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Natural methane on Mars

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to under detection limit (< 0.05 ppbv)) have been reported in various missions and observational studies. The source of methane on Mars and the explanation for the enormous discrepancy in the observed methane concentrations are still unknown and are under study. Whenever methane is detected, it is
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In 2011, NASA scientists reported a comprehensive search using high-resolution infrared spectroscopy from high-altitude Earth ground-based observatories (VLT, Keck-2, NASA-IRTF) for trace species (including methane) on Mars, deriving sensitive upper limits for methane (< 7 ppbv), ethane
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science team suggested the presence of methane in the atmosphere at a concentration of about 10 ppbv. This was confirmed soon after by three ground-based telescope teams, although large differences in the abundances were measured between observations taken in 2003 and 2006. This spatial and temporal
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ratio in the atmosphere (less than approximately 40) may indicate that a large part of atmospheric methane could be attributed to biological activities, but the observed ratios in the lower Martian atmosphere were "approximately 10 times" higher "suggesting that biological processes may not be
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models cannot explain the apparent rapid variability of the methane levels on Mars. Research suggests that the implied methane destruction lifetime is as long as ≈ 4 Earth years and as short as ≈ 0.6 Earth years. This unexplained fast destruction rate also suggests a very active
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found that the volumes of methane released this way are too low to sustain the measured levels of the gas. 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
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Giuranna, Marco; Viscardy, Sébastien; Daerden, Frank; Neary, Lori; Etiope, Giuseppe; Oehler, Dorothy; Formisano, Vittorio; Aronica, Alessandro; Wolkenberg, Paulina; Aoki, Shohei; Cardesín-Moinelo, Alejandro; Julia; Merritt, Donald; Amoroso, Marilena (2019). "Independent confirmation of a methane
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It was initially thought that methane is chemically unstable in an oxidizing atmosphere with UV radiation and so its lifetime in the Martian atmosphere should be about 400 years, but in 2014, it was concluded that the strong methane sinks are not subject to atmospheric oxidation, suggesting an
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rover detected a tenfold increase ('spike') in methane in the atmosphere around it in late 2013 and early 2014. Four measurements taken over two months in this period averaged 7.2 ppbv, implying that Mars is episodically producing or releasing methane from an unknown source. Before and after,
3688:"Methane vanishing on Mars: Danish researchers propose new mechanism as an explanation - An interdisciplinary research group from Aarhus University has proposed a previously overlooked physical-chemical process that can explain the rapid disappearance of methane from Mars' atmosphere" 512:) generation. The long-term ground-based spectroscopic observation did not find these organic molecules in the Martian atmosphere. Given the expected long lifetimes for some of these molecules, emission of biogenic organics seems to be extremely rare or currently non-existent. 3781:
Jensen, Svend J. Knak; Skibsted, Jørgen; Jakobsen, Hans J.; Kate, Inge L. ten; Gunnlaugsson, Haraldur P.; Merrison, Jonathan P.; Finster, Kai; Bak, Ebbe; Iversen, Jens J.; Kondrup, Jens C.; Nørnberg, Per (2014). "A sink for methane on Mars? The answer is blowing in the wind".
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On modern Earth, volcanism is a minor source of methane emission, and it is usually accompanied by sulfur dioxide gases. However, several studies of trace gases in the Martian atmosphere have found no evidence for sulfur dioxide in the Martian atmosphere, which makes
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would suggest that this process is occurring. An analog on Earth suggests that low-temperature production and exhalation of methane from serpentinized rocks may be possible on Mars. Another possible geophysical source could be ancient methane trapped in
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readings averaged around one-tenth that level. On 7 June 2018, NASA announced the confirmation of a cyclical seasonal variation in the background level of atmospheric methane. The largest concentration of methane detected
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Research at the University of Arkansas published in 2015 suggested that some methanogens could survive on Mars' low pressure in an environment similar to a subsurface liquid aquifer on Mars. The four species tested were
812: 391:, which is known to be common on Mars. The required conditions for this reaction (i.e. high temperature and pressure) do not exist on the surface but may exist within the crust. Detection of the mineral by-product 700:) as their carbon source, so they could exist in subsurface environments on Mars. If microscopic Martian life is producing the methane, it probably resides far below the surface, where it is still warm enough for 161:(UV) radiation from the Sun and chemical reactions with other gases. Therefore, a persistent or episodic presence of methane in the atmosphere may imply the existence of a source to continually replenish the gas. 2639:
Etiope, Giuseppe; Ehlmannc, Bethany L.; Schoell, Martin (2013). "Low temperature production and exhalation of methane from serpentinized rocks on Earth: A potential analog for methane production on Mars".
451:. The discharges from the electrification of dust particles from sand storms and dust devils in contact with permafrost ice may produce about 1.41×10 molecules of methane per joule of applied energy. 2345:"NASA Rover on Mars Detects Puff of Gas That Hints at Possibility of Life - The Curiosity mission's scientists picked up the signal this week, and are seeking additional readings from the red planet" 2910:
Keppler, Frank; Vigano, Ivan; MacLeod, Andy; Ott, Ulrich; Früchtl, Marion; Röckmann, Thomas (Jun 2012). "Ultraviolet-radiation-induced methane emissions from meteorites and the Martian atmosphere".
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Per Nørnberg, Jan Thøgersen, Ebbe Nordskov Bak, Kai Finster, Hans Jørgen Jacobsen, and Svend J. Knak Jensen. Geophysical Research Abstracts. Vol. 21, EGU2019-13986, 2019. EGU General Assembly 2019.
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bonds. The researchers showed that these solids can be oxidized and gases are ionized during the erosion processes. Thus, the ionized methane reacts with the mineral surfaces and bonds to them.
