Life on Mars

For centuries people have speculated about the possibility of life on Mars knowing to the planet's proximity and similarity to Earth. Serious searches for evidence of life began in the 19th century, and continue via telescopic investigations and landed missions. While early work focused on phenomenology and bordered on fantasy, modern scientific inquiry has emphasized the search for water, chemical biosignatures in the soil and rocks at the planet's surface, and the search for biomarker gases in the atmosphere.^[1]

Mars is of particular interest for the study of the origins of life, because of its similarity to the early Earth. This is especially so as Mars has a cold climate and lacks plate tectonics or continental drift, and has remained pretty much unchanged since the end of the Hesperian period. At least two thirds of Mars' surface is more than 3.5 billion years old, and Mars may thus hold the best record of the prebiotic conditions leading to abiogenesis, even if life does not or has never existed there.^[2][3] It remains an open question whether life currently exists on Mars, or has existed there in the past, and fictional Martians have been a recurring feature of popular entertainment of the 20th and 21st centuries.

Contents 1 Early speculation 2 Liquid water 2.1 Silica 3 Habitability 3.1 Past 3.2 Present 3.2.1 Subsurface 3.2.2 Surface brines 3.3 Cosmic radiation 4 Possible biosignatures 4.1 Methane 4.2 Formaldehyde 4.3 Meteorites 4.3.1 ALH84001 4.3.2 Nakhla 4.3.3 Shergotty 5 Geysers on Mars 6 Forward contamination 7 Life under simulated Martian conditions 8 Missions 8.1 Mariner 4 8.2 Viking orbiters 8.3 Viking experiments 8.3.1 Gillevinia straata 8.4 Phoenix lander, 2008 8.5 Mars Science Laboratory 8.6 Future missions 9 See also 10 References 11 External links

Early speculation[edit]

Mars' polar ice caps were observed as early as the mid-17th century, and they were first proven to grow and shrink alternately, in the summer and winter of each hemisphere, by William Herschel in the latter part of the 18th century. By the mid-19th century, astronomers knew that Mars had certain other similarities to Earth, for example that the length of a day on Mars was almost the same as a day on Earth. They also knew that its axial tilt was similar to Earth's, which meant it experienced seasons just as Earth does — but of nearly double the length owing to its much longer year. These observations led to the increase in speculation that the darker albedo features were water, and brighter ones were land. It was therefore natural to suppose that Mars may be inhabited by some form of life.

In 1854, William Whewell, a fellow of Trinity College, Cambridge, who popularized the word scientist, theorized that Mars had seas, land and possibly life forms. Speculation about life on Mars exploded in the late 19th century, following telescopic observation by some observers of apparent Martian canals — which were later found to be optical illusions. Despite this, in 1895, American astronomer Percival Lowell published his book Mars, followed by Mars and its Canals in 1906, proposing that the canals were the work of a long-gone civilization.^[4] This idea led British writer H. G. Wells to write The War of the Worlds in 1897, telling of an invasion by aliens from Mars who were fleeing the planet’s desiccation.

Spectroscopic analysis of Mars' atmosphere began in earnest in 1894, when U.S. astronomer William Wallace Campbell showed that neither water nor oxygen were present in the Martian atmosphere.^[5] By 1909 better telescopes and the best perihelic opposition of Mars since 1877 conclusively put an end to the canal theory.

Liquid water[edit]

No Mars probe since Viking has tested the Martian regolith specifically for metabolism which is the ultimate sign of current life. NASA's recent missions have focused on another question: whether Mars held lakes or oceans of liquid water on its surface in the ancient past. Scientists have found hematite, a mineral that forms in the presence of water. Thus, the mission of the Mars Exploration Rovers of 2004 was not to look for present or past life, but for evidence of liquid water on the surface of Mars in the planet's ancient past.

Liquid water, necessary for Earth life and for metabolism as generally conducted by species on Earth, cannot exist on the surface of Mars under its present low atmospheric pressure and temperature, except at the lowest shaded elevations for short periods^[6][7] and liquid water does not appear at the surface itself.^[8] Liquid water could also form around dust particles in snow heated by the Sun,^[9][10] and there may be ancient equatorial ice sheets beneath the ground that slowly sublimate or melt, accessible from the surface via caves.^{[11][12][13][14]} Also, dust grains embedded in snow may form warm micro-climates when the water around them is briefly melted by the Sun, as has been observed in Antarctica.^[15][16] Some lichens and bacteria in cracks in rocks may also be able to survive solely on the humidity of the air when it briefly condenses on the surface in the morning and evening.^{[17][18][19][20]} In June 2000, evidence for water currently under the surface of Mars was discovered in the form of flood-like gullies.^[21] Deep subsurface water deposits near the planet's liquid core might form a present-day habitat for life. There is also observational evidence which may suggest liquid water forming on or near the surface of Mars seasonally.^[22] However, in March 2006, astronomers announced the discovery of similar gullies on the Moon,^[23] which is believed never to have had liquid water on its surface. The astronomers suggest that the gullies could be the result of micrometeorite impacts.^{[citation needed]}

