth in the constellation of Centaurus, is the nearest known exoplanet, and is orbiting in the habitable zone of its star. The CHZ is also of particular interest to the emerging field of habitability of natural satellites, because planetary-mass moons in the CHZ might outnumber planets.[8]

In subsequent decades, the CHZ concept began to be challenged as a primary criterion for life, so the concept is still evolving.[9] Since the discovery of evidence for extraterrestrial liquid water, substantial quantities of it are now thought to occur outside the circumstellar habitable zone. The concept of deep biospheres, like Earth’s, that exist independently of stellar energy, are now generally accepted in astrobiology given the large amount of liquid water known to exist within in lithospheres and asthenospheres of the Solar System.[10] Sustained by other energy sources, such as tidal heating[11][12] or radioactive decay[13] or pressurized by non-atmospheric means, liquid water may be found even on rogue planets, or their moons.[14] Liquid water can also exist at a wider range of temperatures and pressures as a solution, for example with sodium chlorides in seawater on Earth, chlorides and sulphates on equatorial Mars,[15] or ammoniates,[16] due to its different colligative properties. In addition, other circumstellar zones, where non-water solvents favorable to hypothetical life based on alternative biochemistries could exist in liquid form at the surface, have been proposed.[17]


The concept of a circumstellar habitable zone was first introduced in 1953 by Hubertus Strughold, who in his treatise The Green and the Red Planet: A Physiological Study of the Possibility of Life on Mars coined the term “ecosphere” and referred to various “zones” in which life could emerge.[3][18] In the same year, Harlow Shapley wrote “Liquid Water Belt”, which described the same theory in further scientific detail. Both works stressed the importance of liquid water to life.[19]Su-Shu Huang, an American astrophysicist, first introduced the term “habitable zone” in 1959 to refer to the area around a star where liquid water could exist on a sufficiently large body, and was the first to introduce it in the context of planetary habitability and extraterrestrial life.[20][21] A major early contributor to habitable zone theory, Huang argued in 1960 that circumstellar habitable zones, and by extension extraterrestrial life, would be uncommon in multiple star systems, given the gravitational instabilities of those systems.[22]

The theory of habitable zones was further developed in 1964 by Stephen H. Dole in his book Habitable Planets for Man, in which he covered the circumstellar habitable zone itself as well as various other determinants of planetary habitability, eventually estimating the number of habitable planets in the Milky Way to be about 600 million.[23] At the same time, science-fiction author Isaac Asimov introduced the concept of a circumstellar habitable zone to the general public through his various explorations of space colonization.[24] The term “Goldilocks zone” emerged in the 1970s, referencing specifically a region around a star whose temperature is “just right” for water to be present in the liquid phase.[25] In 1993, astronomer James Kasting introduced the term “circumstellar habitable zone” to refer more precisely to the region then (and still) known as the habitable zone.[20]

An update to habitable-zone theory came in 2000, when astronomers Peter Ward and Donald Brownlee introduced the idea of the “galactic habitable zone“, which they later developed with Guillermo Gonzalez.[26][27] The galactic habitable zone, defined as the region where life is most likely to emerge in a galaxy, encompasses those regions close enough to a galactic center that stars there are enriched with heavier elements, but not so close that star systems, planetary orbits, and the emergence of life would be frequently disrupted by the intense radiation and enormous gravitational forces commonly found at galactic centers.[26]

Subsequently, some astrobiologists propose that the concept be extended to other solvents, including dihydrogen, sulfuric acid, dinitrogen, formamide, and methane, among others, which would support hypothetical life forms that use an alternative biochemistry.[17] In 2013, further developments in habitable zone theory were made with the proposal of a circumplanetary habitable zone, also known as the “habitable edge”, to encompass the region around a planet where the orbits of natural satellites would not be disrupted, and at the same time tidal heating from the planet would not cause liquid water to boil away.[28]

Determination of the circumstellar habitable zone[edit]

The range of published estimates for the extent of the Sun’s CHZ. The conservative CHZ[23] is indicated by a dark-green band crossing the inner edge of the aphelion of Venus, whereas an extended CHZ,[29] extending to the orbit of the dwarf planetCeres, is indicated by a light-green band.

Whether a body is in the circumstellar habitable zone of its host star is dependent on the radius of the planet’s orbit (for natural satellites, the host planet’s orbit), the mass of the body itself, and the radiative flux of the host star. Given the large spread in the masses of planets within a circumstellar habitable zone, coupled with the discovery of super-Earth planets which can sustain thicker atmospheres and stronger magnetic fields than Earth, circumstellar habitable zones are now split into two separate regions—a “conservative habitable zone” in which lower-mass planets like Earth or Venus can remain habitable, complemented by a larger “extended habitable zone” in which super-Earth planets, with stronger greenhouse effects, can have the right temperature for liquid water to exist at the surface.[30]

The inner edge of the HZ is the distance where runaway greenhouse effect vaporize the whole water reservoir and,[9] as a second effect, induce the photodissociation of water vapor and the loss of hydrogen to space. The outer edge of the HZ is the distance from the star where adding more carbon dioxide to the atmosphere fails to keep the surface of the planet above the freezing point.[9]

Solar System estimates[edit]

Estimates for the habitable zone within the Solar System range from 0.5 to 3.0 astronomical units,[31] though arriving at these estimates has been challenging for a variety of reasons. Numerous planetary mass objects orbit within, or close to, this range and as such receive sufficient sunlight to raise temperatures above the freezing point of water. However their atmospheric conditions vary substantially. The aphelion of Venus, for example, touches the inner edge of the zone and while atmospheric pressure at the surface is sufficient for liquid water, a strong greenhouse effect raises surface temperatures to 462 °C (864 °F) at which water can only exist as vapour.[32] The entire orbits of the Moon,[33]Mars,[34] and numerous asteroids also lie within various estimates of the habitable zone. Only at Mars’ lowest elevations (less than 30% of the planet’s surface) is atmospheric pressure and temperature sufficient for water to, if present, exist in liquid form for short periods.[35] At Hellas Basin, for example, atmospheric pressures can reach 1,115 Pa and temperatures above zero Celsius (around the triple point for water) for 70 days in the Martian year.[35] Despite indirect evidence in the form of seasonal flows on warm Martian slopes,[36][37][38][39] no confirmation has been made of the presence of liquid water there. While other objects orbit partly within this zone, including comets, Ceres[40] is the only one of planetary mass. A combination of low mass and an inability to mitigate evaporation and atmosphere loss against the solar wind make it impossible for these bodies to sustain liquid water on their surface. Most estimates, therefore, are inferred from the effect that a repositioned orbit would have on the habitability of Earth or Venus.

According to extended habitable zone theory, planetary mass objects with atmospheres capable of inducing sufficient radiative forcing could possess liquid water farther out from the Sun. Such objects could include those whose atmospheres contain a high component of greenhouse gas and terrestrial planets much more massive than Earth (super-Earth class planets), that have retained atmospheres with surface pressures of up to 100 kbar. There are no examples of such objects in the Solar System to study; not enough is known about the nature of atmospheres of these kinds of extrasolar objects, and the net temperature effect of such atmospheres including induced albedo, anti-greenhouse or other possible heat sources cannot be determined by their position in the habitable zone.

Estimates of the circumstellar habitable zone boundaries of the Solar System
Inner edge (AU) Outer edge (AU) Year Notes
0.725 1.24 Dole 1964[23] Used optically thin atmospheres and fixed albedos. Places the aphelion of Venus just inside the zone.
1.385–1.398 Budyko 1969[41] Based on studies of ice albedo feedback models to determine the point at which Earth would experience global glaciation. This estimate was supported in studies by Sellers 1969[42] and North 1975.[43]
0.88–0.912 Rasool and De Bergh 1970[44] Based on studies of Venus’s atmosphere, Rasool and De Bergh concluded that this is the minimum distance at which Earth would have formed stable oceans.
0.95 1.01 Hart et al. 1979[45] Based on computer modelling and simulations of the evolution of Earth’s atmospheric composition and surface temperature. This estimate has often been cited by subsequent publications.
3.0 Fogg 1992[29] Used the carbon cycle to estimate the outer edge of the circumstellar habitable zone.
1.37 Kasting et al. 1993[20] Noted the cooling effect of cloud albedo.
2.0 Spiegel et al. 2010[46] Proposed that seasonal liquid water is possible to this limit when combining high obliquity and orbital eccentricity.
0.75 Abe et al. 2011[47] Found that land-dominated “desert planets” with water at the poles could exist closer to the Sun than watery planets like Earth.
0.77—0.87 1.02—1.18 Vladilo et al. 2013[48] Inner edge of circumstellar habitable zone is closer and outer edge is farther for higher atmospheric pressures; determined minimum atmospheric pressure required to be 15 millibar.
0.99 1.688 Kopparapu et al. 2013[1] Revised estimates using updated runaway greenhouse and water loss algorithms. According to this measure Earth is at the inner edge of the HZ and close to, but just outside, the runaway greenhouse limit. This applies to a planet with Earth-like atmospheric composition and pressure.
0.5 Zsom et al. 2013
Estimate based on various possible combinations of atmospheric composition, pressure and relative humidity of the planet’s atmosphere.

Extrasolar extrapolation[edit]

Astronomers use stellar flux and the inverse-square law to extrapolate circumstellar habitable zone models created for the Solar System to other stars. For example, although the Solar System has a circumstellar habitable zone centered at 1.34 AU from the Sun,[1] a star with 0.25 times the luminosity of the Sun would have a habitable zone centered at {\displaystyle {\sqrt {0.25}}}{\sqrt {0.25}}, or 0.5, the distance from the star, corresponding to a distance of 0.67 AU. Various complicating factors, though, including the individual characteristics of stars themselves, mean that extrasolar extrapolation of the CHZ concept is more complex.