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Keppler, Frank; Vigano, Ivan; McLeod, Andy; Ott, Ulrich; Früchtl, Marion; Röckmann, Thomas (2012). "Ultraviolet-radiation-induced methane emissions from meteorites and the Martian atmosphere".
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Even if rover missions determine that microscopic Martian life is the seasonal source of the methane, the life forms probably reside far below the surface, outside of the rover's reach.
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Vago, Jorge L.; Svedhem, Håkan; Zelenyi, Lev; Etiope, Giuseppe; Wilson, Colin F.; López-Moreno, Jose-Juan; Bellucci, Giancarlo; Patel, Manish R.; Neefs, Eddy (April 2019).
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Vasavada, Ashwin R.; Zurek, Richard W.; Sander, Stanley P.; Crisp, Joy; Lemmon, Mark; Hassler, Donald M.; Genzer, Maria; Harri, Ari-Matti; Smith, Michael D. (2018-06-08).
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methane detection, as well as 24 and 48 hours after the detection, and the TGO was performing atmospheric observations at around the same time but at a higher latitude.
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to measure atmospheric methane, but after entering Mars orbit it was determined that it was not capable of detecting methane, so the instrument was repurposed as an
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Etiope, G.; Fridriksson, T.; Italiano, F.; Winiwarter, W.; Theloke, J. (2007-08-15). "Natural emissions of methane from geothermal and volcanic sources in Europe".
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Levin, Gilbert V.; Straat, Patricia Ann (2009). "Methane and life on Mars". In Hoover, Richard B; Levin, Gilbert V; Rozanov, Alexei Y; Retherford, Kurt D (eds.).
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variability of the gas suggests that the methane was locally concentrated and probably seasonal. It is estimated that Mars produces 270 tons of methane per year.
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suggested that both phenomena—methane production and degradation—could be accounted for by an ecology of methane-producing and methane-consuming microorganisms.
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Yung, Yuk L.; Chen, Pin; Nealson, Kenneth; Atreya, Sushil; Beckett, Patrick; Blank, Jennifer G.; Ehlmann, Bethany; Eiler, John; Etiope, Giuseppe (2018-09-19).
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Webster, C. R.; Mahaffy, P. R.; Atreya, S. K.; Flesch, G. J.; Mischna, M. A.; Meslin, P.-Y.; Farley, K. A.; Conrad, P. G.; Christensen, L. E. (2015-01-23) .
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Thøgersen, Jan; et al. (22 June 2019). "Light on windy nights on Mars: A study of saltation-mediated ionization of argon in a Mars-like atmosphere".
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Krasnopolsky, Vladimir A.; Maillard, Jean Pierre; Owen, Tobias C. (December 2004). "Detection of methane in the martian atmosphere: evidence for life?".
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Court, Richard W.; Sephton, Mark A. (2009). "Investigating the contribution of methane produced by ablating micrometeorites to the atmosphere of Mars".
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If microscopic Martian life is producing the methane, it probably resides far below the surface, where it's still warm enough for liquid water to exist
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bacteria on simulated Martian soil, where all four methanogen strains tested produced substantial levels of methane, even in the presence of 1.0 wt%
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Franck, Lefèvre; Forget, François (6 August 2009). "Observed variations of methane on Mars unexplained by known atmospheric chemistry and physics".
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Lasue, Jeremie; Quesnel, Yoann; Langlais, Benoit; Chassefière, Eric (1 November 2015). "Methane storage capacity of the early martian cryosphere".
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landed on Mars. The rover's instruments are capable of making precise abundance measurements, but cannot be used to distinguish between different
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salt. Methanogens do not require oxygen or organic nutrients, are non-photosynthetic, use hydrogen as their energy source, and carbon dioxide (CO
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Etiope, Giuseppe; Oehler, Dorothy Z. (2019). "Methane spikes, background seasonality and non-detections on Mars: A geological perspective".
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Robledo-Martinez, A.; Sobral, H.; Ruiz-Meza, A. (2012). "Electrical discharges as a possible source of methane on Mars: lab simulation".
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It had also been proposed that the methane might be replenished by meteorites entering the atmosphere of Mars, but researchers from the
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Mumma, M. J.; Villanueva, G. L.; Novak, R. E.; Hewagama, T.; Bonev, B. P.; DiSanti, M. A.; Mandell, A. M.; Smith, M. D. (2009-02-20).
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Krasnopolskya, V. A.; Maillard, J. P.; Owen, T. C. (2004). "Detection of methane in the Martian atmosphere: evidence for life?".
2511:"The Astrobiology of Mars: Methane and Other Candinate Biomarker Gases, and Related Interdisciplinary Studies on Earth and Mars" 5930: 5805: 5545: 5460: 4058: 447:
Lab tests have demonstrated that bursts of methane can be produced when an electrical discharge interacts with water ice and CO
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Thomas, Caroline; et al. (January 2009). "Variability of the methane trapping in Martian subsurface clathrate hydrates".
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Webster, Christopher R.; Mahaffy, Paul R.; Atreya, Sushil K.; Flesch, Gregory J.; Farley, Kenneth A. (19 September 2013).
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Kral, T. A.; Goodhart, T.; Howe, K. L.; Gavin, P. (2009). "Can Methanogens Grow in a Perchlorate Environment on Mars?".
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in the mid-2030s seems the earliest a sample could be analyzed to differentiate a geological from a biological origin.
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A hypothesis postulates that the methane is not consumed at all, but rather condenses and evaporates seasonally from
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Villanueva, G. L.; Mumma, M. J.; Novak, R. E.; Radeva, Y. L.; Käufl, H. U.; Smette, A.; Tokunaga, A.; Khayat, A.;
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efficient physical-chemical process at the surface that "consumes" methane, generically called a "sink".
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Atmospheres in boldface are significant atmospheres; atmospheres in italics are unconfirmed atmospheres.