In March 2004, NASA announced that its rover Opportunity had discovered evidence that Mars was, in the ancient past, a wet planet.^[24] This had raised hopes that evidence of past life might be found on the planet today. ESA confirmed that the Mars Express orbiter had directly detected huge reserves of water ice at Mars' south pole in January 2004.^[25]

On July 28, 2005, ESA announced that they had recorded photographic evidence of surface water ice near Mars' North pole.^[26]

In December 2006, NASA showed images taken by the Mars Global Surveyor that suggested that water occasionally flows on the surface of Mars. The images did not actually show flowing water. Rather, they showed changes in craters and sediment deposits, providing the strongest evidence yet that water coursed through them as recently as several years ago. Some researchers were skeptical that liquid water was responsible for the surface feature changes seen by the spacecraft. They said other materials such as sand or dust can flow like a liquid and produce similar results.^[27]

Recent analysis of Martian sandstones, using data obtained from orbital spectrometry, suggests that the waters that previously existed on the surface of Mars would have had too high a salinity to support most Earth-like life. Tosca et al. found that the Martian water in the locations they studied all had water activity, a_w ≤ 0.78 to 0.86—a level fatal to most Terrestrial life.^[28] Haloarchaea, however, are able to live in hypersaline solutions, up to the saturation point.^[29]

The Phoenix Mars lander from NASA, which landed in the Mars Arctic plain in May 2008, confirmed the presence of frozen water near the surface. This was confirmed when bright material, exposed by the digging arm of the lander, was found to have vaporized and disappeared in 3 to 4 days. This has been attributed to sub-surface ice, exposed by the digging and sublimated on exposure to the atmosphere.^[30]

Silica[edit]

In May 2007, the Spirit rover disturbed a patch of ground with its inoperative wheel, uncovering an area extremely rich in silica (90%).^[31] The feature is reminiscent of the effect of hot spring water or steam coming into contact with volcanic rocks. Scientists consider this as evidence of a past environment that may have been favorable for microbial life, and theorize that one possible origin for the silica may have been produced by the interaction of soil with acid vapors produced by volcanic activity in the presence of water.^[32]

Based on Earth analogs, hydrothermal systems on Mars would be highly attractive for their potential for preserving organic and inorganic biosignatures.^[33][34][35] For example, iron oxidizing bacteria are abundant in marine and terrestrial hydrothermal systems, where they often display distinctive cell morphologies and are commonly encrusted by minerals, especially bacteriogenic iron oxides and silica. Microfossils of iron oxidizing bacteria have been found in ancient Si-Fe deposits and iron oxidation may be an ancient and widespread metabolic pathway.^[33] If possible, future rover missions will target extinct hydrothermal vent systems on Mars.

Habitability[edit]

The two current ecological approaches for predicting the potential habitability of the Martian surface use 19 or 20 environmental factors, with emphasis on water availability, temperature, presence of nutrients, an energy source, and protection from Solar ultraviolet and galactic cosmic radiation.^[36][37]

Some habitability factors[37]
Water	· liquid water activity (aw)  · Past/future liquid (ice) inventories  · Salinity, pH, and Eh of available water
Chemical environment	Nutrients:  · C, H, N, O, P, S, essential metals, essential micronutrients  · Fixed nitrogen  · Availability/mineralogy Toxin abundances and lethality:  · Heavy metals (e.g., Zn, Ni, Cu, Cr, As, Cd, etc., some essential, but toxic at high levels)  · Globally distributed oxidizing soils
Energy for metabolism	Solar (surface and near-surface only) Geochemical (subsurface)  · Oxidants  · Reductants  · Redox gradients
Conducive physical conditions	· Temperature  · Extreme diurnal temperature fluctuations  · Low pressure (Is there a low-pressure threshold for terrestrial anaerobes?)  · Strong ultraviolet germicidal irradiation  · Galactic cosmic radiation and solar particle events (long-term accumulated effects)  · Solar UV-induced volatile oxidants, e.g., O 2–, O–, H2O2, O3  · Climate/variability (geography, seasons, diurnal, and eventually, obliquity variations)  · Substrate (soil processes, rock microenvironments, dust composition, shielding)  · High CO2 concentrations in the global atmosphere  · Transport (aeolian, ground water flow, surface water, glacial)

Past[edit]

When there is a magnetic field, the atmosphere is protected from erosion by solar wind, and ensures the maintenance of a dense atmosphere, necessary for liquid water to exist on the surface of Mars.^[38] Soil and rock samples studied in 2013 by NASA's Curiosity rover onboard instruments, brought about additional information on several habitability factors.^[39] The rover team identified some of the key chemical ingredients for life in this soil, including sulfur, nitrogen, hydrogen, oxygen, phosphorus and possibly carbon, as well as clay minerals, suggesting a long-ago aqueous environment —perhaps a lake or an ancient streambed— that was neutral and not too salty.^[39] The confirmation that liquid water once flowed on Mars, the existence of nutrients, and the previous discovery of a past magnetic field that protected the planet from cosmic and Solar radiation,^[40][41] together strongly suggest that Mars could have had the environmental factors to support life.^[42] To be clear, the find of past habitability is not evidence that Martian life has ever actually existed.