Spectral types and star-system characteristics[edit]

File:Circling Two Suns.ogv

A video explaining the significance of the 2011 discovery of a planet in the circumbinary habitable zone of Kepler-47.

Some scientists argue that the concept of a circumstellar habitable zone is actually limited to stars in certain types of systems or of certain spectral types. Binary systems, for example, have circumstellar habitable zones that differ from those of single-star planetary systems, in addition to the orbital stability concerns inherent with a three-body configuration.[50] If the Solar System were such a binary system, the outer limits of the resulting circumstellar habitable zone could extend as far as 2.4 AU.[51][52]

With regard to spectral types, Zoltán Balog proposes that O-type stars cannot form planets due to the photoevaporation caused by their strong ultraviolet emissions.[53]Studying ultraviolet emissions, Andrea Buccino found that only 40% of stars studied (including the Sun) had overlapping liquid water and ultraviolet habitable zones.[54] Stars smaller than the Sun, on the other hand, have distinct impediments to habitability. Michael Hart, for example, proposed that only main-sequence stars of spectral classK0 or brighter could offer habitable zones, an idea which has evolved in modern times into the concept of a tidal locking radius for red dwarfs. Within this radius, which is coincidental with the red-dwarf habitable zone, it has been suggested that the volcanism caused by tidal heating could cause a “tidal Venus” planet with high temperatures and no hospitable environment to life.[55]

Others maintain that circumstellar habitable zones are more common and that it is indeed possible for water to exist on planets orbiting cooler stars. Climate modelling from 2013 supports the idea that red dwarf stars can support planets with relatively constant temperatures over their surfaces in spite of tidal locking.[56] Astronomy professor Eric Agol argues that even white dwarfs may support a relatively brief habitable zone through planetary migration.[57] At the same time, others have written in similar support of semi-stable, temporary habitable zones around brown dwarfs.[55]

Stellar evolution[edit]

Natural defenses against space weather, such as the magnetosphere depicted in this artistic rendition, may be required for planets to sustain surface water for prolonged periods.

Circumstellar habitable zones change over time with stellar evolution. For example, hot O-type stars, which may remain on the main sequence for fewer than 10 million years,[58] would have rapidly changing habitable zones not conducive to the development of life. Red dwarf stars, on the other hand, which can live for hundreds of billions of years on the main sequence, would have planets with ample time for life to develop and evolve.[59][60] Even while stars are on the main sequence, though, their energy output steadily increases, pushing their habitable zones farther out; our Sun, for example, was 75% as bright in the Archaean as it is now,[61] and in the future, continued increases in energy output will put Earth outside the Sun’s habitable zone, even before it reaches the red giant phase.[62] In order to deal with this increase in luminosity, the concept of a continuously habitable zone has been introduced. As the name suggests, the continuously habitable zone is a region around a star in which planetary-mass bodies can sustain liquid water for a given period of time. Like the general circumstellar habitable zone, the continuously habitable zone of a star is divided into a conservative and extended region.[62]

In red dwarf systems, gigantic stellar flares which could double a star’s brightness in minutes[63] and huge starspots which can cover 20% of the star’s surface area,[64] have the potential to strip an otherwise habitable planet of its atmosphere and water.[65] As with more massive stars, though, stellar evolution changes their nature and energy flux,[66] so by about 1.2 billion years of age, red dwarfs generally become sufficiently constant to allow for the development of life.[65][67]

Once a star has evolved sufficiently to become a red giant, its circumstellar habitable zone will change dramatically from its main-sequence size.[68] For example, the Sun is expected to engulf the previously-habitable Earth as a red giant.[69] However, once a red giant star reaches the horizontal branch, it achieves a new equilibrium and can sustain a new circumstellar habitable zone, which in the case of the Sun would range from 7 to 22 AU.[70] At such stage, Saturn’s moon Titan would likely be habitable in Earth’s temperature sense.[71] Given that this new equilibrium lasts for about 1 Gyr, and because life on Earth emerged by 0.7 Gyr from the formation of the Solar System at latest, life could conceivably develop on planetary mass objects in the habitable zone of red giants.[70] However, around such a helium-burning star, important life processes like photosynthesis could only happen around planets where the atmosphere has been artificially seeded with carbon dioxide, as by the time a solar-mass star becomes a red giant, planetary-mass bodies would have already absorbed much of their free carbon dioxide.[72]

Desert planets[edit]

A planet’s atmospheric conditions influence its ability to retain heat, so that the location of the habitable zone is also specific to each type of planet: desert planets (also known as dry planets), with very little water, will have less water vapor in the atmosphere than Earth and so have a reduced greenhouse effect, meaning that a desert planet could maintain oases of water closer to its star than Earth is to the Sun. The lack of water also means there is less ice to reflect heat into space, so the outer edge of desert-planet habitable zones is further out.[73][74]

Other considerations[edit]

Earth’s hydrosphere. Water covers 71% of Earth’s surface, with the global ocean accounting for 97.3% of the water distribution on Earth.

A planet cannot have a hydrosphere—a key ingredient for the formation of carbon-based life—unless there is a source for water within its stellar system. The origin of water on Earth is still not completely understood; possible sources include the result of impacts with icy bodies, outgassing, mineralization, leakage from hydrous minerals from the lithosphere, and photolysis.[75][76] For an extrasolar system, an icy body from beyond the frost line could migrate into the habitable zone of its star, creating an ocean planet with seas hundreds of kilometers deep[77] such as GJ 1214 b[78][79] or Kepler-22b may be.[80]

Maintenance of liquid surface water also requires a sufficiently thick atmosphere. Possible origins of terrestrial atmospheres are currently theorised to outgassing, impact degassing and ingassing.[81] Atmospheres are thought to be maintained through similar processes along with biogeochemical cycles and the mitigation of atmospheric escape.[82] In a 2013 study led by Italian astronomer Giovanni Vladilo, it was shown that the size of the circumstellar habitable zone increased with greater atmospheric pressure.[48] Below an atmospheric pressure of about 15 millibars, it was found that habitability could not be maintained[48] because even a small shift in pressure or temperature could render water unable to form a liquid.[83]

In the case of planets orbiting in the CHZs of red dwarf stars, the extremely close distances to the stars cause tidal locking, an important factor in habitability. For a tidally locked planet, the sidereal day is as long as the orbital period, causing one side to permanently face the host star and the other side to face away. In the past, such tidal locking was thought to cause extreme heat on the star-facing side and bitter cold on the opposite side, making many red dwarf planets uninhabitable; however, three-dimensional climate models in 2013, showed that the side of a red dwarf planet facing the host star could have extensive cloud cover, increasing its bond albedo and reducing significantly temperature differences between the two sides.[56]

Planetary-mass natural satellites have the potential to be habitable as well. However, these bodies need to fulfill additional parameters, in particular being located within the circumplanetary habitable zones of their host planets.[28] More specifically, moons need to be far enough from their host giant planets that they are not transformed by tidal heating into volcanic worlds like Io,[28] but must still remain within the Hill radius of the planet so that they are not pulled out of orbit of their host planet.[84] Red dwarfs that have masses less than 20% of that of the Sun cannot have habitable moons around giant planets, as the small size of the circumstellar habitable zone would put a habitable moon so close to the star that it would be stripped from its host planet. In such a system, a moon close enough to its host planet to maintain its orbit would have tidal heating so intense as to eliminate any prospects of habitability.[28]

Artist’s concept of a planet on an eccentric orbit that passes through the CHZ for only part of its orbit

A planetary object that orbits a star with high orbital eccentricity may spend only some of its year in the CHZ and experience a large variation in temperature and atmospheric pressure. This would result in dramatic seasonal phase shifts where liquid water may exist only intermittently. It is possible that subsurface habitats could be insulated from such changes and that extremophiles on or near the surface might survive through adaptions such as hibernation (cryptobiosis) and/or hyperthermostability. Tardigrades, for example, can survive in a dehydrated state temperatures between 0.150 K (−273 °C)[85] and 424 K (151 °C).[86] Life on a planetary object orbiting outside CHZ might hibernate on the cold side as the planet approaches the apastron where the planet is coolest and become active on approach to the periastron when the planet is sufficiently warm.[87]

Extrasolar discoveries[edit]

Among exoplanets, a review in 2015 came to the conclusion that Kepler-62f, Kepler-186f and Kepler-442b were likely the best candidates for being potentially habitable.[88] These are at a distance of 1200, 490 and 1,120 light-years away, respectively. Of these, Kepler-186f is similar in size to Earth with a 1.2-Earth-radius measure, and it is located towards the outer edge of the habitable zone around its red dwarf star. Among nearest terrestrial exoplanet candidates, Tau Ceti e is 11.9 light-years away. It is in the inner edge of its solar system’s habitable zone, giving it an estimated average surface temperature of 68 °C (154 °F).[89]

Studies that have attempted to estimate the number of terrestrial planets within the circumstellar habitable zone tend to reflect the availability of scientific data. A 2013 study by Ravi Kumar Kopparapu put ηe, the fraction of stars with planets in the CHZ, at 0.48,[1] meaning that there may be roughly 95–180 billion habitable planets in the Milky Way.[90] However, this is merely a statistical prediction; only a small fraction of these possible planets have yet been discovered.[91]

Previous studies have been more conservative. In 2011, Seth Borenstein concluded that there are roughly 500 million habitable planets in the Milky Way.[92] NASA’s Jet Propulsion Laboratory 2011 study, based on observations from the Kepler mission, raised the number somewhat, estimating that about “1.4 to 2.7 percent” of all stars of spectral class F, G, and K are expected to have planets in their CHZs.[93][94]

Early findings[edit]