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Aoki, Shohei; Guiranna, Marco; Kasaba, Yasumasa; Nakagawa, Hiromu; Sindoni, Giuseppe (1 January 2015).
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could trap such methane as clathrates in a stable form at depth, which might exhibit sporadic release.
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Since the 2003 discovery of methane in the atmosphere, some scientists have been designing models and
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located about 500 km east of Gale crater. The region is fractured and is likely volcanic in origin.
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Krasnopolsky, Vladimir A (2012). "Search for methane and upper limits to ethane and SO2 on Mars".
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The principal candidates for the origin of Mars' methane include non-biological processes such as
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of methane and so it cannot determine if it is geophysical or biological in origin. However, the
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Oze, Christopher; Jones, Camille; Goldsmith, Jonas I.; Rosenbauer, Robert J. (7 June 2012).
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Krasnopolsky, Vladimir A. (2006). "Some problems related to the origin of methane on Mars".
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that may be released occasionally. Under the assumption of a cold early Mars environment, a
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2009 ruled out this possibility, research published in 2012 suggested that a source may be
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On Mars, atmospheric methane—a sign of life on Earth—changes mysteriously with the seasons
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Witze, Alexandra (2018-10-25). "Mars scientists edge closer to solving methane mystery".
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Levin, Gilbert V.; Straat, Patricia Ann (3 September 2009). "Methane and life on Mars".
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unlikely to be the source of methane. Although geologic sources of methane such as
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orbiter happened to be performing spot tracking in that area 20 hours before
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in 2012 indicated that there was no methane —or less than 5 ppb— at the
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rapidly removed from the atmosphere by an efficient, yet unknown process.
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with the hydrogen to produce methane is coupled with the generation of an
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rover showed a spike to 21 ppbv, during an event in late June 2019. The
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The first evidence of methane in the atmosphere was measured by ESA's
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Hand, Eric (2018). "Mars methane rises and falls with the seasons".
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rover detected a cyclical seasonal variation in atmospheric methane.
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Instruments and Methods for Astrobiology and Planetary Missions XII
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Webster, Guy; Neal-Jones, Nancy; Brown, Dwayne (16 December 2014).
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Methane Production by Methanogens in Perchlorate-Supplemented Media
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The source of Mars methane is unknown; its detection is shown here.
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Saltation may be contributory in the depletion of methane on Mars.
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and methane levels on Mars may help determine the likelihood of
5198: 5194: 4884: 3874: 3557:"Earth organisms survive under low-pressure Martian conditions" 2123:"NASA Rover Finds Active and Ancient Organic Chemistry on Mars" 4880: 2151:"'A Great Moment': Rover Finds Clue That Mars May Harbor Life" 1678: 1666: 15: 3662:"Martian Methane Reveals the Red Planet is not a Dead Planet" 3587:"Martian Methane Reveals the Red Planet is not a Dead Planet" 1825: 1554:
Is Mars' Methane Spike a Sign of Life? Here's How We'll Know.