Present[edit]

Subsurface[edit]

Life on the surface of Mars is extremely unlikely because it is bathed in radiation and it is completely frozen.^{[43][44][45][46][47][48]} Therefore, the best potential locations for discovering life on Mars may be at subsurface environments that have not been studied yet.^{[48][49][50][51][52]} The extensive volcanism in the past, possibly created subsurface cracks and caves within different strata, and the liquid water could have been stored in these subterraneous places, forming large aquifers with deposits of saline liquid water, minerals, organic molecules, and geothermal heat – potentially providing a habitable environment away from the harsh surface conditions.^{[48][53][54][55]}

Surface brines[edit]

Although liquid water does not appear at the surface of Mars,^[56][57] several modeling studies suggest that potential locations on Mars could include regions where thin films of salty liquid brine or perchlorate may form near the surface^[57][58][59] that may provide a potential location for terrestrial salt and cold-loving microorganisms (halophile psychrophilic).^[60] Various salts present in the Martian soil acting as an antifreeze could keep water liquid well below its normal freezing point and some researchers estimate that thin films of liquid water could exist in some areas for some of the year (estimates between 2% and 10% of the year. ^[61][62]) Astrobiologists are keen to find out more, as not much is known about these brines at the moment. The briny water may or may not be habitable to microbes from Earth or Mars.^[63] Although chemically important, thin films of transient liquid water are not likely to provide suitable sites for life.^[61] In addition, the activity of water on salty films, the temperature, or both are less than the biological thresholds across the entire Martian surface and shallow subsurface.^[37]

However, the damaging effect of ionising radiation on cellular structure is one of the prime limiting factors on the survival of life in potential astrobiological habitats.^[46][47] Even at a depth of 2 meters beneath the surface, any microbes would likely be dormant, cryopreserved by the current freezing conditions, and so metabolically inactive and unable to repair cellular degradation as it occurs.^[47]

Cosmic radiation[edit]

In 1965, the Mariner 4 probe discovered that Mars had no global magnetic field that would protect the planet from potentially life-threatening cosmic radiation and solar radiation; observations made in the late 1990s by the Mars Global Surveyor confirmed this discovery.^[64] Scientists speculate that the lack of magnetic shielding helped the solar wind blow away much of Mars's atmosphere over the course of several billion years.^[65] As a result, the planet has been vulnerable to radiation from space for about 4 billion years.^[66] Even the hardiest cells known could not possibly survive the cosmic radiation near the surface of Mars for that long.^[43] After mapping cosmic radiation levels at various depths on Mars, researchers have concluded that any life within the first several meters of the planet's surface would be killed by lethal doses of cosmic radiation.^[43][44][45] The team calculated that the cumulative damage to DNA and RNA by cosmic radiation would limit retrieving viable dormant cells on Mars to depths greater than 7.5 metres below the planet's surface.^[44]

Even the most radiation-tolerant Earthly bacteria would survive in dormant spore state only 18,000 years at the surface; at 2 meters —the greatest depth at which the ExoMars rover will be capable of reaching— survival time would be 90,000 to half million years, depending on the type of rock. ^[45]

Possible biosignatures[edit]

Methane[edit]

Trace amounts of methane in the atmosphere of Mars were discovered in 2003 and verified in 2004.^{[67][68][69][70][71][72]} As methane is an unstable gas, its presence indicates that there must be an active source on the planet in order to keep such levels in the atmosphere. It is estimated that Mars must produce 270 ton/year of methane,^[73][74] but asteroid impacts account for only 0.8% of the total methane production. Although geologic sources of methane such as serpentinization are possible, the lack of current volcanism, hydrothermal activity or hotspots are not favorable for geologic methane. It has been suggested that the methane was produced by chemical reactions in meteorites, driven by the intense heat during entry through the atmosphere. Although research published in December 2009 ruled out this possibility,^[75][76] research published in 2012 suggest that a source may be organic compounds on meteorites that are converted to methane by ultraviolet radiation.^[77]

The existence of life in the form of microorganisms such as methanogens is among possible, but as yet unproven sources. If microscopic Martian life is producing the methane, it likely resides far below the surface, where it is still warm enough for liquid water to exist.^[49]

Since the 2003 discovery of methane in the atmosphere, some scientists have been designing models and in vitro experiments testing growth of methanogenic bacteria on simulated Martian soil, where all four methanogen strains tested produced substantial levels of methane, even in the presence of 1.0wt% perchlorate salt.^[78] The results reported indicate that the perchlorates discovered by the Phoenix Lander would not rule out the possible presence of methanogens on Mars.^[78][79]

A team led by Levin suggested that both phenomena—methane production and degradation—could be accounted for by an ecology of methane-producing and methane-consuming microorganisms.^[79][80]

In June 2012, scientists reported that measuring the ratio of hydrogen and methane levels on Mars may help determine the likelihood of life on Mars.^[81][82] According to the scientists, "...low H₂/CH₄ ratios (less than approximately 40) indicate that life is likely present and active."^[81] Other scientists have recently reported methods of detecting hydrogen and methane in extraterrestrial atmospheres.^[83][84]

The Curiosity rover, which landed on Mars in August 2012, is able to make measurements that distinguish between different isotopologues of methane;^[85] but even if the mission is to determine that microscopic Martian life is the source of the methane, the life forms likely reside far below the surface, outside of the rover's reach.^[86] The first measurements with the Tunable Laser Spectrometer (TLS) indicated that there is less than 5 ppb of methane at the landing site at the point of the measurement.^{[87][88][89][90]} The Mars Trace Gas Mission orbiter planned to launch in 2016 would further study the methane,^[91][92] as well as its decomposition products such as formaldehyde and methanol.