The first discoveries of extrasolar planets in the CHZ occurred just a few years after the first extrasolar planets were discovered. One of the first discoveries was 70 Virginis b, a gas giant initially nicknamed “Goldilocks” due to it being neither “too hot” nor “too cold.” Later study revealed temperatures analogous to Venus, ruling out any potential for liquid water.[95]16 Cygni Bb, also discovered in 1996, has an extremely eccentric orbit that causes extreme seasonal effects on the planet’s surface. In spite of this, simulations have suggested that it is possible for a terrestrialnatural satellite to support water at its surface year-round.[96]

Gliese 876 b, discovered in 1998, and Gliese 876 c, discovered in 2001, are both gas giants discovered in the habitable zone around Gliese 876. Although they are not thought to possess significant water at their surfaces, both may have habitable moons.[97]Upsilon Andromedae d, discovered in 1999, is a gas giant in its star’s circumstellar habitable zone considered to be large enough to favor the formation of large, Earth-like moons.[98]

Announced on April 4, 2001, HD 28185 b is a gas giant found to orbit entirely within its star’s circumstellar habitable zone[99] and has a low orbital eccentricity, comparable to that of Mars in the Solar System.[100] Tidal interactions suggest that HD 28185 b could harbor habitable Earth-mass satellites in orbit around it for many billions of years,[101] though it is unclear whether such satellites could form in the first place.[102]

HD 69830 d, a gas giant with 17 times the mass of Earth, was found in 2006 orbiting within the circumstellar habitable zone of HD 69830, 41 light years away from Earth.[103] The following year, 55 Cancri f was discovered within the CHZ of its host star 55 Cancri A.[104][105] Although conditions on this massive and dense planet are not conducive to the formation of water or life as we know it, a hypothetical moon of this planet with the proper mass and composition could be able to support liquid water at its surface.[106]

Habitable super-Earths[edit]

The habitable zone of Gliese 581 compared with our Solar System’s habitable zone.

The 2007 discovery of Gliese 581 c, the first super-Earth in the circumstellar habitable zone, created significant interest in the system by the scientific community, although the planet was later found to have extreme surface conditions that may resemble Venus.[107] Gliese 581 d, another planet in the same system and thought to be a better candidate for habitability, was also announced in 2007. Its existence was later disconfirmed in 2014. Gliese 581 g, yet another planet thought to have been discovered in the circumstellar habitable zone of the system, was considered to be more habitable than both Gliese 581 c and d. However, its existence was also disconfirmed in 2014.[108]

A diagram comparing size (artist’s impression) and orbital position of planet Kepler-22b within Sun-like star Kepler 22’s habitable zone and that of Earth in the Solar System

Discovered in August 2011, HD 85512 b was initially speculated to be habitable,[109] but the new circumstellar-habitable-zone criteria devised by Kopparapu et al. in 2013 place the planet outside the circumstellar habitable zone.[91] With an increase in the frequency of exoplanet discovery, the Earth Similarity Index was devised in October 2011 as a way of comparing planetary properties, such as surface temperature and density, to those of Earth in order to better gauge the habitability of extrasolar bodies.[110]

Kepler-22 b, discovered in December 2011 by the Kepler space probe,[111] is the first transiting exoplanet discovered around a Sun-like star. With a radius 2.4 times that of Earth, Kepler-22b has been predicted by some to be an ocean planet.[112]Gliese 667 Cc, discovered in 2011 but announced in 2012,[113] is a super-Earth orbiting in the circumstellar habitable zone of Gliese 667 C. Subsequently in June 2013, two other habitable super-Earths orbiting the same star, Gliese 667 Cf and Gliese 667 Ce, were discovered in the CHZ.[114]

Gliese 163 c, discovered in September 2012 in orbit around the red dwarf Gliese 163[115] is located 49 light years from Earth. The planet has 6.9 Earth masses and 1.8–2.4 Earth radii, and with its close orbit receives 40 percent more stellar radiation than Earth, leading to surface temperatures of about 60° C.[116][117][118]HD 40307 g, a candidate planet tentatively discovered in November 2012, is in the circumstellar habitable zone of HD 40307.[119] In December 2012, Tau Ceti e and Tau Ceti f were found in the circumstellar habitable zone of Tau Ceti, a Sun-like star 12 light years away.[120] Although more massive than Earth, they are among the least massive planets found to date orbiting in the habitable zone;[121] however, Tau Ceti f, like HD 85512 b, did not fit the new circumstellar habitable zone criteria established by the 2013 Kopparapu study.[122]

Earth-sized planets and Solar analogs[edit]

Comparison of the CHZ position of Earth-radius planet Kepler-186f and the Solar System (17 April 2014)

While larger than Kepler 186f, Kepler-452b’s orbit and star are more similar to Earth’s.

Recent discoveries have uncovered planets that are thought to be similar in size or mass to Earth. While there is no universal definition of “Earth-sized”, ranges are typically defined by mass. The lower range used in many definitions of the super-Earth class is 1.9 Earth masses, likewise, sub-Earths range up to the size of Venus (~0.815 Earth masses). An upper limit of 1.5 Earth radii is also considered, given that above 1.5 R the average planet density rapidly decreases with increasing radius, indicating that these planets have a large fraction of volatiles by volume overlying a rocky core.[123]Solar analogs and solar twins are stars that resemble the Sun. To date no solar twin with an exact match as that of the Sun has been found, however, there are some stars that are nearly identical to the Sun, and are such considered solar twins. An exact solar twin would be a G2V star with a 5,778 K temperature, be 4.6 billion years old, with the correct metallicity and a 0.1% solar luminosity variation.[124] Stars with an age of 4.6 billion years are at the most stable state. Proper metallicity and size are also very important to low luminosity variation.[125][126][127]

On 7 January 2013, astronomers from the Kepler team announced the discovery of Kepler-69c (formerly KOI-172.02), an Earth-size exoplanet candidate (1.7 times the radius of Earth) orbiting Kepler-69, a star similar to our Sun, in the CHZ and expected to offer habitable conditions.[128][129][130][131] The discovery of two planets orbiting in the habitable zone of Kepler-62, by the Kepler team was announced on April 19, 2013. The planets, named Kepler-62e and Kepler-62f, are likely solid planets with sizes 1.6 and 1.4 times the radius of Earth, respectively.[130][131][132]

With a radius estimated at 1.1 Earth, Kepler-186f, discovery announced in April 2014, is the closest yet size to Earth of an exoplanet confirmed by the transit method[133][134][135] though its mass remains unknown and its parent star is not a Solar analog.

On 6 January 2015, NASA announced the 1000th confirmed exoplanet discovered by the Kepler Space Telescope. Three of the newly confirmed exoplanets were found to orbit within habitable zones of their related stars: two of the three, Kepler-438b and Kepler-442b, are near-Earth-size and likely rocky; the third, Kepler-440b, is a super-Earth.[136] Announced 16 January, EPIC 201367065 d is a planet of 1.5 Earth radii found to orbit within the habitable zone of EPIC 201367065, receiving 1.4 times the intensity of visible light as Earth.[137]

Kepler-452b, announced on 23 July 2015 is 50% bigger than Earth, likely rocky and takes approximately 385 Earth days to orbit the habitable zone of its G-class (solar analog) star Kepler-452.[138][139]

The discovery of a system of three tidally-locked planets orbiting the habitable zone of an ultracool dwarf star, TRAPPIST-1, was announced in May 2016.[140] The discovery is considered significant because it greatly increases the possibility of smaller, cooler, more numerous and closer stars possessing habitable planets.

Notable exoplanetsKepler Space Telescope
Confirmed small exoplanets in habitable zones.
(Kepler-62e, Kepler-62f, Kepler-186f, Kepler-296e, Kepler-296f, Kepler-438b, Kepler-440b, Kepler-442b)
(Kepler Space Telescope; January 6, 2015).[136]

Habitability outside the CHZ[edit]

The discovery of hydrocarbon lakes on Saturn’s moon Titan has begun to call into question the carbon chauvinism that underpins CHZ theory.

Liquid-water environments have been found to exist in the absence of atmospheric pressure, and at temperatures outside the CHZ temperature range. For example, Saturn‘s moons Titan and Enceladus and Jupiter‘s moons Europa and Ganymede, all of which are outside the habitable zone, may hold large volumes of liquid water in subsurface oceans.[141]

Outside the CHZ, tidal heating and radioactive decay are two possible heat sources that could contribute to the existence of liquid water.[11][12] Abbot and Switzer (2011) put forward the possibility that subsurface water could exist on rogue planets as a result of radioactive decay-based heating and insulation by a thick surface layer of ice.[14]

With some theorising that life on Earth may have actually originated in stable, subsurface habitats,[142][143] it has been suggested that it may be common for wet subsurface extraterrestrial habitats such as these to ‘teem with life’.[144] Indeed, on Earth itself living organisms may be found more than 6 kilometres below the surface.[145]

Another possibility is that outside the CHZ organisms may use alternative biochemistries that do not require water at all. Astrobiologist Christopher McKay, has suggested that methane (CH
) may be a solvent conducive to the development of “cryolife”, with the Sun’s “methane habitable zone” being centered on 1,610,000,000 km (1.0×109 mi; 11 AU) from the star.[17] This distance is coincidental with the location of Titan, whose lakes and rain of methane make it an ideal location to find McKay’s proposed cryolife.[17] In addition, testing of a number of organisms has found some are capable of surviving in extra-CHZ conditions.[146]

Significance for complex and intelligent life[edit]

The Rare Earth hypothesis argues that complex and intelligent life is uncommon and that the CHZ is one of many critical factors. According to Ward & Brownlee (2004) and others, not only is a CHZ orbit and surface water a primary requirement to sustain life but a requirement to support the secondary conditions required for multicellular life to emerge and evolve. The secondary habitability factors are both geological (the role of surface water in sustaining necessary plate tectonics)[26] and biochemical (the role of radiant energy in supporting photosynthesis for necessary atmospheric oxygenation).[147] But others, such as Ian Stewart and Jack Cohen in their 2002 book Evolving the Alien argue that complex intelligent life may arise outside the CHZ.[148] Intelligent life outside the CHZ may have evolved in subsurface environments, from alternative biochemistries[148] or even from nuclear reactions.[149]