976:"Martian Methane Reveals the Red Planet is not a Dead Planet" 879:"Methane on Mars and Habitability: Challenges and Responses" 375:
that could then generate methane and other hydrocarbons via
3215:"Strong Release of Methane on Mars in Northern Summer 2003" 1214:"Strong Release of Methane on Mars in Northern Summer 2003" 2849:"A stringent upper limit to SO2 in the Martian atmosphere" 1004:
Howe, K. L.; Gavin, P.; Goodhart, T.; Kral, T. A. (2009).
258:(TGO) can measure these ratios and point to their origin. 5936:
Astrobiology Science and Technology for Exploring Planets
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Zahnle, Kevin; Freedman, Richard; Catling, David (2010).
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spike on Mars and a source region east of Gale Crater".
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rover may have been released from a nearby area called
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Eigenbrode, Jennifer L.; et al. (8 June 2018).
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Webster, Christopher R.; et al. (8 June 2018).
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Since 2004, trace amounts of methane (range from 60
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(10 February 2009). 2433:"ExoMars official says launch unlikely before 2028" 1549: 1547: 1545: 1543: 1147:; Ignatiev, Nikolai; Giuranna, Marco (2004-12-03). 46:Please help to ensure that disputed statements are 3020:"Life on Mars theory boosted by new methane study" 2966:"Life on Mars theory boosted by new methane study" 2374:India's Mars Orbiter Mission Has a Methane Problem 1839: 1837: 1835: 1716:"First results from the ExoMars Trace Gas Orbiter" 609: 5456:Habitability of F-type main-sequence star systems 5446:Habitability of K-type main-sequence star systems 2964:Court, Richard; Sephton, Mark (8 December 2009). 2317:"Curiosity Detects Unusually High Methane Levels" 2097:"Mars Rover Comes Up Empty in Search for Methane" 2064:"Mars Rover Finds No Evidence of Burps and Farts" 1889:Andrew Good, NASA. Press release on 23 June 2019. 3397: 3395: 3393: 1934:"Curiosity Rover Finds No Methane on Mars — Yet" 1887:Curiosity Detects Unusually High Methane Levels. 1611:"Detection of Methane in the Atmosphere of Mars" 1149:"Detection of Methane in the Atmosphere of Mars" 30:The factual accuracy of part of this article is 5381:Search for extraterrestrial intelligence (SETI) 3528:72nd Annual Meeting of the Meteoritical Society 2476: 2474: 440:on meteorites that are converted to methane by 2768:Journal of Volcanology and Geothermal Research 2392:Mission Mars: India's Quest for the Red Planet 2004:"Low Upper Limit to Methane Abundance on Mars" 1013:. 40th Lunar and Planetary Science Conference. 821:measurements in the atmosphere of Mars by the 5210: 4896: 3886: 3762:. 41st Lunar and Planetary Science Conference 2623:Team Finds New Hope for Life in Martian Crust 2369: 2367: 2315:Good, Andrew; Johnson, Alana (23 June 2019). 459:replenishing source. A team from the Italian 8: 5361:List of microorganisms tested in outer space 2524:. Greenbelt, MD: Goddard Space Flight Center 347:Possible methane sources and sinks on Mars. 5786:Enceladus Life Signatures and Habitability 5490: 5217: 5203: 5195: 4903: 4889: 4881: 4643: 4424: 3923: 3893: 3879: 3871: 463:suspects that the methane detected by the 5973:European Astrobiology Network Association 3551: 3549: 3439: 3429: 2872: 2691: 2568: 2291: 2281: 2230: 1901:"Curiosity Finds Methane on Mars, or Not" 1634: 1375: 1237: 1172: 918: 599: 594: 589: 579: 574: 563: 558: 553: 543: 538: 533: 531: 70:Learn how and when to remove this message 5466:List of potentially habitable exoplanets 2770:. Gas geochemistry and Earth degassing. 1818:"Planetary Fourier Spectrometer website" 133: 81: 5884:Living Interplanetary Flight Experiment 866: 796: 428:is not favorable for geologic methane. 3660:Steigerwald, Bill (January 15, 2009). 3585:Steigerwald, Bill (January 15, 2009). 3088: 3086: 1474: 1472: 1405: 1403: 1279: 1277: 1275: 1273: 999: 997: 952: 170:orbiter with an instrument called the 98:is of interest to many geologists and 50:. See the relevant discussion on the 5874:Biological Oxidant and Life Detection 2899:from the original on October 4, 2013. 1692:from the original on 24 February 2006 1609:; Ignatiev, N.; Giuranna, M. (2004). 