Formaldehyde[edit]

In February 2005, it was announced that the Planetary Fourier Spectrometer (PFS) on the European Space Agency's Mars Express Orbiter, detected traces of formaldehyde in the atmosphere of Mars. Vittorio Formisano, the director of the PFS, has speculated that the formaldehyde could be the byproduct of the oxidation of methane, and according to him, would provide evidence that Mars is either extremely geologically active, or harbouring colonies of microbial life.^[93][94] NASA scientists consider the preliminary findings well worth a follow-up, but have also rejected the claims of life.^[95][96]

Meteorites[edit]

NASA maintains a catalog of 34 Mars meteorites.^[97] These assets are highly valuable since they are the only physical samples available of Mars. Studies conducted by NASA's Johnson Space Center show that at least three of the meteorites contain potential evidence of past life on Mars, in the form of microscopic structures resembling fossilized bacteria (so-called biomorphs). Although the scientific evidence collected is reliable, its interpretation varies. To date, none of the original lines of scientific evidence for the hypothesis that the biomorphs are of exobiological origin (the so-called biogenic hypothesis) have been either discredited or positively ascribed to non-biological explanations.^[98]

Over the past few decades, seven criteria have been established for the recognition of past life within terrestrial geologic samples. Those criteria are:^[98]

1. Is the geologic context of the sample compatible with past life?
2. Is the age of the sample and its stratigraphic location compatible with possible life?
3. Does the sample contain evidence of cellular morphology and colonies?
4. Is there any evidence of biominerals showing chemical or mineral disequilibria?
5. Is there any evidence of stable isotope patterns unique to biology?
6. Are there any organic biomarkers present?
7. Are the features indigenous to the sample?

For general acceptance of past life in a geologic sample, essentially most or all of these criteria must be met. All seven criteria have not yet been met for any of the Martian samples, but continued investigations are in progress.^[98]

As of 2010, reexaminations of the biomorphs found in the three Martian meteorites are underway with more advanced analytical instruments than previously available.

ALH84001[edit]

The ALH84001 meteorite was found in December 1984 in Antarctica, by members of the ANSMET project; the meteorite weighs 1.93 kilograms (4.3 lb).^[99] The sample was ejected from Mars about 17 million years ago and spent 11,000 years in or on the Antarctic ice sheets. Composition analysis by NASA revealed a kind of magnetite that on Earth, is only found in association with certain microorganisms.^[98] Then, in August 2002, another NASA team led by Thomas-Keptra published a study indicating that 25% of the magnetite in ALH 84001 occurs as small, uniform-sized crystals that, on Earth, is associated only with biologic activity, and that the remainder of the material appears to be normal inorganic magnetite. The extraction technique did not permit determination as to whether the possibly biological magnetite was organized into chains as would be expected. The meteorite displays indication of relatively low temperature secondary mineralization by water and shows evidence of preterrestrial aqueous alteration.^{[clarification needed]} Evidence of polycyclic aromatic hydrocarbons (PAHs) have been identified with the levels increasing away from the surface.

Some structures resembling the mineralized casts of terrestrial bacteria and their appendages (fibrils) or by-products (extracellular polymeric substances) occur in the rims of carbonate globules and preterrestrial aqueous alteration regions.^[100][101] The size and shape of the objects is consistent with Earthly fossilized nanobacteria, but the existence of nanobacteria itself is controversial.

In November 2009, NASA scientists reported after more detailed analyses, that a biogenic explanation is a more viable hypothesis for the origin of the magnetites in the meteorite.^[102][103]

Nakhla[edit]

The Nakhla meteorite fell on Earth on June 28, 1911 on the locality of Nakhla, Alexandria, Egypt.^[104][105]

In 1998, a team from NASA's Johnson Space Center obtained a small sample for analysis. Researchers found preterrestrial aqueous alteration phases and objects^[106] of the size and shape consistent with Earthly fossilized nanobacteria, but the existence of nanobacteria itself is controversial. Analysis with gas chromatography and mass spectrometry (GC-MS) studied its high molecular weight polycyclic aromatic hydrocarbons in 2000, and NASA scientists concluded that as much as 75% of the organic matter in Nakhla "may not be recent terrestrial contamination".^[98][107]

This caused additional interest in this meteorite, so in 2006, NASA managed to obtain an additional and larger sample from the London Natural History Museum. On this second sample, a large dendritic carbon content was observed. When the results and evidence were published on 2006, some independent researchers claimed that the carbon deposits are of biologic origin. However, it was remarked that since carbon is the fourth most abundant element in the Universe, finding it in curious patterns is not indicative or suggestive of biological origin.^[108][109]

Shergotty[edit]

The Shergotty meteorite, a 4 kg Martian meteorite, fell on Earth on Shergotty, India on August 25, 1865 and was retrieved by witnesses almost immediately.^[110] This meteorite is relatively young, calculated to have been formed on Mars only 165 million years ago from volcanic origin. It is composed mostly of pyroxene and thought to have undergone preterrestrial aqueous alteration for several centuries. Certain features in its interior suggest remnants of a biofilm and its associated microbial communities.^[98] Work is in progress on searching for magnetites within alteration phases.