On Earth, several complex multicellular life forms (or eukaryotes) have been identified with the potential to survive conditions that might exist outside the conservative habitable zone. Geothermal energy sustains ancient circumvental ecosystems, supporting large complex life forms such as Riftia pachyptila.[150] Similar environments may be found in oceans pressurised beneath solid crusts, such as those of Europa and Enceladus, outside of the habitable zone.[151]Numerous microorganisms have been tested in simulated conditions and in low Earth orbit, including eukaryotes. An animal example is the Milnesium tardigradum, which can withstand extreme temperatures well above the boiling point of water and the cold vacuum of outer space.[152] In addition, the plants Rhizocarpon geographicum and Xanthoria elegans have been found to survive in an environment where the atmospheric pressure is far too low for surface liquid water and where the radiant energy is also much lower than that which most plants require to photosynthesize.[153][154][155] The fungi Cryomyces antarcticus and Cryomyces minteri are also able to survive and reproduce in Mars-like conditions.[155]

Species, including humans, known to possess animal cognition require large amounts of energy,[156] and have adapted to specific conditions, including an abundance of atmospheric oxygen and the availability of large quantities of chemical energy synthesized from radiant energy. If humans are to colonize other planets, true Earth analogs in the CHZ are most likely to provide the closest natural habitat; this concept was the basis of Stephen H. Dole’s 1964 study. With suitable temperature, gravity, atmospheric pressure and the presence of water, the necessity of spacesuits or space habitat analogues on the surface may be eliminated and complex Earth life can thrive.[23]

Planets in the CHZ remain of paramount interest to researchers looking for intelligent life elsewhere in the universe.[157] The 1961 Drake equation, sometimes used to estimate the number of intelligent civilizations in our galaxy, contains the factor or parameter ηe, which is the fraction of stars that have planetary-mass objects orbiting within the CHZ. A low value lends support to the Rare Earth hypothesis, which posits that intelligent life is a rarity in the Universe, whereas a high value provides evidence for the Copernicanmediocrity principle, the view that habitability—and therefore life—is common throughout the Universe.[26] A 1971 NASA report by Drake and Bernard Oliverproposed the “waterhole“, based on the spectral absorption lines of the hydrogen and hydroxyl components of water, as a good, obvious band for communication with extraterrestrial intelligence[158][159] that has since been widely adopted by astronomers involved in the search for extraterrestrial intelligence. According to Jill Tarter, Margaret Turnbull and many others, CHZ candidates are the priority targets to narrow waterhole searches[160][161] and the Allen Telescope Array now extends Project Phoenix to such candidates.[162]

Because the CHZ is considered the most likely habitat for intelligent life, METI efforts have also been focused on systems likely to have planets there. The 2001 Teen Age Message and the 2003 Cosmic Call 2, for example, were sent to the 47 Ursae Majoris system, known to contain three Jupiter-mass planets and possibly with a terrestrial planet in the CHZ.[163][164][165][166] The Teen Age Message was also directed to the 55 Cancri system, which has a gas giant in its CHZ.[104] A Message from Earth in 2008,[167] and Hello From Earth in 2009, were directed to the Gliese 581 system, containing three planets in the CHZ—Gliese 581 c, d, and the unconfirmed g.

See also[edit]