1143:Formisano, Vittorio; Atreya, Sushil; 974:Steigerwald, Bill (15 January 2009). 872: 870: 7: 6023: 5451:Habitability of yellow dwarf systems 5436:Habitability of neutron star systems 2518:Astrobiology Science Conference 2010 2509:Mumma, Michael; et al. (2010). 2095:Chang, Kenneth (19 September 2013). 1899:Kerr, Richard A. 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Proceedings of SPIE. 806:Volatile gases on Mars. 660:Measuring the ratio of 433:Imperial College London 5781:Enceladus Life Finder‎ 5761:Breakthrough Enceladus 5285:Planetary oceanography 4484:Solar eclipses on Mars 4343:"Swiss cheese" feature 4199:Concentric crater fill 3561:University of Arkansas 3463:Staff (25 June 2012). 1848:; Hartogh, P. (2013). 1669:Press release (2004). 617:(∆G˚' = -134 kJ/mol CH 611: 348: 240: 147: 87: 5956:Breakthrough Starshot 5556:Lunar Micro Ecosystem 5476:Superhabitable planet 5341:Extraterrestrial life 1824:. ESA. Archived from 1720:European Space Agency 1485:European Space Agency 1481:"The methane mystery" 947:Astrobiology Magazine 903:10.1089/ast.2018.1917 612: 422:hydrothermal activity 346: 235: 174:. In March 2004, the 137: 130:History of detections 116:hydrothermal activity 85: 36:The dispute is about 5963:Carl Sagan Institute 5951:Breakthrough Message 5791:Enceladus Orbilander 5526:Biosatellite program 5376:Planetary protection 5260:Evolutionary biology 5250:Atmospheric sciences 5162:Prebiotic atmosphere 4684:Permanent settlement 3115:10.1029/2012gl053255 2570:10.1029/2005GL022691 2076:on 20 September 2013 530: 304:Mars Orbiter Mission 5946:Breakthrough Listen 4826:Timekeeping on Mars 4503:Planetary transits 4488:Satellite transits 4401:Observation history 4249:Lobate debris apron 3833:2019Icar..332...14T 3796:2014Icar..236...24K 3732:2015Icar..245..177A 3621:2009SPIE.7441E..0DL 3505:2004Icar..172..537K 3422:2012PNAS..109.9750O 3368:2019NatGe..12..326G 3293:10.1038/nature08228 3285:2009Natur.460..720L 3234:2009Sci...323.1041M 3228:(5917): 1041–1045. 3107:2012GeoRL..3917202R 3061:10.1038/nature11203 3053:2012Natur.486...93K 2932:10.1038/nature11203 2924:2012Natur.486...93K 2823:2012Icar..217..144K 2780:2007JVGR..165...76E 2745:2015Icar..260..205L 2654:2013Icar..224..276E 2561:2005GeoRL..3210203O 2390:Lele, Ajey (2014). 2274:2018Sci...360.1096E 2268:(6393): 1096–1101. 2223:2018Sci...360.1093W 2217:(6393): 1093–1096. 2025:2013Sci...342..355W 1866:2013Icar..223...11V 1796:2006Icar..180..359K 1753:2018Sci...359...16H 1687:2004xmm..pres...80. 1627:2004Sci...306.1758F 1621:(5702): 1758–1761. 1584:2004Icar..172..537K 1431:2019Natur.568..517K 1368:2018Sci...360.1093W 1362:(6393): 1093–1096. 1305:2015Sci...347..415W 1230:2009Sci...323.1041M 1224:(5917): 1041–1045. 1165:2004Sci...306.1758F 1159:(5702): 1758–1761. 1106:2018Natur.563...18W 1038:2009SPIE.7441E..0DL 895:2018AsBio..18.1221Y 711:Methanothermobacter 625:This reaction of CO 602: 582: 566: 546: 6051:Atmosphere of Mars 5776:Enceladus Explorer 5177:Stellar atmosphere 5055:Natural satellites 3095:Geophys. 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Archived from 2059: 2053: 2052: 2008: 1999: 1993: 1990:Science Magazine 1983: 1977: 1976: 1974: 1972: 1957: 1951: 1950: 1948: 1946: 1929: 1923: 1922: 1920: 1918: 1909:. Archived from 1896: 1890: 1884: 1878: 1877: 1841: 1830: 1829: 1814: 1808: 1807: 1779: 1773: 1772: 1736: 1730: 1729: 1727: 1726: 1711: 1702: 1701: 1699: 1697: 1663: 1657: 1656: 1638: 1602: 1596: 1595: 1567: 1561: 1551: 1538: 1537: 1501: 1495: 1494: 1492: 1491: 1476: 1467: 1466: 1416: 1407: 1398: 1397: 1379: 1347: 1341: 1340: 1290: 1281: 1268: 1267: 1241: 1209: 1203: 1202: 1176: 1140: 1134: 1133: 1089: 1083: 1082: 1080: 1079: 1064: 1058: 1057: 1021: 1015: 1014: 1012: 1001: 992: 991: 989: 987: 971: 965: 964: 958: 950: 939: 933: 932: 922: 874: 815: 803: 788: 787: 786: 772: 771: 770: 725:Methanobacterium 616: 614: 613: 608: 606: 603: 601: 598: 591: 581: 578: 571: 565: 562: 555: 545: 542: 535: 511: 510: 509: 501: 500: 414:serpentinization 298: 267: 110:process such as 75: 68: 64: 61: 55: 48:reliably sourced 24: 16: 6076: 6075: 6071: 6070: 6069: 6067: 6066: 6065: 6041: 6040: 6039: 6034: 6002: 5923: 5913: 5856: 5850: 5811:Icebreaker Life 5749: 5711: 5695: 5669: 5663: 5580: 5486: 5480: 5397: 5390: 5294: 5270:Geomicrobiology 5228: 5223: 5193: 5188: 5181: 5150: 5116: 5049: 5010: 4943: 4934: 4914: 4909: 4879: 4874: 4864: 4862: 4842: 4836:Darian calendar 4761: 4716: 4698: 4629: 4613: 4597: 4590: 4585: 4580: 4575: 4570: 4565: 4545: 4544: 4541: 4518: 4470: 4464:Voltaire crater 4442:Stickney crater 4410: 4372: 4214:Fretted terrain 4160: 4060: 4053: 4014:Sinus Meridiani 3999:Planum Australe 3974:Cerberus (Mars) 3955: 3913: 3911:Outline of Mars 3904: 3899: 3869: 3868: 3860: 3856: 3816: 3815: 3811: 3780: 3779: 3775: 3765: 3763: 3759: 3752: 3751: 3747: 3713: 3712: 3708: 3698: 3696: 3686:(2 July 2019). 