Geysers on Mars[edit]

The seasonal frosting and defrosting of the southern ice cap results in the formation of spider-like radial channels carved on 1 meter thick ice by sunlight. Then, sublimed CO₂ – and probably water –increase pressure in their interior producing geyser-like eruptions of cold fluids often mixed with dark basaltic sand or mud.^{[111][112][113][114]} This process is rapid, observed happening in the space of a few days, weeks or months, a growth rate rather unusual in geology - especially for Mars.

A team of Hungarian scientists proposes that the geysers' most visible features, dark dune spots and spider channels, may be colonies of photosynthetic Martian microorganisms, which over-winter beneath the ice cap, and as the sunlight returns to the pole during early spring, light penetrates the ice, the microorganisms photosynthesize and heat their immediate surroundings. A pocket of liquid water, which would normally evaporate instantly in the thin Martian atmosphere, is trapped around them by the overlying ice. As this ice layer thins, the microorganisms show through grey. When the layer has completely melted, the microorganisms rapidly desiccate and turn black, surrounded by a grey aureole.^{[115][116][117][118]} The Hungarian scientists believe that even a complex sublimation process is insufficient to explain the formation and evolution of the dark dune spots in space and time.^[119][120] Since their discovery, fiction writer Arthur C. Clarke promoted these formations as deserving of study from an astrobiological perspective.^[121]

A multinational European team suggests that if liquid water is present in the spiders' channels during their annual defrost cycle, they might provide a niche where certain microscopic life forms could have retreated and adapted while sheltered from solar radiation.^[122] A British team also considers the possibility that organic matter, microbes, or even simple plants might co-exist with these inorganic formations, especially if the mechanism includes liquid water and a geothermal energy source.^[123] However, they also remark that the majority of geological structures may be accounted for without invoking any organic "life on Mars" hypothesis.^[123] It has been proposed to develop the Mars Geyser Hopper lander to study the geysers up close.^[124][125]

Forward contamination[edit]

Planetary protection of Mars aims to prevent biological contamination of the planet.^[126] A major goal is to preserve the planetary record of natural processes by preventing human-caused microbial introductions, also called forward contamination. There is abundant evidence as to what can happen when organisms from regions on Earth that have been isolated from one another for significant periods of time are introduced into each other's environment. Species that are constrained in one environment can thrive - often out of control - in another environment much to the detriment of the original species that were present. In some ways this problem could be compounded if life forms from one planet were introduced into the totally alien ecology of another world.^[127]

The prime concern of hardware contaminating Mars, derives from incomplete spacecraft sterilization of some hardy terrestrial bacteria (extremophiles) despite best efforts.^[128][37] Hardware includes landers, crashed probes, end of mission disposal of hardware, and hard landing of entry, descent, and landing systems. This has prompted research on radiation-resistant microorganisms including Brevundimonas, Rhodococcus, Pseudomonas genera and Deinococcus radiodurans survival rates under simulated Martian conditions.^[129] Results from one of these this experimental irradiation experiments, combined with previous radiation modeling, indicate that Brevundimonas sp. MV.7 emplaced only 30 cm deep in Martian dust could survive the cosmic radiation for up to 100,000 years before suffering 10⁶ population reduction.^[129] Surprisingly, the diurnal Mars-like cycles in temperature and relative humidity affected the viability of Deinococcus radiodurans cells quite severely.^[130]

Life under simulated Martian conditions[edit]

On 26 April 2012, scientists reported that lichen survived and showed remarkable results on the adaptation capacity of photosynthetic activity within the simulation time of 34 days under Martian conditions in the Mars Simulation Laboratory (MSL) maintained by the German Aerospace Center (DLR).^[131][132] However, the ability to survive in an environment is not the same as the ability to thrive, reproduce and evolve in that same environment, necessitating further study.

Missions[edit]

Mariner 4[edit]

Mariner 4 probe performed the first successful flyby of the planet Mars, returning the first pictures of the Martian surface in 1965. The photographs showed an arid Mars without rivers, oceans, or any signs of life. Further, it revealed that the surface (at least the parts that it photographed) was covered in craters, indicating a lack of plate tectonics and weathering of any kind for the last 4 billion years. The probe also found that Mars has no global magnetic field that would protect the planet from potentially life-threatening cosmic rays. The probe was able to calculate the atmospheric pressure on the planet to be about 0.6 kPa (compared to Earth's 101.3 kPa), meaning that liquid water could not exist on the planet's surface.^[5] After Mariner 4, the search for life on Mars changed to a search for bacteria-like living organisms rather than for multicellular organisms, as the environment was clearly too harsh for these.