  1. ^ Jump up to:a b c d Kopparapu, Ravi Kumar (2013). “A revised estimate of the occurrence rate of terrestrial planets in the habitable zones around kepler m-dwarfs”. The Astrophysical Journal Letters. 767 (1): L8. arXiv:1303.2649Freely accessible. Bibcode:2013ApJ…767L…8K. doi:10.1088/2041-8205/767/1/L8.
  2. Jump up^ Cruz, Maria; Coontz, Robert (2013). “Exoplanets – Introduction to Special Issue”. Science. 340 (6132): 565. doi:10.1126/science.340.6132.565. Retrieved 18 May 2013.
  3. ^ Jump up to:a b Huggett, Richard J. (1995). Geoecology: An Evolutionary Approach. Routledge, Chapman & Hall. p. 10. ISBN 978-0-415-08689-9.
  4. Jump up^ Overbye, Dennis (January 6, 2015). “As Ranks of Goldilocks Planets Grow, Astronomers Consider What’s Next”. New York Times. Retrieved January 6, 2015.
  5. Jump up^ Overbye, Dennis (November 4, 2013). “Far-Off Planets Like the Earth Dot the Galaxy”. New York Times. Retrieved November 5, 2013.
  6. Jump up^ Petigura, Eric A.; Howard, Andrew W.; Marcy, Geoffrey W. (October 31, 2013). “Prevalence of Earth-size planets orbiting Sun-like stars”. Proceedings of the National Academy of Sciences of the United States of America. 110: 19273–19278. arXiv:1311.6806Freely accessible. Bibcode:2013PNAS..11019273P. doi:10.1073/pnas.1319909110. Retrieved November 5, 2013.
  7. Jump up^ Khan, Amina (November 4, 2013). “Milky Way may host billions of Earth-size planets”. Los Angeles Times. Retrieved November 5, 2013.
  8. Jump up^ Schirber, Michael (26 Oct 2009). “Detecting Life-Friendly Moons”. Astrobiology Magazine. NASA. Retrieved 9 May 2013.
  9. ^ Jump up to:a b c Lammer, H.; Bredehöft, J. H.; Coustenis, A.; Khodachenko, M. L.; et al. (2009). “What makes a planet habitable?” (PDF). The Astronomy and Astrophysics Review. 17: 181–249. Bibcode:2009A&ARv..17..181L. doi:10.1007/s00159-009-0019-z. Retrieved 2016-05-03.
  10. Jump up^ Edwards, Katrina J.; Becker, Keir; Colwell, Frederick (2012). “The Deep, Dark Energy Biosphere: Intraterrestrial Life on Earth”. Annual Review of Earth and Planetary Sciences. 40 (1): 551–568. Bibcode:2012AREPS..40..551E. doi:10.1146/annurev-earth-042711-105500. ISSN 0084-6597.
  11. ^ Jump up to:a b Cowen, Ron (2008-06-07). “A Shifty Moon”. Science News.
  12. ^ Jump up to:a b Bryner, Jeanna (24 June 2009). “Ocean Hidden Inside Saturn’s Moon”. Space.com. TechMediaNetwork. Retrieved 22 April 2013.
  13. Jump up^ Abbot, D. S.; Switzer, E. R. (2011). “The Steppenwolf: A Proposal for a Habitable Planet in Interstellar Space”. The Astrophysical Journal. 735 (2): L27. arXiv:1102.1108Freely accessible. Bibcode:2011ApJ…735L..27A. doi:10.1088/2041-8205/735/2/L27.
  14. ^ Jump up to:a b “Rogue Planets Could Harbor Life in Interstellar Space, Say Astrobiologists”. MIT Technology Review. MIT Technology Review. 9 February 2011. Retrieved 24 June 2013.
  15. Jump up^ Wall, Mike (28 September 2015). “Salty Water Flows on Mars Today, Boosting Odds for Life”. Space.com. Retrieved 2015-09-28.
  16. Jump up^ Sun, Jiming; Clark, Bryan K.; Torquato, Salvatore; Car, Roberto (2015). “The phase diagram of high-pressure superionic ice”. Nature Communications. 6: 8156. Bibcode:2015NatCo…6E8156S. doi:10.1038/ncomms9156. ISSN 2041-1723.
  17. ^ Jump up to:a b c d Villard, Ray (November 18, 2011). “Alien Life May Live in Various Habitable Zones : Discovery News”. News.discovery.com. Discovery Communications LLC. Retrieved April 22, 2013.
  18. Jump up^ Strughold, Hubertus (1953). The Green and Red Planet: A Physiological Study of the Possibility of Life on Mars. University of New Mexico Press.
  19. Jump up^ Kasting, James (2010). How to Find a Habitable Planet. Princeton University Press. p. 127. ISBN 978-0-691-13805-3. Retrieved 4 May 2013.
  20. ^ Jump up to:a b c Kasting, James F.; Whitmire, Daniel P.; Reynolds, Ray T. (January 1993). “Habitable Zones around Main Sequence Stars”. Icarus. 101 (1): 108–118. Bibcode:1993Icar..101..108K. doi:10.1006/icar.1993.1010. PMID 11536936.
  21. Jump up^ Huang, Su-Shu (1966). Extraterrestrial life: An Anthology and Bibliography. National Research Council (U.S.). Study Group on Biology and the Exploration of Mars. Washington, D. C.: National Academy of Sciences. pp. 87–93.
  22. Jump up^ Huang, Su-Shu (April 1960). “Life-Supporting Regions in the Vicinity of Binary Systems”. Publications of the Astronomical Society of the Pacific. 72(425): 106–114. Bibcode:1960PASP…72..106H. doi:10.1086/127489.
  23. ^ Jump up to:a b c d Dole, Stephen H (1964). Habitable Planets for Man. Blaisdell Publishing Company. p. 103.
  24. Jump up^ Gilster, Paul (2004). Centauri Dreams: Imagining and Planning Interstellar Exploration. Springer. p. 40. ISBN 978-0-387-00436-5.
  25. Jump up^ “The Goldilocks Zone” (Press release). NASA. October 2, 2003. Retrieved April 22, 2013.
  26. ^ Jump up to:a b c d Brownlee, Donald; Ward, Peter (2004). Rare Earth: Why Complex Life Is Uncommon in the Universe. New York: Copernicus. ISBN 0-387-95289-6.
  27. Jump up^ Gonzalez, Guillermo; Brownlee, Donald; Ward, Peter (July 2001). “The Galactic Habitable Zone I. Galactic Chemical Evolution”. Icarus. 152 (1): 185–200. arXiv:astro-ph/0103165Freely accessible. Bibcode:2001Icar..152..185G. doi:10.1006/icar.2001.6617.
  28. ^ Jump up to:a b c d Hadhazy, Adam (April 3, 2013). “The ‘Habitable Edge’ of Exomoons”. Astrobiology Magazine. NASA. Retrieved April 22, 2013.
  29. ^ Jump up to:a b Fogg, M. J. (1992). “An Estimate of the Prevalence of Biocompatible and Habitable Planets”. Journal of the British Interplanetary Society. 45 (1): 3–12. Bibcode:1992JBIS…45….3F. PMID 11539465.
  30. Jump up^ Redd, Nola Taylor (25 August 2011). “Greenhouse Effect Could Extend Habitable Zone”. Astrobiology Magazine. NASA. Retrieved 25 June 2013.
  31. Jump up^ “Stellar habitable zone calculator”. University of Washington. Retrieved 17 December 2015.
  32. Jump up^ “Venus”. Case Western Reserve University. 13 September 2006. Retrieved 2011-12-21.
  33. Jump up^ Sharp, Tim. “Atmosphere of the Moon”. Space.com. TechMediaNetwork. Retrieved April 23, 2013.
  34. Jump up^ Bolonkin, Alexander A. (2009). Artificial Environments on Mars. Berlin Heidelberg: Springer. pp. 599–625. ISBN 978-3-642-03629-3.
  35. ^ Jump up to:a b Haberle, Robert M.; McKay, Christopher P.; Schaeffer, James; Cabrol, Nathalie A.; Grin, Edmon A.; Zent, Aaron P.; Quinn, Richard (2001). “On the possibility of liquid water on present-day Mars”. Journal of Geophysical Research. 106 (E10): 23317. Bibcode:2001JGR…10623317H. doi:10.1029/2000JE001360. ISSN 0148-0227.
  36. Jump up^ Mann, Adam (February 18, 2014). “Strange Dark Streaks on Mars Get More and More Mysterious”. Wired (magazine). Retrieved February 18,2014.
  37. Jump up^ “NASA Finds Possible Signs of Flowing Water on Mars”. voanews.com. Retrieved August 5, 2011.
  38. Jump up^ “Is Mars Weeping Salty Tears?”. news.sciencemag.org. Retrieved August 5, 2011.
  39. Jump up^ Webster, Guy; Brown, Dwayne (December 10, 2013). “NASA Mars Spacecraft Reveals a More Dynamic Red Planet”. NASA. Retrieved December 10, 2013.
  40. Jump up^ A’Hearn, Michael F.; Feldman, Paul D. (1992). “Water vaporization on Ceres”. Icarus. 98 (1): 54–60. Bibcode:1992Icar…98…54A. doi:10.1016/0019-1035(92)90206-M.
  41. Jump up^ Budyko, M. I. (1969). “The effect of solar radiation variations on the climate of the Earth”. Tellus. 21 (5): 611–619. doi:10.1111/j.2153-3490.1969.tb00466.x.
  42. Jump up^ Sellers, William D. (June 1969). “A Global Climatic Model Based on the Energy Balance of the Earth-Atmosphere System”. Journal of Applied Meteorology. 8 (3): 392–400. Bibcode:1969JApMe…8..392S. doi:10.1175/1520-0450(1969)008<0392:AGCMBO>2.0.CO;2.
  43. Jump up^ North, Gerald R. (November 1975). “Theory of Energy-Balance Climate Models”. Journal of the Atmospheric Sciences. 32 (11): 2033–2043. Bibcode:1975JAtS…32.2033N. doi:10.1175/1520-0469(1975)032<2033:TOEBCM>2.0.CO;2.
  44. Jump up^ Rasool, I.; De Bergh, C. (Jun 1970). “The Runaway Greenhouse and the Accumulation of CO2 in the Venus Atmosphere” (PDF). Nature. 226(5250): 1037–1039. Bibcode:1970Natur.226.1037R. doi:10.1038/2261037a0. ISSN 0028-0836. PMID 16057644.
  45. Jump up^ Hart, M. H. (1979). “Habitable zones about main sequence stars”. Icarus. 37: 351–357. Bibcode:1979Icar…37..351H. doi:10.1016/0019-1035(79)90141-6.
  46. Jump up^ Spiegel, D. S.; Raymond, S. N.; Dressing, C. D.; Scharf, C. A.; Mitchell, J. L. (2010). “Generalized Milankovitch Cycles and Long-Term Climatic Habitability”. The Astrophysical Journal. 721 (2): 1308–1318. arXiv:1002.4877Freely accessible. Bibcode:2010ApJ…721.1308S. doi:10.1088/0004-637X/721/2/1308.
  47. Jump up^ Abe, Y.; Abe-Ouchi, A.; Sleep, N. H.; Zahnle, K. J. (2011). “Habitable Zone Limits for Dry Planets”. Astrobiology. 11 (5): 443–460. Bibcode:2011AsBio..11..443A. doi:10.1089/ast.2010.0545. PMID 21707386.