3682: 3681: 3677: 3659: 3658: 3654: 3639: 3610: 3609: 3605: 3584: 3583: 3579: 3570: 3568: 3563:. 2 June 2015. 3555: 3554: 3547: 3525: 3524: 3520: 3490: 3489: 3485: 3475: 3473: 3462: 3461: 3457: 3401: 3400: 3391: 3352: 3351: 3347: 3337: 3335: 3321: 3320: 3316: 3270: 3269: 3265: 3217: 3212: 3211: 3207: 3197: 3195: 3186: 3185: 3181: 3171: 3169: 3160: 3159: 3155: 3146: 3144: 3135: 3134: 3130: 3092: 3091: 3084: 3038: 3037: 3033: 3018: 2989: 2988: 2984: 2974: 2972: 2963: 2962: 2958: 2909: 2908: 2904: 2887: 2886: 2882: 2843: 2842: 2838: 2808: 2807: 2803: 2765: 2764: 2760: 2730: 2729: 2725: 2677: 2676: 2672: 2638: 2637: 2633: 2621: 2617: 2607: 2605: 2591: 2590: 2586: 2542: 2541: 2537: 2527: 2525: 2513: 2508: 2507: 2503: 2493: 2491: 2480: 2479: 2472: 2462: 2460: 2455: 2454: 2450: 2441: 2439: 2430: 2429: 2425: 2417: 2413: 2406: 2389: 2388: 2384: 2376:. Irene Klotz, 2372: 2365: 2355: 2353: 2342: 2341: 2337: 2327: 2325: 2314: 2313: 2309: 2253: 2252: 2248: 2202: 2201: 2197: 2187: 2185: 2176: 2175: 2171: 2161: 2159: 2148: 2147: 2143: 2133: 2131: 2120: 2119: 2115: 2105: 2103: 2094: 2093: 2089: 2079: 2077: 2061: 2060: 2056: 2006: 2001: 2000: 1996: 1984: 1980: 1970: 1968: 1959: 1958: 1954: 1944: 1942: 1931: 1930: 1926: 1916: 1914: 1898: 1897: 1893: 1885: 1881: 1843: 1842: 1833: 1828:on May 2, 2013. 1816: 1815: 1811: 1781: 1780: 1776: 1747:(6371): 16–17. 1738: 1737: 1733: 1724: 1722: 1713: 1712: 1705: 1695: 1693: 1665: 1664: 1660: 1604: 1603: 1599: 1569: 1568: 1564: 1560:. 24 June 2019. 1552: 1541: 1503: 1502: 1498: 1489: 1487: 1478: 1477: 1470: 1414: 1409: 1408: 1401: 1349: 1348: 1344: 1288: 1283: 1282: 1271: 1211: 1210: 1206: 1142: 1141: 1137: 1100:(7729): 18–19. 1091: 1090: 1086: 1077: 1075: 1066: 1065: 1061: 1023: 1022: 1018: 1010: 1003: 1002: 995: 985: 983: 973: 972: 968: 951: 941: 940: 936: 876: 875: 868: 863: 855:Weather of Mars 845:Climate of Mars 836: 829: 816: 807: 804: 795: 785: 782: 781: 780: 778: 769: 766: 765: 764: 762: 751: 749:Potential sinks 699: 680: 675: 671: 657:or nutrients. 645:. In contrast, 628: 620: 528: 527: 508: 505: 504: 503: 499: 496: 495: 494: 492: 477: 450: 386: 373: 354: 341: 296: 265: 228: 224: 220: 216: 211: 207: 200: 196: 188: 156: 145: 132: 100:astrobiologists 76: 65: 59: 56: 45: 25: 12: 11: 5: 6074: 6072: 6064: 6063: 6058: 6053: 6043: 6042: 6036: 6035: 6033: 6032: 6020: 6007: 6004: 6003: 6001: 6000: 5995: 5990: 5985: 5980: 5975: 5970: 5965: 5960: 5959: 5958: 5953: 5948: 5938: 5933: 5927: 5925: 5919: 5918: 5915: 5914: 5912: 5911: 5906: 5901: 5899:Northern Light 5896: 5891: 5886: 5881: 5876: 5871: 5866: 5860: 5858: 5855:Cancelled and 5852: 5851: 5849: 5848: 5843: 5838: 5833: 5828: 5823: 5818: 5813: 5808: 5803: 5798: 5793: 5788: 5783: 5778: 5773: 5768: 5763: 5757: 5755: 5751: 5750: 5748: 5747: 5746: 5745: 5732: 5730:Europa Clipper 5727: 5719: 5717: 5713: 5712: 5710: 5709: 5703: 5701: 5697: 5696: 5694: 5693: 5686: 5681: 5673: 5671: 5665: 5664: 5662: 5661: 5656: 5651: 5650: 5649: 5636: 5629: 5628: 5627: 5614: 5613: 5612: 5599: 5594: 5588: 5586: 5582: 5581: 5579: 5578: 5573: 5568: 5563: 5558: 5553: 5548: 5543: 5538: 5533: 5528: 5523: 5518: 5513: 5508: 5503: 5497: 5495: 5488: 5482: 5481: 5479: 5478: 5473: 5468: 5463: 5458: 5453: 5448: 5443: 5438: 5433: 5428: 5423: 5418: 5413: 5408: 5402: 5400: 5392: 5391: 5389: 5388: 5383: 5378: 5373: 5368: 5363: 5358: 5353: 5348: 5343: 5338: 5333: 5328: 5326:Drake equation 5323: 5318: 5313: 5308: 5302: 5300: 5296: 5295: 5293: 5292: 5287: 5282: 5277: 5272: 5267: 5265:Exoplanetology 5262: 5257: 5252: 5247: 5242: 5240:Astrochemistry 5236: 5234: 5230: 5229: 5224: 5222: 5221: 5214: 5207: 5199: 5190: 5189: 5186: 5183: 5182: 5180: 5179: 5174: 5169: 5164: 5158: 5156: 5152: 5151: 5149: 5148: 5141: 5134: 5126: 5124: 5118: 5117: 5115: 5114: 5107: 5100: 5095: 5090: 5085: 5080: 5075: 5070: 5065: 5059: 5057: 5051: 5050: 5048: 5047: 5040: 5033: 5026: 5020: 5018: 5012: 5011: 5009: 5008: 5001: 4994: 4987: 4980: 4973: 4966: 4959: 4953: 4951: 4945: 4944: 4937: 