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Age aspects of habitability

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dc.contributor.author Safonova, M
dc.contributor.author Murthy, J
dc.contributor.author Shchekinov, Yu. A
dc.date.accessioned 2020-11-17T14:37:21Z
dc.date.available 2020-11-17T14:37:21Z
dc.date.issued 2016-04
dc.identifier.citation International Journal of Astrobiology, Vol. 15, No. 02, pp. 93-105 en_US
dc.identifier.issn 1473-5504
dc.identifier.uri http://prints.iiap.res.in/handle/2248/7181
dc.description Restricted Access © Cambridge University Press http://dx.doi.org/10.1017/S1473550415000208 en_US
dc.description.abstract A ‘habitable zone’ of a star is defined as a range of orbits within which a rocky planet can support liquid water on its surface. The most intriguing question driving the search for habitable planets is whether they host life. But is the age of the planet important for its habitability? If we define habitability as the ability of a planet to beget life, then probably it is not. After all, life on Earth has developed within only ~800 Myr after its formation – the carbon isotope change detected in the oldest rocks indicates the existence of already active life at least 3.8 Gyr ago. If, however, we define habitability as our ability to detect life on the surface of exoplanets, then age becomes a crucial parameter. Only after life had evolved sufficiently complex to change its environment on a planetary scale, can we detect it remotely through its imprint on the atmosphere – the so-called biosignatures, out of which the photosynthetic oxygen is the most prominent indicator of developed (complex) life as we know it. Thus, photosynthesis is a powerful biogenic engine that is known to have changed our planet's global atmospheric properties. The importance of planetary age for the detectability of life as we know it follows from the fact that this primary process, photosynthesis, is endothermic with an activation energy higher than temperatures in habitable zones, and is sensitive to the particular thermal conditions of the planet. Therefore, the onset of photosynthesis on planets in habitable zones may take much longer time than the planetary age. The knowledge of the age of a planet is necessary for developing a strategy to search for exoplanets carrying complex (developed) life – many confirmed potentially habitable planets are too young (orbiting Population I stars) and may not have had enough time to develop and/or sustain detectable life. In the last decade, many planets orbiting old (9–13 Gyr) metal-poor Population II stars have been discovered. Such planets had had enough time to develop necessary chains of chemical reactions and may carry detectable life if located in a habitable zone. These old planets should be primary targets in search for the extraterrestrial life. en_US
dc.language.iso en en_US
dc.publisher Cambridge University Press en_US
dc.subject Formation en_US
dc.subject Habitability en_US
dc.subject Photosynthesis en_US
dc.subject Planetary systems en_US
dc.title Age aspects of habitability en_US
dc.type Article en_US


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