  48. ^ Jump up to:a b c Vladilo, Giovanni; Murante, Giuseppe; Silva, Laura; Provenzale, Antonello; Ferri, Gaia; Ragazzini, Gregorio (March 2013). “The habitable zone of Earth-like planets with different levels of atmospheric pressure”. The Astrophysical Journal. 767 (1): 65–?. arXiv:1302.4566Freely accessible. Bibcode:2013ApJ…767…65V. doi:10.1088/0004-637X/767/1/65.
  49. Jump up^ Zsom, Andras; Seager, Sara; De Wit, Julien (2013). “Towards the Minimum Inner Edge Distance of the Habitable Zone”. arXiv:1304.3714Freely accessible[astro-ph.EP].
  50. Jump up^ Cuntz, Manfred (2013). “S-Type and P-Type Habitability in Stellar Binary Systems: A Comprehensive Approach. I. Method and Applications”. arXiv:1303.6645Freely accessible [astro-ph.EP].
  51. Jump up^ Forget, F.; Pierrehumbert, RT (1997). “Warming Early Mars with Carbon Dioxide Clouds That Scatter Infrared Radiation”. Science. 278 (5341): 1273–6. Bibcode:1997Sci…278.1273F. doi:10.1126/science.278.5341.1273. PMID 9360920.
  52. Jump up^ Mischna, M; Kasting, JF; Pavlov, A; Freedman, R (2000). “Influence of Carbon Dioxide Clouds on Early Martian Climate”. Icarus. 145 (2): 546–54. Bibcode:2000Icar..145..546M. doi:10.1006/icar.2000.6380. PMID 11543507.
  53. Jump up^ Vu, Linda. “Planets Prefer Safe Neighborhoods” (Press release). Spitzer.caltech.edu. NASA/Caltech. Retrieved April 22, 2013.
  54. Jump up^ Buccino, Andrea P.; Lemarchand, Guillermo A.; Mauas, Pablo J.D. (2006). “Ultraviolet radiation constraints around the circumstellar habitable zones”. Icarus. 183 (2): 491–503. arXiv:astro-ph/0512291Freely accessible. Bibcode:2006Icar..183..491B. doi:10.1016/j.icarus.2006.03.007.
  55. ^ Jump up to:a b Barnes, Rory; Heller, René (March 2013). “Habitable Planets Around White and Brown Dwarfs: The Perils of a Cooling Primary”. Astrobiology. 13 (3): 279–291. arXiv:1203.5104Freely accessible. Bibcode:2013AsBio..13..279B. doi:10.1089/ast.2012.0867. PMC 3612282Freely accessible. PMID 23537137.
  56. ^ Jump up to:a b Yang, J.; Cowan, N. B.; Abbot, D. S. (2013). “Stabilizing Cloud Feedback Dramatically Expands the Habitable Zone of Tidally Locked Planets”. The Astrophysical Journal. 771 (2): L45. arXiv:1307.0515Freely accessible. Bibcode:2013ApJ…771L..45Y. doi:10.1088/2041-8205/771/2/L45.
  57. Jump up^ Agol, Eric (April 2011). “Transit Surveys for Earths in the Habitable Zones of White Dwarfs”. The Astrophysical Journal Letters. 731 (2): 1–5. arXiv:1103.2791Freely accessible. Bibcode:2011ApJ…731L..31A. doi:10.1088/2041-8205/731/2/L31.
  58. Jump up^ Carroll, Bradley; Ostlie, Dale (2007). An Introduction to Modern Astrophysics (2 ed.).
  59. Jump up^ Richmond, Michael (November 10, 2004). “Late stages of evolution for low-mass stars”. Rochester Institute of Technology. Retrieved 2007-09-19.
  60. Jump up^ Guo, J.; Zhang, F.; Chen, X.; Han, Z. (2009). “Probability distribution of terrestrial planets in habitable zones around host stars”. Astrophysics and Space Science. 323 (4): 367–373. arXiv:1003.1368Freely accessible. Bibcode:2009Ap&SS.323..367G. doi:10.1007/s10509-009-0081-z.
  61. Jump up^ Kasting, J.F.; Ackerman, T.P. (1986). “Climatic Consequences of Very High Carbon Dioxide Levels in the Earth’s Early Atmosphere”. Science. 234(4782): 1383–1385. doi:10.1126/science.11539665. PMID 11539665.
  62. ^ Jump up to:a b Franck, S.; von Bloh, W.; Bounama, C.; Steffen, M.; Schönberner, D.; Schellnhuber, H.-J. (2002). “Habitable Zones and the Number of Gaia’s Sisters” (PDF). In Montesinos, Benjamin; Giménez, Alvaro; Guinan, Edward F. ASP Conference Series. The Evolving Sun and its Influence on Planetary Environments. Astronomical Society of the Pacific. pp. 261–272. Bibcode:2002ASPC..269..261F. ISBN 1-58381-109-5. Retrieved April 26,2013.
  63. Jump up^ Croswell, Ken (January 27, 2001). “Red, willing and able” (Full reprint). New Scientist. Retrieved August 5, 2007.
  64. Jump up^ Alekseev, I. Y.; Kozlova, O. V. (2002). “Starspots and active regions on the emission red dwarf star LQ Hydrae”. Astronomy and Astrophysics. 396: 203–211. Bibcode:2002A&A…396..203A. doi:10.1051/0004-6361:20021424.
  65. ^ Jump up to:a b Alpert, Mark (November 7, 2005). “Red Star Rising”. Scientific American. Retrieved January 19, 2013.
  66. Jump up^ Research Corporation (December 19, 2006). “Andrew West: ‘Fewer flares, starspots for older dwarf stars'”. EarthSky. Retrieved April 27, 2013.
  67. Jump up^ Cain, Fraser; Gay, Pamela (2007). “AstronomyCast episode 40: American Astronomical Society Meeting, May 2007”. Universe Today. Retrieved 2007-06-17.
  68. Jump up^ Ray Villard (27 July 2009). “Living in a Dying Solar System, Part 1”. Astrobiology. Retrieved 8 April 2016.
  69. Jump up^ Christensen, Bill (April 1, 2005). “Red Giants and Planets to Live On”. Space.com. TechMediaNetwork. Retrieved April 27, 2013.
  70. ^ Jump up to:a b Lopez, B.; Schneider, J.; Danchi, W. C. (2005). “Can Life Develop in the Expanded Habitable Zones around Red Giant Stars?”. The Astrophysical Journal. 627 (2): 974–985. arXiv:astro-ph/0503520Freely accessible. Bibcode:2005ApJ…627..974L. doi:10.1086/430416.
  71. Jump up^ Lorenz, Ralph D.; Lunine, Jonathan I.; McKay, Christopher P. (1997). “Titan under a red giant sun: A new kind of “habitable” moon”. Geophysical Research Letters. 24 (22): 2905–2908. Bibcode:1997GeoRL..24.2905L. doi:10.1029/97GL52843. ISSN 0094-8276. PMID 11542268.
  72. Jump up^ Voisey, Jon (February 23, 2011). “Plausibility Check – Habitable Planets around Red Giants”. Universe Today. Retrieved April 27, 2013.
  73. Jump up^ Alien Life More Likely on ‘Dune’ Planets, 09/01/11, Charles Q. Choi, Astrobiology Magazine
  74. Jump up^ Habitable Zone Limits for Dry Planets, Yutaka Abe, Ayako Abe-Ouchi, Norman H. Sleep, and Kevin J. Zahnle. Astrobiology. June 2011, 11(5): 443–460. doi:10.1089/ast.2010.0545
  75. Jump up^ Drake, Michael J. (April 2005). “Origin of water in the terrestrial planets”. Meteoritics & Planetary Science. John Wiley & Sons. 40 (4): 519–527. Bibcode:2005M&PS…40..519D. doi:10.1111/j.1945-5100.2005.tb00960.x.
  76. Jump up^ Drake, Michael J.; et al. (August 2005). “Origin of water in the terrestrial planets”. Asteroids, Comets, and Meteors (IAU S229). 229th Symposium of the International Astronomical Union. 1. Búzios, Rio de Janeiro, Brazil: Cambridge University Press. pp. 381–394. Bibcode:2006IAUS..229..381D. doi:10.1017/S1743921305006861. ISBN 978-0-521-85200-5.
  77. Jump up^ Kuchner, Marc (2003). “Volatile-rich Earth-Mass Planets in the Habitable Zone”. Astrophysical Journal. 596: L105–L108. arXiv:astro-ph/0303186Freely accessible. Bibcode:2003ApJ…596L.105K. doi:10.1086/378397.
  78. Jump up^ Charbonneau, David; Zachory K. Berta; Jonathan Irwin; Christopher J. Burke; Philip Nutzman; Lars A. Buchhave; Christophe Lovis; Xavier Bonfils; et al. (2009). “A super-Earth transiting a nearby low-mass star”. Nature. 462 (17 December 2009): 891–894. arXiv:0912.3229Freely accessible. Bibcode:2009Natur.462..891C. doi:10.1038/nature08679. PMID 20016595. Retrieved 2009-12-15.
  79. Jump up^ Kuchner, Seager; Hier-Majumder, M.; Militzer, C. A. (2007). “Mass–radius relationships for solid exoplanets”. The Astrophysical Journal. 669 (2): 1279–1297. arXiv:0707.2895Freely accessible. Bibcode:2007ApJ…669.1279S. doi:10.1086/521346.
  80. Jump up^ Vastag, Brian (December 5, 2011). “Newest alien planet is just the right temperature for life”. The Washington Post. Retrieved April 27, 2013.
  81. Jump up^ Robinson, Tyler D.; Catling, David C. (2012). “An Analytic Radiative-Convective Model for Planetary Atmospheres”. The Astrophysical Journal. 757 (1): 104. arXiv:1209.1833Freely accessible. Bibcode:2012ApJ…757..104R. doi:10.1088/0004-637X/757/1/104.
  82. Jump up^ Shizgal, B. D.; Arkos, G. G. (1996). “Nonthermal escape of the atmospheres of Venus, Earth, and Mars”. Reviews of Geophysics. 34 (4): 483–505. Bibcode:1996RvGeo..34..483S. doi:10.1029/96RG02213.
  83. Jump up^ Chaplin, Martin (April 8, 2013). “Water Phase Diagram”. Ices. London South Bank University. Retrieved April 27, 2013.
  84. Jump up^ D.P. Hamilton; J.A. Burns (1992). “Orbital stability zones about asteroids. II – The destabilizing effects of eccentric orbits and of solar radiation”. Icarus. 96 (1): 43–64. Bibcode:1992Icar…96…43H. doi:10.1016/0019-1035(92)90005-R.
  85. Jump up^ Becquerel P. (1950). “La suspension de la vie au dessous de 1/20 K absolu par demagnetization adiabatique de l’alun de fer dans le vide les plus eléve”. C. R. Hebd. Séances Acad. Sci. Paris (in French). 231: 261–263.
  86. Jump up^ Horikawa, Daiki D. (2012). Alexander V. Altenbach, Joan M. Bernhard & Joseph Seckbach, ed. Anoxia Evidence for Eukaryote Survival and Paleontological Strategies. (21 ed.). Springer Netherlands. pp. 205–217. ISBN 978-94-007-1895-1. Retrieved 21 January 2012.
  87. Jump up^ Kane, Stephen R.; Gelino, Dawn M. (2012). “The Habitable Zone and Extreme Planetary Orbits”. Astrobiology. 12 (10): 940–945. arXiv:1205.2429Freely accessible. Bibcode:2012AsBio..12..940K. doi:10.1089/ast.2011.0798. PMID 23035897.