4935: 4933: 4932: 4924: 4922: 4916: 4915: 4910: 4908: 4907: 4900: 4893: 4885: 4876: 4875: 4873: 4872: 4859: 4847: 4844: 4843: 4841: 4840: 4839: 4838: 4833: 4823: 4818: 4813: 4808: 4807: 4806: 4801: 4796: 4786: 4785: 4784: 4773: 4771: 4767: 4766: 4763: 4762: 4760: 4759: 4754: 4749: 4747:Mars Institute 4744: 4739: 4732: 4724: 4722: 4718: 4717: 4715: 4714: 4708: 4706: 4700: 4699: 4697: 4696: 4691: 4686: 4681: 4676: 4671: 4666: 4661: 4656: 4650: 4648: 4641: 4635: 4634: 4631: 4630: 4628: 4627: 4621: 4619: 4615: 4614: 4612: 4611: 4605: 4603: 4599: 4598: 4596: 4595: 4594: 4593: 4588: 4583: 4578: 4573: 4568: 4563: 4553: 4552: 4551: 4534: 4528: 4526: 4520: 4519: 4517: 4516: 4515: 4514: 4509: 4501: 4500: 4499: 4494: 4486: 4480: 4478: 4472: 4471: 4469: 4468: 4467: 4466: 4461: 4451: 4450: 4449: 4444: 4433: 4431: 4422: 4416: 4415: 4412: 4411: 4409: 4408: 4403: 4398: 4393: 4388: 4382: 4380: 4374: 4373: 4371: 4370: 4365: 4360: 4355: 4350: 4345: 4340: 4335: 4330: 4325: 4323:Seasonal flows 4320: 4318:Rootless cones 4315: 4310: 4305: 4304: 4303: 4293: 4288: 4283: 4278: 4273: 4272: 4271: 4266: 4256: 4251: 4246: 4241: 4236: 4231: 4226: 4221: 4216: 4211: 4206: 4201: 4196: 4191: 4186: 4181: 4176: 4170: 4168: 4162: 4161: 4159: 4158: 4153: 4148: 4146:Valley network 4143: 4138: 4133: 4131:Observed rocks 4128: 4127: 4126: 4116: 4111: 4106: 4101: 4096: 4091: 4086: 4081: 4076: 4065: 4063: 4055: 4054: 4052: 4051: 4046: 4044:Ultimi Scopuli 4041: 4036: 4031: 4026: 4024:Terra Cimmeria 4021: 4016: 4011: 4006: 4001: 3996: 3991: 3986: 3981: 3976: 3971: 3965: 3963: 3957: 3956: 3954: 3953: 3948: 3943: 3938: 3932: 3930: 3921: 3915: 3914: 3909: 3906: 3905: 3900: 3898: 3897: 3890: 3883: 3875: 3867: 3866: 3854: 3809: 3773: 3745: 3706: 3675: 3652: 3637: 3603: 3577: 3545: 3518: 3499:(2): 537–547. 3483: 3455: 3389: 3362:(5): 326–332. 3345: 3314: 3263: 3205: 3179: 3153: 3142:Universe Today 3128: 3101:(17): L17202. 3082: 3047:(7401): 93–6. 3031: 3029: 3028: 2998:(3–4): 382–5. 2982: 2956: 2918:(7401): 93–6. 2902: 2880: 2836: 2817:(1): 144–152. 2801: 2758: 2723: 2670: 2648:(2): 276–285. 2631: 2615: 2584: 2555:(10): L10203. 2535: 2501: 2470: 2448: 2423: 2411: 2404: 2382: 2363: 2335: 2307: 2246: 2195: 2169: 2141: 2113: 2087: 2054: 1994: 1978: 1952: 1924: 1891: 1879: 1831: 1809: 1774: 1731: 1703: 1658: 1597: 1578:(2): 537–547. 1562: 1539: 1496: 1468: 1399: 1342: 1269: 1204: 1135: 1084: 1059: 1016: 993: 966: 934: 865: 864: 862: 859: 858: 857: 852: 847: 842: 835: 832: 831: 830: 817: 810: 808: 805: 798: 794: 791: 783: 767: 750: 747: 738:A team led by 718:Methanosarcina 697: 678: 673: 669: 668:. A low H 626: 623: 622: 618: 597: 588: 585: 577: 569: 561: 552: 549: 541: 517:carbon dioxide 506: 497: 481:microorganisms 476: 473: 448: 384: 371: 364:of water, and 353: 350: 340: 337: 226: 222: 218: 214: 209: 205: 198: 194: 186: 154: 143: 131: 128: 78: 77: 60:September 2022 28: 26: 19: 13: 10: 9: 6: 4: 3: 2: 6073: 6062: 6059: 6057: 6054: 6052: 6049: 6048: 6046: 6031: 6030: 6021: 6019: 6018: 6009: 6008: 6005: 5999: 5996: 5994: 5991: 5989: 5986: 5984: 5981: 5979: 5976: 5974: 5971: 5969: 5966: 5964: 5961: 5957: 5954: 5952: 5949: 5947: 5944: 5943: 5942: 5939: 5937: 5934: 5932: 5929: 5928: 5926: 5920: 5910: 5907: 5905: 5902: 5900: 5897: 5895: 5892: 5890: 5887: 5885: 5882: 5880: 5877: 5875: 5872: 5870: 5867: 5865: 5862: 5861: 5859: 5853: 5847: 5844: 5842: 5839: 5837: 5834: 5832: 5829: 5827: 5824: 5822: 5819: 5817: 5814: 5812: 5809: 5807: 5804: 5802: 5799: 5797: 5796:Europa Lander 5794: 5792: 5789: 5787: 5784: 5782: 5779: 5777: 5774: 5772: 5769: 5767: 5764: 5762: 5759: 5758: 5756: 5752: 5744: 5742: 5738: 5737: 5736: 5733: 5731: 5728: 5726: 5725: 5721: 5720: 5718: 5714: 5708: 5705: 5704: 5702: 5698: 5692: 5691: 5687: 5685: 5682: 5680: 5679: 5675: 5674: 5672: 5666: 5660: 5657: 5655: 5652: 5648: 5646: 5642: 5641: 5640: 5637: 5635: 5634: 5630: 5626: 5624: 5620: 5619: 5618: 5615: 5611: 5609: 5605: 5604: 5603: 5600: 5598: 5595: 5593: 5590: 5589: 5587: 5583: 5577: 5574: 5572: 5569: 5567: 5564: 5562: 5559: 5557: 5554: 5552: 5549: 5547: 5544: 5542: 5539: 5537: 5534: 5532: 5529: 5527: 5524: 5522: 5519: 5517: 5514: 5512: 5509: 5507: 5504: 5502: 5499: 5498: 5496: 5492: 5489: 5483: 5477: 5474: 5472: 5469: 5467: 5464: 5462: 5459: 5457: 5454: 5452: 5449: 5447: 5444: 5442: 5439: 5437: 5434: 5432: 5429: 5427: 5424: 5422: 5419: 5417: 5414: 5412: 5409: 5407: 5404: 5403: 5401: 5399: 5393: 5387: 5384: 