Viking orbiters[edit]

Liquid water is necessary for known life and metabolism, so if water was present on Mars, the chances of it having supported life may have been determinant. The Viking orbiters found evidence of possible river valleys in many areas, erosion and, in the southern hemisphere, branched streams.^{[133][134][135]}

Viking experiments[edit]

The primary mission of the Viking probes of the mid-1970s was to carry out experiments designed to detect microorganisms in Martian soil because the favorable conditions for the evolution of multicellular organisms ceased some four billion years ago on Mars.^[136] The tests were formulated to look for microbial life similar to that found on Earth. Of the four experiments, only the Labeled Release (LR) experiment returned a positive result, showing increased ¹⁴CO₂ production on first exposure of soil to water and nutrients. All scientists agree on two points from the Viking missions: that radiolabeled ¹⁴CO₂ was evolved in the Labeled Release experiment, and that the GC-MS detected no organic molecules. However, there are vastly different interpretations of what those results imply.

One of the designers of the Labeled Release experiment, Gilbert Levin, believes his results are a definitive diagnostic for life on Mars.^[5] However, this result is disputed by many scientists, who argue that superoxidant chemicals in the soil could have produced this effect without life being present. An almost general consensus discarded the Labeled Release data as evidence of life, because the gas chromatograph & mass spectrometer, designed to identify natural organic matter, did not detect organic molecules.^[137] The results of the Viking mission concerning life are considered by the general expert community, at best, as inconclusive.^[5][138]

In 2007, during a Seminar of the Geophysical Laboratory of the Carnegie Institution (Washington, D.C., USA), Gilbert Levin's investigation was assessed once more.^[137] Levin still maintains that his original data were correct, as the positive and negative control experiments were in order.^[139] Moreover, Levin's team, on 12 April 2012, reported a statistical speculation, based on old data —reinterpreted mathematically through complexity analysis— of the Labeled Release experiments, that may suggest evidence of "extant microbial life on Mars."^[139][140] Critics counter that the method has not yet been proven effective for differentiating between biological and non-biological processes on Earth so it is premature to draw any conclusions.^[140]

Ronald Paepe, an edaphologist (soil scientist), communicated to the European Geosciences Union Congress that the discovery of the recent detection of silicate minerals on Mars may indicate pedogenesis, or soil development processes, extended over the entire surface of Mars.^[141] Paepe's interpretation views most of Mars surface as active soil, colored red by eons of widespread wearing by water, vegetation and microbial activity.^[141]

A research team from the National Autonomous University of Mexico headed by Rafael Navarro-González, concluded that the equipment (TV-GC-MS) used by the Viking program to search for organic molecules, may not be sensitive enough to detect low levels of organics.^[142] Because of the simplicity of sample handling, TV–GC–MS is still considered the standard method for organic detection on future Mars missions, so Navarro-González suggests that the design of future organic instruments for Mars should include other methods of detection.

Gillevinia straata[edit]

The claim for life on Mars, in the form of Gillevinia straata, is based on old data reinterpreted as sufficient evidence of life, mainly by professors Gilbert Levin,^[137] Rafael Navarro-González^[142] and Ronalds Paepe.^[141] The evidence supporting the existence of Gillevinia straata microorganisms relies on the data collected by the two Mars Viking landers that searched for biosignatures of life, but the analytical results were, officially, inconclusive.^[5]

In 2006, Mario Crocco, a neurobiologist at the Neuropsychiatric Hospital Borda in Buenos Aires, Argentina, proposed the creation of a new nomenclatural rank that classified the Viking landers' results as 'metabolic' and therefore belonging to a form of life. Crocco proposed to create new biological ranking categories (taxa), in the new kingdom system of life, in order to be able to accommodate the genus of Martian microorganisms. Crocco proposed the following taxonomical entry:^[143]

• Organic life system: Solaria
• Biosphere: Marciana
• Kingdom: Jakobia (named after neurobiologist Christfried Jakob)
• Genus et species: Gillevinia straata

As a result, the hypothetical Gillevinia straata would not be a bacterium (which rather is a terrestrial taxon), but a member of the kingdom 'Jakobia' in the biosphere 'Marciana' of the 'Solaria' system. The intended effect of the new nomenclature was to reverse the burden of proof concerning the life issue, but the taxonomy proposed by Crocco has not been accepted by the scientific community and is considered a single nomen nudum. Further, no Mars mission has found traces of biomolecules.