  88. Jump up^ Paul Gilster; Andrew LePage (2015-01-30). “A Review of the Best Habitable Planet Candidates”. Centauri Dreams, Tau Zero Foundation. Retrieved 2015-07-24.
  89. Jump up^ Giovanni F. Bignami (2015). The Mystery of the Seven Spheres: How Homo sapiens will Conquer Space. Springer. ISBN 9783319170046., Page 110
  90. Jump up^ Wethington, Nicholos (September 16, 2008). “How Many Stars are in the Milky Way?”. UniverseToday. Retrieved April 21, 2013.
  91. ^ Jump up to:a b Torres, Abel Mendez (April 26, 2013). “Ten potentially habitable exoplanets now”. Habitable Exoplanets Catalog. University of Puerto Rico. Retrieved April 29, 2013.
  92. Jump up^ Borenstein, Seth (19 February 2011). “Cosmic census finds crowd of planets in our galaxy”. Associated Press. Retrieved 24 April 2011.
  93. Jump up^ Choi, Charles Q. (21 March 2011). “New Estimate for Alien Earths: 2 Billion in Our Galaxy Alone”. Space.com. Retrieved 2011-04-24.
  94. Jump up^ Catanzarite, J.; Shao, M. (2011). “The Occurrence Rate of Earth Analog Planets Orbiting Sun-Like Stars”. The Astrophysical Journal. 738 (2): 151. arXiv:1103.1443Freely accessible. Bibcode:2011ApJ…738..151C. doi:10.1088/0004-637X/738/2/151.
  95. Jump up^ “70 Virginis b”. Extrasolar Planet Guide. Extrasolar.net. Archived from the original on 2012-06-19. Retrieved 2009-04-02.
  96. Jump up^ Williams, D.; Pollard, D. (2002). “Earth-like worlds on eccentric orbits: excursions beyond the habitable zone”. International Journal of Astrobiology. 1 (1): 61–69. Bibcode:2002IJAsB…1…61W. doi:10.1017/S1473550402001064.
  97. Jump up^ Sudarsky, David; et al. (2003). “Theoretical Spectra and Atmospheres of Extrasolar Giant Planets”. The Astrophysical Journal. 588 (2): 1121–1148. arXiv:astro-ph/0210216Freely accessible. Bibcode:2003ApJ…588.1121S. doi:10.1086/374331.
  98. Jump up^ Williams, D.; Pollard, D. (2002). “Earth-like worlds on eccentric orbits: excursions beyond the habitable zone”. International Journal of Astrobiology. Cambridge University Press. 1 (1): 61–69. Bibcode:2002IJAsB…1…61W. doi:10.1017/S1473550402001064.
  99. Jump up^ Jones, B. W.; Sleep, P. N.; Underwood, D. R. (2006). “Habitability of Known Exoplanetary Systems Based on Measured Stellar Properties”. The Astrophysical Journal. 649 (2): 1010–1019. arXiv:astro-ph/0603200Freely accessible. Bibcode:2006ApJ…649.1010J. doi:10.1086/506557.
  100. Jump up^ Butler, R. P.; Wright, J. T.; Marcy, G. W.; Fischer, D. A.; Vogt, S. S.; Tinney, C. G.; Jones, H. R. A.; Carter, B. D.; Johnson, J. A.; McCarthy, C.; Penny, A. J. (2006). “Catalog of Nearby Exoplanets”. The Astrophysical Journal. 646: 505–522. arXiv:astro-ph/0607493Freely accessible. Bibcode:2006ApJ…646..505B. doi:10.1086/504701.
  101. Jump up^ Barnes, J. W.; O’Brien, D. P. (2002). “Stability of Satellites around Close‐in Extrasolar Giant Planets”. The Astrophysical Journal. 575: 1087–1093. arXiv:astro-ph/0205035Freely accessible. Bibcode:2002ApJ…575.1087B. doi:10.1086/341477.
  102. Jump up^ Canup, R. M.; Ward, W. R. (2006). “A common mass scaling for satellite systems of gaseous planets”. Nature. 441 (7095): 834–839. Bibcode:2006Natur.441..834C. doi:10.1038/nature04860. PMID 16778883.
  103. Jump up^ Lovis; et al. (2006). “An extrasolar planetary system with three Neptune-mass planets”. Nature. 441 (7091): 305–309. arXiv:astro-ph/0703024Freely accessible. Bibcode:2006Natur.441..305L. doi:10.1038/nature04828. PMID 16710412.
  104. ^ Jump up to:a b “Astronomers Discover Record Fifth Planet Around Nearby Star 55 Cancri”. Sciencedaily.com. November 6, 2007. Archived from the original on 26 September 2008. Retrieved 2008-09-14.
  105. Jump up^ Fischer, Debra A.; et al. (2008). “Five Planets Orbiting 55 Cancri”. The Astrophysical Journal. 675 (1): 790–801. arXiv:0712.3917Freely accessible. Bibcode:2008ApJ…675..790F. doi:10.1086/525512.
  106. Jump up^ Ian Sample, science correspondent (7 November 2007). “Could this be Earth’s near twin? Introducing planet 55 Cancri f”. London: The Guardian. Archived from the original on 2 October 2008. Retrieved 17 October2008.
  107. Jump up^ Than, Ker (2007-02-24). “Planet Hunters Edge Closer to Their Holy Grail”. space.com. Retrieved 2007-04-29.
  108. Jump up^ Robertson, Paul; Mahadevan, Suvrath; Endl, Michael; Roy, Arpita (3 July 2014). “Stellar activity masquerading as planets in the habitable zone of the M dwarf Gliese 581”. Science. 345: 440–444. arXiv:1407.1049Freely accessible. Bibcode:2014Sci…345..440R. doi:10.1126/science.1253253.
  109. Jump up^ “Researchers find potentially habitable planet” (in French). maxisciences.com. Retrieved 2011-08-31.
  110. Jump up^ Schulze-Makuch, D.; Méndez, A.; Fairén, A. G.; Von Paris, P.; Turse, C.; Boyer, G.; Davila, A. F.; António, M. R. D. S.; Catling, D.; Irwin, L. N. (2011). “A Two-Tiered Approach to Assessing the Habitability of Exoplanets”. Astrobiology. 11 (10): 1041–1052. Bibcode:2011AsBio..11.1041S. doi:10.1089/ast.2010.0592. PMID 22017274.
  111. Jump up^ “Kepler 22-b: Earth-like planet confirmed”. BBC. December 5, 2011. Retrieved May 2, 2013.
  112. Jump up^ Scharf, Caleb A. (2011-12-08). “You Can’t Always Tell an Exoplanet by Its Size”. Scientific American. Retrieved 2012-09-20.: “If it [Kepler-22b] had a similar composition to Earth, then we’re looking at a world in excess of about 40 Earth masses”.
  113. Jump up^ Anglada-Escude, Guillem; Arriagada, Pamela; Vogt, Steven; Rivera, Eugenio J.; Butler, R. Paul; Crane, Jeffrey D.; Shectman, Stephen A.; Thompson, Ian B.; Minniti, Dante (2012). “A planetary system around the nearby M dwarf GJ 667C with at least one super-Earth in its habitable zone”. arXiv:1202.0446Freely accessible [astro-ph.EP].
  114. Jump up^ Anglada-Escudé, Guillem; Tuomi, Mikko; Gerlach, Enrico; Barnes, Rory; Heller, René; Jenkins, James S.; Wende, Sebastian; Vogt, Steven S.; Butler, R. Paul; Reiners, Ansgar; Jones, Hugh R. A. (2013-06-07). “A dynamically-packed planetary system around GJ 667C with three super-Earths in its habitable zone” (PDF). Astronomy & Astrophysics. 556: A126. arXiv:1306.6074Freely accessible. Bibcode:2013A&A…556A.126A. doi:10.1051/0004-6361/201321331. Retrieved 2013-06-25.
  115. Jump up^ Staff (September 20, 2012). “LHS 188 — High proper-motion Star”. Centre de données astronomiques de Strasbourg (Strasbourg astronomical Data Center). Retrieved September 20, 2012.
  116. Jump up^ Méndez, Abel (August 29, 2012). “A Hot Potential Habitable Exoplanet around Gliese 163”. University of Puerto Rico at Arecibo (Planetary Habitability Laboratory). Retrieved September 20, 2012.
  117. Jump up^ Redd (September 20, 2012). “Newfound Alien Planet a Top Contender to Host Life”. Space.com. Retrieved September 20, 2012.
  118. Jump up^ “A Hot Potential Habitable Exoplanet around Gliese 163”. Spacedaily.com. Retrieved 2013-02-10.
  119. Jump up^ Tuomi, Mikko; Anglada-Escude, Guillem; Gerlach, Enrico; Jones, Hugh R. R.; Reiners, Ansgar; Rivera, Eugenio J.; Vogt, Steven S.; Butler, Paul (2012). “Habitable-zone super-Earth candidate in a six-planet system around the K2.5V star HD 40307”. Astronomy and Astrophysics. 549: A48. arXiv:1211.1617Freely accessible. Bibcode:2013A&A…549A..48T. doi:10.1051/0004-6361/201220268.
  120. Jump up^ Aron, Jacob (December 19, 2012). “Nearby Tau Ceti may host two planets suited to life”. New Scientist. Reed Business Information. Retrieved April 1, 2013.
  121. Jump up^ Tuomi, M.; Jones, H. R. A.; Jenkins, J. S.; Tinney, C. G.; Butler, R. P.; Vogt, S. S.; Barnes, J. R.; Wittenmyer, R. A.; o’Toole, S.; Horner, J.; Bailey, J.; Carter, B. D.; Wright, D. J.; Salter, G. S.; Pinfield, D. (2013). “Signals embedded in the radial velocity noise”. Astronomy & Astrophysics. 551: A79. arXiv:1212.4277Freely accessible. Bibcode:2013A&A…551A..79T. doi:10.1051/0004-6361/201220509.
  122. Jump up^ Torres, Abel Mendez (May 1, 2013). “The Habitable Exoplanets Catalog”. Habitable Exoplanets Catalog. University of Puerto Rico. Retrieved May 1, 2013.
  123. Jump up^ Lauren M. Weiss, and Geoffrey W. Marcy. “The mass-radius relation for 65 exoplanets smaller than 4 Earth radii
  124. Jump up^ “Solar Variability and Terrestrial Climate”. NASA Science. 2013-01-08.
  125. Jump up^ “Stellar Luminosity Calculator”. University of Nebraska-Lincoln astronomy education group.
  126. Jump up^ Council, National Research (18 September 2012). “The Effects of Solar Variability on Earth’s Climate: A Workshop Report”. doi:10.17226/13519.
  127. Jump up^ Most of Earth’s twins aren’t identical, or even close!, By Ethan. June 5, 2013.
  128. Jump up^ Moskowitz, Clara (January 9, 2013). “Most Earth-Like Alien Planet Possibly Found”. Space.com. Retrieved January 9, 2013.
