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Habitable zone
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==Habitability outside the HZ== [[Image:Liquid lakes on titan.jpg|thumb|upright|The discovery of hydrocarbon lakes on Saturn's moon Titan has begun to call into question the [[carbon chauvinism]] that underpins HZ concept.]] Liquid-water environments have been found to exist in the absence of atmospheric pressure and at temperatures outside the HZ temperature range. For example, [[Saturn]]'s moons [[Titan (moon)|Titan]] and [[Enceladus]] and [[Jupiter]]'s moons [[Europa (moon)|Europa]] and [[Ganymede (moon)|Ganymede]], all of which are outside the habitable zone, may hold large volumes of liquid water in [[subsurface ocean]]s.<ref>{{cite web |url = http://phl.upr.edu/library/media/liquidwaterinthesolarsystem |title = Liquid Water in the Solar System |access-date = 2013-12-15 |last = Torres |first = Abel |date = 2012-06-12 |archive-date = 2013-11-18 |archive-url = https://web.archive.org/web/20131118034218/http://phl.upr.edu/library/media/liquidwaterinthesolarsystem |url-status = dead }}</ref> Outside the HZ, [[tidal heating]] and [[radioactive decay]] are two possible heat sources that could contribute to the existence of liquid water.<ref name="Cowen2008"/><ref name="Bryner, Jeanna"/> Abbot and Switzer (2011) put forward the possibility that subsurface water could exist on [[rogue planet]]s as a result of radioactive decay-based heating and insulation by a thick surface layer of ice.<ref name="physcisarxivlab-2011"/> With some theorising that life on Earth may have actually originated in stable, subsurface habitats,<ref name=Munro2013>{{Citation |title = Miners deep underground in northern Ontario find the oldest water ever known |url = https://nationalpost.com/news/canada/worlds-oldest-water-bubbling-into-northern-ontario-mine |date = 2013 |author = Munro, Margaret |work = National Post |access-date = 2013-10-06 }}</ref><ref name=Davies2013>{{cite journal |title = The Origin of Life II: How did it begin? |journal = Science Progress |issn = 2047-7163 |volume = 84 |issue = 1 |pages = 17β29 |date = February 2001 |doi = 10.3184/003685001783239096 |doi-access = free |pmid = 11382135 |pmc = 10367499 |last = Davies |first = Paul }}</ref> it has been suggested that it may be common for wet subsurface extraterrestrial habitats such as these to 'teem with life'.<ref name=Taylor1996>{{Citation |title = Life Underground |url = http://www.psrd.hawaii.edu/Dec96/PSRD-LifeUnderground.pdf |date = 1996 |author = Taylor, Geoffrey |journal = Planetary Science Research Discoveries |page = 4 |bibcode = 1996psrd.reptE...4T |access-date = 2013-10-06 }}</ref> On Earth itself, living organisms may be found more than {{convert|6|km|mi|abbr=on}} below the surface.<ref name=Doyle2013>{{Citation |title = Deep underground, worms and "zombie microbes" rule |url = https://www.reuters.com/article/us-life-idUSBRE9230WM20130304 |author = Doyle, Alister |access-date = 2013-10-06 |work=Reuters |date=4 March 2013 }}</ref> Another possibility is that outside the HZ organisms may use [[alternative biochemistry|alternative biochemistries]] that do not require water at all. Astrobiologist [[Christopher McKay]], has suggested that [[methane]] ({{chem|C|H|4}}) may be a solvent conducive to the development of "cryolife", with the Sun's "methane habitable zone" being centered on {{convert|1610000000|km|mi AU|sigfig=2|abbr=on}} from the star.<ref name=villard-2011 /> This distance is coincident with the location of Titan, whose lakes and rain of methane make it an ideal location to find McKay's proposed cryolife.<ref name=villard-2011 /> In addition, [[list of microorganisms tested in outer space|testing of a number of organisms]] has found some are capable of surviving in extra-HZ conditions.<ref> {{cite journal |last1=Nicholson |first1=W. L. |last2=Moeller |first2=R. |last3=Horneck |first3=G. |date=2012 |title=Transcriptomic Responses of Germinating Bacillus subtilis Spores Exposed to 1.5 Years of Space and Simulated Martian Conditions on the EXPOSE-E Experiment PROTECT |journal=Astrobiology |volume=12 |issue=5 |pages=469β86 |bibcode=2012AsBio..12..469N |doi=10.1089/ast.2011.0748 |pmid=22680693 }}</ref>
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