Phoenix lander, 2008[edit]

The Phoenix mission landed a robotic spacecraft in the polar region of Mars on May 25, 2008 and it operated until November 10, 2008. One of the mission's two primary objectives was to search for a "habitable zone" in the Martian regolith where microbial life could exist, the other main goal being to study the geological history of water on Mars. The lander has a 2.5 meter robotic arm that was capable of digging shallow trenches in the regolith. There was an electrochemistry experiment which analysed the ions in the regolith and the amount and type of antioxidants on Mars. The Viking program data indicate that oxidants on Mars may vary with latitude, noting that Viking 2 saw fewer oxidants than Viking 1 in its more northerly position. Phoenix landed further north still.^[144] Phoenix's preliminary data revealed that Mars soil contains perchlorate, and thus may not be as life-friendly as thought earlier.^{[145][146][147]} The pH and salinity level were viewed as benign from the standpoint of biology. The analysers also indicated the presence of bound water and CO₂.^[148]

Mars Science Laboratory[edit]

The Mars Science Laboratory mission is a NASA project that launched on November 26, 2011 the Curiosity rover, a nuclear-powered robotic vehicle, bearing instruments designed to assess past and present habitability conditions on Mars.^[149][150] The Curiosity rover landed on Mars on Aeolis Palus in Gale Crater, near Aeolis Mons (a.k.a.Mount Sharp),^{[151][152][153][154]} on August 6, 2012.^{[155][156][157]}

Future missions[edit]

• ExoMars is a European-led multi-spacecraft programme currently under development by the European Space Agency (ESA) and the Russian Federal Space Agency for launch in 2016 and 2018.^[158] Its primary scientific mission will be to search for possible biosignatures on Mars, past or present. A rover with a 2 metres (6.6 ft) core drill will be used to sample various depths beneath the surface where liquid water may be found and where microorganisms might survive cosmic radiation.^[42]

• Mars Sample Return Mission — The best life detection experiment proposed is the examination on Earth of a soil sample from Mars. However, the difficulty of providing and maintaining life support over the months of transit from Mars to Earth remains to be solved. Providing for still unknown environmental and nutritional requirements is daunting. Should dead organisms be found in a sample, it would be difficult to conclude that those organisms were alive when obtained.

See also[edit]

• Astrobiology
• Astronomy on Mars
• Colonization of Mars
• Extraterrestrial life
• List of artificial objects on Mars
• List of rocks on Mars
• Planetary habitability
• Seasonal flows on warm Martian slopes
• Space medicine
• Terraforming

References[edit]

External links[edit]

• Study Reveals Young Mars Was A Wet World
• NASA - The Mars Exploration Program
• Scientists have discovered that Mars once had saltwater oceans
• BBC News: Ammonia on Mars could mean life
• Scientist says that life on Mars is likely today
• Ancient salty sea on Mars wins as the most important scientific achievement of 2004 - Journal Science
• Mars meteor found on Earth provides evidence that suggests microbial life once existed on Mars
• Scientific American Magazine (November 2005 Issue) Did Life Come from Another World?
• Audio interview about "Dark Dune Spots"

v t e Mars Geography Atmosphere Climate Dust devil tracks Methane MGCM Seasonal Changes Regions Arabia Terra Cerberus Hemisphere Cydonia Eridania Lake Iani Chaos Olympia Undae Planum Australe Planum Boreum Quadrangles Tempe Terra Terra Cimmeria Tharsis Undae Ultimi Scopuli Vastitas Borealis Quadrangles Aeolis Amazonis Amenthes Arabia Arcadia Argyre Casius Cebrenia Coprates Diacria Elysium Eridania Hellas Iapygia Ismenius Lacus Lunae Palus Mare Acidalium Mare Australe (South Pole) Mare Boreum (North Pole) Mare Tyrrhenum Margaritifer Sinus Memnonia Noachis Oxia Palus Phaethontis Phoenicis Lacus Sinus Sabaeus Syrtis Major Tharsis Thaumasia Mountains and volcanoes Aeolis Mons Alba Mons Albor Tholus Anseris Mons Apollinaris Mons Arsia Mons Ascraeus Mons Ausonia Montes Biblis Tholus Centauri Montes Ceraunius Tholus Charitum Montes Echus Montes Elysium Mons Erebus Montes Galaxius Mons Hadriacus Mons Hecates Tholus Jovis Tholus Libya Montes "Mount Sharp" Nereidum Montes Olympus Mons Orcus Patera Pavonis Mons Peneus Patera Phlegra Montes Pityusa Patera Syrtis Major Planum Tartarus Montes Tharsis Tharsis Montes Tharsis Tholus Tholus Tyrrhenus Mons Ulysses Tholus Uranius group Uranius Mons Uranius Tholus Volcanology By height Plains and plateaus Acidalia Planitia Aeolis Palus Amazonis Planitia Arcadia Planitia Argyre Planitia Chryse Planitia Daedalia Planum Elysium Planitia Hellas Planitia Hesperia Planum Icaria Planum Isidis Planitia Lunae Planum Meridiani Planum Planum Australe Planum Boreum Syria Planum Syrtis Major Planum Utopia Planitia Canyons and valleys Aram Chaos Arsia Chasmata Atlantis Chaos Aureum Chaos Candor Chasma Chasma Boreale Coprates Chasma Echus Chasma Eos Chaos Eos Chasma Galaxias Chaos Ganges Chasma Gorgonum Chaos Hebes Chasma Hydaspis Chaos Hydraotes Chaos Iani Chaos Ister Chaos Ius Chasma Juventae Chasma Melas Chasma Ophir Chasma Tithonium Chasma Apsus Ares Arnus Asopus Athabasca Auqakuh Bahram Buvinda Dao Enipeus Frento Harmakhis Hebrus Huo Hsing 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Thira Tikhonravov Timbuktu Tooting Trouvelot Tugaske Tycho Brahe Victoria Virrat Vishniac Wirtz Wislicenus Yuty Zumba Zunil Meteorites On Earth About Balsaltic Breccia NWA 7034 Chassignites Chassigny Kaidun Nakhla Nakhlites Orthopyroxenite/OPX ALH84001 Shergottites Shergotty Category On Mars Opportunity Block Island Heat Shield Mackinac Island Meridiani Planum Oileán Ruaidh Shelter Island Rocks Curiosity Bathurst Inlet Coronation Goulburn Hottah Jake Matijevic Link Rocknest Rocknest 3 Tintina Opportunity Bounce El Capitan Last Chance Sojourner Barnacle Bill Yogi Spirit Adirondack Home Plate Mimi Pot of Gold Viking Big Joe Other Face Monolith Rootless cones Geology Canals (list) Carbonates Chaos terrain Color Composition Concentric crater fill Dark slope streaks Dichotomy Fretted terrain Geysers Glaciers Lobate debris apron North Polar Basin Ocean hypothesis Polar caps Rocks Rootless cones Soil Spherules Surface "Swiss cheese" feature Tharsis bulge Water History Amazonian Hesperian Noachian Observation history Classical albedo features Moons Specific Deimos Features Phobos Features Stickney crater Monolith Common Moons of Mars In fiction Exploration Current and past Artificial objects on Mars Curiosity HiWish program Mars 3 Mars Exploration Rover Mars Express Mars flyby Mars Global Surveyor Mars landing Mars Odyssey Mars Pathfinder Mars Reconnaissance Orbiter Mars rover Mars Science Laboratory (MSL) MSL Timeline Opportunity observed Phobos program Phoenix Sojourner Spirit observed Viking program Viking 1 Viking 2 Proposed Caves of Mars Project Colonization ExoMars FMARS Haughton–Mars Project InSight Inspiration Mars Mangalyaan Manned mission Mars Geyser Hopper Mars One Mars to Stay MAVEN MDRS Phobos Surveyor Terraforming Astronomy Eclipses Solar eclipses on Mars Transits Deimos Phobos Earth Mercury Venus Asteroids Mars-crosser asteroid 2007 WD5 Trojans List 5261 Eureka 1998 VF31 1999 UJ7 2007 NS2 Related Darian calendar Flag of Mars In fiction Life on Mars Mars Institute Mars Society Martian Mythology Timekeeping on Mars Book:Mars Category:Mars Portal:Mars Portal:Solar System