  129. Jump up^ Barclay, Thomas; Burke, Christopher J.; Howell, Steve B.; Rowe, Jason F.; Huber, Daniel; Isaacson, Howard; Jenkins, Jon M.; Kolbl, Rea; Marcy, Geoffrey W. (2013). “A Super-Earth-Sized Planet Orbiting in or Near the Habitable Zone Around a Sun-Like Star”. The Astrophysical Journal. 768(2): 101. arXiv:1304.4941Freely accessible. Bibcode:2013ApJ…768..101B. doi:10.1088/0004-637X/768/2/101.
  130. ^ Jump up to:a b Johnson, Michele; Harrington, J.D. (18 April 2013). “NASA’s Kepler Discovers Its Smallest ‘Habitable Zone’ Planets to Date”. NASA. Retrieved 18 April 2013.
  131. ^ Jump up to:a b Overbye, Dennis (18 April 2013). “Two Promising Places to Live, 1,200 Light-Years from Earth”. New York Times. Retrieved 18 April 2013.
  132. Jump up^ Borucki, William J.; et al. (18 April 2013). “Kepler-62: A Five-Planet System with Planets of 1.4 and 1.6 Earth Radii in the Habitable Zone”. Science Express. 340 (6132): 587–90. arXiv:1304.7387Freely accessible. Bibcode:2013Sci…340..587B. doi:10.1126/science.1234702. PMID 23599262. Retrieved 18 April 2013.
  133. Jump up^ Chang, Kenneth (17 April 2014). “Scientists Find an ‘Earth Twin,’ or Maybe a Cousin”. New York Times. Retrieved 17 April 2014.
  134. Jump up^ Chang, Alicia (17 April 2014). “Astronomers spot most Earth-like planet yet”. AP News. Retrieved 17 April 2014.
  135. Jump up^ Morelle, Rebecca (17 April 2014). “‘Most Earth-like planet yet’ spotted by Kepler”. BBC News. Retrieved 17 April 2014.
  136. ^ Jump up to:a b Clavin, Whitney; Chou, Felicia; Johnson, Michele (6 January 2015). “NASA’s Kepler Marks 1,000th Exoplanet Discovery, Uncovers More Small Worlds in Habitable Zones”. NASA. Retrieved 6 January 2015.
  137. Jump up^ Jensen, Mari N. (16 January 2015). “Three nearly Earth-size planets found orbiting nearby star: One in ‘Goldilocks’ zone”. Science Daily. Retrieved 25 July 2015.
  138. Jump up^ Jenkins, Jon M.; Twicken, Joseph D.; Batalha, Natalie M.; Caldwell, Douglas A.; Cochran, William D.; Endl, Michael; Latham, David W.; Esquerdo, Gilbert A.; Seader, Shawn; Bieryla, Allyson; Petigura, Erik; Ciardi, David R.; Marcy, Geoffrey W.; Isaacson, Howard; Huber, Daniel; Rowe, Jason F.; Torres, Guillermo; Bryson, Stephen T.; Buchhave, Lars; Ramirez, Ivan; Wolfgang, Angie; Li, Jie; Campbell, Jennifer R.; Tenenbaum, Peter; Sanderfer, Dwight; Henze, Christopher E.; Catanzarite, Joseph H.; Gilliland, Ronald L.; Borucki, William J. (23 July 2015). “Discovery and Validation of Kepler-452b: A 1.6 R⨁ Super Earth Exoplanet in the Habitable Zone of a G2 Star”. The Astronomical Journal. 150 (2): 56. arXiv:1507.06723Freely accessible. Bibcode:2015AJ….150…56J. doi:10.1088/0004-6256/150/2/56. ISSN 1538-3881. Retrieved 24 July 2015.
  139. Jump up^ “NASA telescope discovers Earth-like planet in star’s habitable zone”. BNO News. 23 July 2015. Retrieved 23 July 2015.
  140. Jump up^ “Three Potentially Habitable Worlds Found Around Nearby Ultracool Dwarf Star”. European Southern Observatory. 2 May 2016.
  141. Jump up^ Torres, Abel (2012-06-12). “Liquid Water in the Solar System”. Retrieved 2013-12-15.
  142. Jump up^ Munro, Margaret (2013), “Miners deep underground in northern Ontario find the oldest water ever known”, National Post, retrieved 2013-10-06
  143. Jump up^ Davies, Paul (2013), The Origin of Life II: How did it begin? (PDF), retrieved 2013-10-06
  144. Jump up^ Taylor, Geoffrey (1996), “Life Underground” (PDF), Planetary Science Research, retrieved 2013-10-06
  145. Jump up^ Doyle, Alister (4 March 2013), “Deep underground, worms and “zombie microbes” rule”, Reuters, retrieved 2013-10-06
  146. Jump up^ Nicholson, W. L.; Moeller, R.; Horneck, G.; PROTECT Team (2012). “Transcriptomic Responses of Germinating Bacillus subtilis Spores Exposed to 1.5 Years of Space and Simulated Martian Conditions on the EXPOSE-E Experiment PROTECT”. Astrobiology. 12 (5): 469–86. Bibcode:2012AsBio..12..469N. doi:10.1089/ast.2011.0748. PMID 22680693.
  147. Jump up^ Decker, Heinz; Holde, Kensal E. (2011). “Oxygen and the Exploration of the Universe (article) (book:Oxygen and the Evolution of Life)”: 157–168. doi:10.1007/978-3-642-13179-0_9. ISBN 978-3-642-13178-3.
  148. ^ Jump up to:a b Stewart, Ian; Cohen, Jack (2002). Evolving the Alien. Ebury Press. ISBN 978-0-09-187927-3.
  149. Jump up^ Goldsmith, Donald; Owen, Tobias (1992). The Search for Life in the Universe (2 ed.). Addison-Wesley. p. 247. ISBN 0-201-56949-3.
  150. Jump up^ Vaclav Smil (2003). The Earth’s Biosphere: Evolution, Dynamics, and Change. MIT Press. p. 166. ISBN 978-0-262-69298-4.
  151. Jump up^ Reynolds, R.T.; McKay, C.P.; Kasting, J.F. (1987). “Europa, Tidally Heated Oceans, and Habitable Zones Around Giant Planets”. Advances in Space Research. 7 (5): 125–132. Bibcode:1987AdSpR…7..125R. doi:10.1016/0273-1177(87)90364-4.
  152. Jump up^ Guidetti, R.; Jönsson, K.I. (2002). “Long-term anhydrobiotic survival in semi-terrestrial micrometazoans”. Journal of Zoology. 257 (2): 181–187. doi:10.1017/S095283690200078X.
  153. Jump up^ Baldwin, Emily (26 April 2012). “Lichen survives harsh Mars environment”. Skymania News. Retrieved 27 April 2012.
  154. Jump up^ de Vera, J.-P.; Kohler, Ulrich (26 April 2012). “The adaptation potential of extremophiles to Martian surface conditions and its implication for the habitability of Mars” (PDF). European Geosciences Union. Retrieved 27 April 2012.
  155. ^ Jump up to:a b Onofri, Silvano; de Vera, Jean-Pierre; Zucconi, Laura; Selbmann, Laura; Scalzi, Giuliano; Venkateswaran, Kasthuri J.; Rabbow, Elke; de la Torre, Rosa; Horneck, Gerda (2015). “Survival of Antarctic Cryptoendolithic Fungi in Simulated Martian Conditions On Board the International Space Station”. Astrobiology. 15 (12): 1052–1059. Bibcode:2015AsBio..15.1052O. doi:10.1089/ast.2015.1324. ISSN 1531-1074.
  156. Jump up^ Isler, K.; van Schaik, C. P (2006). “Metabolic costs of brain size evolution”. Biology Letters. 2 (4): 557–560. doi:10.1098/rsbl.2006.0538. ISSN 1744-9561. PMC 1834002Freely accessible. PMID 17148287.
  157. Jump up^ Palca, Joe (September 29, 2010). “‘Goldilocks’ Planet’s Temperature Just Right For Life”. NPR. NPR. Retrieved April 5, 2011.
  158. Jump up^ “Project Cyclops: A design study of a system for detecting extraterrestrial intelligent life” (PDF). NASA. 1971. Retrieved June 28, 2009.
  159. Jump up^ Joseph A. Angelo (2007). Life in the Universe. Infobase Publishing. p. 163. ISBN 978-1-4381-0892-6. Retrieved 26 June 2013.
  160. Jump up^ Turnbull, Margaret C.; Tarter, Jill C. (2003). “Target Selection for SETI. I. A Catalog of Nearby Habitable Stellar Systems”. The Astrophysical Journal Supplement Series. 145 (1): 181–198. arXiv:astro-ph/0210675Freely accessible. Bibcode:2003ApJS..145..181T. doi:10.1086/345779.
  161. Jump up^ Siemion, Andrew P. V.; Demorest, Paul; Korpela, Eric; Maddalena, Ron J.; Werthimer, Dan; Cobb, Jeff; Howard, Andrew W.; Langston, Glen; Lebofsky, Matt (2013). “A 1.1 to 1.9 GHz SETI Survey of the Kepler Field: I. A Search for Narrow-band Emission from Select Targets”. The Astrophysical Journal. 767 (1): 94. arXiv:1302.0845Freely accessible. Bibcode:2013ApJ…767…94S. doi:10.1088/0004-637X/767/1/94.
  162. Jump up^ Wall, Mike (2011). “HabStars: Speeding Up In the Zone”. Retrieved 2013-06-26
  163. Jump up^ Zaitsev, A. L. (June 2004). “Transmission and reasonable signal searches in the Universe”. Horizons of the Universe Передача и поиски разумных сигналов во Вселенной. Plenary presentation at the National Astronomical Conference WAC-2004 “Horizons of the Universe”, Moscow, Moscow State University, June 7, 2004 (in Russian). Moscow. Retrieved 2013-06-30.
  164. Jump up^ Grinspoon, David (12 December 2007). “Who Speaks for Earth?”. Seedmagazine.com. Retrieved 2012-08-21.
  165. Jump up^ P. C. Gregory; D. A. Fischer (2010). “A Bayesian periodogram finds evidence for three planets in 47 Ursae Majoris”. Monthly Notices of the Royal Astronomical Society. 403 (2): 731–747. arXiv:1003.5549Freely accessible. Bibcode:2010MNRAS.403..731G. doi:10.1111/j.1365-2966.2009.16233.x.
  166. Jump up^ B. Jones; Underwood, David R.; et al. (2005). “Prospects for Habitable “Earths” in Known Exoplanetary Systems”. Astrophysical Journal. 622 (2): 1091–1101. arXiv:astro-ph/0503178Freely accessible. Bibcode:2005ApJ…622.1091J. doi:10.1086/428108.
  167. Jump up^ Moore, Matthew (October 9, 2008). “Messages from Earth sent to distant planet by Bebo”. London: .telegraph.co.uk. Archived from the original on 11 October 2008. Retrieved 2008-10-09.

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About Patrick Ireland

My name is Patrick Ireland, living in the Philippines with my wife and two daughters. I have been studying the web for over a decade. Now that I am 60 years old, I am starting to apply some of the knowledge that I have gained. "Learn from yesterday, live for today, hope for tomorrow. The important thing is to never stop questioning." -Einstein.

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