5382: 5379: 5377: 5374: 5372: 5369: 5367: 5364: 5362: 5359: 5357: 5354: 5352: 5351:Extremophiles 5349: 5347: 5344: 5342: 5339: 5337: 5334: 5332: 5329: 5327: 5324: 5322: 5319: 5317: 5314: 5312: 5309: 5307: 5304: 5303: 5301: 5297: 5291: 5288: 5286: 5283: 5281: 5278: 5276: 5273: 5271: 5268: 5266: 5263: 5261: 5258: 5256: 5253: 5251: 5248: 5246: 5243: 5241: 5238: 5237: 5235: 5231: 5227: 5220: 5215: 5213: 5208: 5206: 5201: 5200: 5197: 5184: 5178: 5175: 5173: 5170: 5168: 5165: 5163: 5160: 5159: 5157: 5153: 5147: 5146: 5142: 5140: 5139: 5135: 5133: 5132: 5128: 5127: 5125: 5123: 5119: 5113: 5112: 5108: 5106: 5105: 5101: 5099: 5096: 5094: 5091: 5089: 5086: 5084: 5081: 5079: 5076: 5074: 5071: 5069: 5066: 5064: 5061: 5060: 5058: 5056: 5052: 5046: 5045: 5041: 5039: 5038: 5034: 5032: 5031: 5027: 5025: 5022: 5021: 5019: 5017: 5016:Dwarf planets 5013: 5007: 5006: 5002: 5000: 4999: 4995: 4993: 4992: 4988: 4986: 4985: 4981: 4979: 4978: 4974: 4972: 4971: 4967: 4965: 4964: 4960: 4958: 4955: 4954: 4952: 4950: 4946: 4941: 4931: 4930: 4926: 4925: 4923: 4921: 4917: 4913: 4906: 4901: 4899: 4894: 4892: 4887: 4886: 4883: 4871: 4860: 4858: 4849: 4848: 4845: 4837: 4834: 4832: 4829: 4828: 4827: 4824: 4822: 4819: 4817: 4814: 4812: 4809: 4805: 4802: 4800: 4797: 4795: 4792: 4791: 4790: 4787: 4783: 4780: 4779: 4778: 4775: 4774: 4772: 4768: 4758: 4755: 4753: 4750: 4748: 4745: 4743: 4740: 4738: 4737: 4733: 4731: 4730: 4726: 4725: 4723: 4719: 4713: 4710: 4709: 4707: 4705: 4701: 4695: 4692: 4690: 4687: 4685: 4682: 4680: 4679:Human mission 4677: 4675: 4674:Sample return 4672: 4670: 4667: 4665: 4662: 4660: 4657: 4655: 4652: 4651: 4649: 4645: 4642: 4640: 4636: 4626: 4623: 4622: 4620: 4616: 4610: 4607: 4606: 4604: 4600: 4591: 4584: 4581: 4574: 4571: 4564: 4562: 4559: 4558: 4557: 4554: 4549: 4540: 4539: 4538: 4537:Mars-crossers 4535: 4533: 4530: 4529: 4527: 4525: 4521: 4513: 4510: 4508: 4505: 4504: 4502: 4498: 4495: 4493: 4490: 4489: 4487: 4485: 4482: 4481: 4479: 4477: 4473: 4465: 4462: 4460: 4457: 4456: 4455: 4452: 4448: 4445: 4443: 4440: 4439: 4438: 4435: 4434: 4432: 4430: 4426: 4423: 4421: 4417: 4407: 4404: 4402: 4399: 4397: 4394: 4392: 4389: 4387: 4384: 4383: 4381: 4379: 4375: 4369: 4366: 4364: 4361: 4359: 4356: 4354: 4353:Tharsis bulge 4351: 4349: 4346: 4344: 4341: 4339: 4336: 4334: 4331: 4329: 4326: 4324: 4321: 4319: 4316: 4314: 4311: 4309: 4306: 4302: 4299: 4298: 4297: 4294: 4292: 4291:Ore resources 4289: 4287: 4284: 4282: 4279: 4277: 4274: 4270: 4267: 4265: 4262: 4261: 4260: 4257: 4255: 4252: 4250: 4247: 4245: 4242: 4240: 4237: 4235: 4232: 4230: 4227: 4225: 4222: 4220: 4217: 4215: 4212: 4210: 4207: 4205: 4202: 4200: 4197: 4195: 4192: 4190: 4187: 4185: 4184:Chaos terrain 4182: 4180: 4177: 4175: 4174:Brain terrain 4172: 4171: 4169: 4167: 4163: 4157: 4154: 4152: 4149: 4147: 4144: 4142: 4139: 4137: 4134: 4132: 4129: 4125: 4122: 4121: 4120: 4117: 4115: 4112: 4110: 4107: 4105: 4102: 4100: 4097: 4095: 4092: 4090: 4089:Chaos terrain 4087: 4085: 4082: 4080: 4077: 4074: 4070: 4067: 4066: 4064: 4062: 4056: 4050: 4047: 4045: 4042: 4040: 4037: 4035: 4032: 4030: 4027: 4025: 4022: 4020: 4017: 4015: 4012: 4010: 4007: 4005: 4004:Planum Boreum 4002: 4000: 3997: 3995: 3994:Olympia Undae 3992: 3990: 3987: 3985: 3984:Eridania Lake 3982: 3980: 3977: 3975: 3972: 3970: 3967: 3966: 3964: 3962: 3958: 3952: 3949: 3947: 3944: 3942: 3939: 3937: 3934: 3933: 3931: 3929: 3925: 3922: 3920: 3916: 3912: 3907: 3903: 3896: 3891: 3889: 3884: 3882: 3877: 3876: 3873: 3863: 3858: 3855: 3850: 3846: 3842: 3838: 3834: 3830: 3826: 3822: 3821: 3813: 3810: 3805: 3801: 3797: 3793: 3789: 3785: 3777: 3774: 3758: 3757: 3749: 3746: 3741: 3737: 3733: 3729: 3725: 3721: 3717: 3710: 3707: 3695: 3694: 3689: 3685: 3679: 3676: 3671: 3667: 3663: 3656: 3653: 3648: 3644: 3640: 3634: 3630: 3626: 3622: 3618: 3614: 3607: 3604: 3600: 3596: 3592: 3588: 3581: 3578: 3566: 3562: 3558: 3552: 3550: 3546: 3541: 3537: 3533: 3529: 3522: 3519: 3514: 3510: 3506: 3502: 3498: 3494: 3487: 3484: 3472: 3471: 3466: 3459: 3456: 3451: 3447: 3442: 3437: 3432: 3427: 3423: 3419: 3415: 3411: 3410: 3405: 3398: 3396: 3394: 3390: 3385: 3381: 3377: 3373: 3369: 3365: 3361: 3357: 3349: 3346: 3333: 3329: 3325: 3318: 3315: 3310: 3306: 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methane
atmosphere of Mars
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Methane
ultraviolet
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