v t e Extraterrestrial life Events and objects ALH84001 Cells in the stratosphere CI1 fossils Murchison meteorite Nakhla meteorite Polonnaruwa meteorite Radio source SHGb02+14a Red rain in Kerala Shergotty meteorite Viking spacecraft biological experiments Yamato 593 meteorite Misidentified signals CTA-102 (misidentified quasar) PSR B1919+21 / LGM-1 (misidentified pulsar) Wow! signal (inconclusive) Extraterrestrial bodies Solar System Europa Mars Titan Venus Extrasolar List of potential habitable exoplanets Gliese 163 c Gliese 581 d Gliese 581 g Gliese 667 Cc HD 40307 g HD 85512 b Kepler-22b Kepler-62e Kepler-62f KOI-1686.01 PH2 b Tau Ceti e Tau Ceti f Planetary habitability Catalog of Nearby Habitable Systems Circumstellar habitable zone Earth analog Earth Similarity Index Extraterrestrial liquid water Galactic habitable zone Habitability of orange dwarf systems Habitability of red dwarf systems Natural satellite habitability Planetary habitability Missions Darwin space mission ExoMars Foton-M3 Living Interplanetary Flight Experiment Mars sample return mission Mars Science Laboratory Communication Active SETI Allen Telescope Array Arecibo message Arecibo Observatory Bracewell probe Communication with Extraterrestrial Intelligence Gauss' Pythagorean right triangle proposal Interstellar communication Lincos (language) Pioneer plaque Project Cyclops Project Ozma Project Phoenix SERENDIP SETI SETI@home setiQuest Voyager Golden Record Waterhole Xenolinguistics Exhibitions The Science of Aliens Hypotheses Ancient astronauts Aurelia and Blue Moon Back-contamination Cosmic pluralism Directed panspermia Drake equation Extraterrestrial hypothesis Fermi paradox Forward-contamination Great Filter Interplanetary contamination Kardashev scale Mediocrity principle Neocatastrophism Panspermia Planetarium hypothesis Rare Earth hypothesis Sentience quotient Zoo hypothesis Related topics Astrobiology Astroecology Biosignature Brookings Report Potential cultural impact of extraterrestrial contact Exotheology Extraterrestrials in fiction Extremophile Hypothetical types of biochemistry Noogenesis Planetary protection San Marino Scale Shermer's Last Law UFO religion Xenoarchaeology

v t e Astrobiology Biochemistry Biosignature Cosmology Ecology Evolutionary biology ExoMars Extremophiles Life on Mars Mars Science Laboratory Microbiology Origin of life Paleontology Planetary habitability Natural satellite habitability Planetary science Solar system formation Terrestrial Planet Finder