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Permafrost is soil that remains below the freezing point of water (0 °C) throughout the year. It is mainly located at high latitudes (24 % of the exposed land in the Earth’s northern hemisphere) and high altitude (alpine permafrost). Mars is the other rocky planet in the Solar System that could have a permafrost layer. Asteroid 25143-Itokawa and Eros show surface morphologies that suggest the occurrence of a permafrost and occasionally meltwater. Earth’s permafrost is a site of microbial activity within thin films of liquid water between ice and soil particles. The occurrence and distribution of these microbial communities are studied as possible analogues of life forms on icy planets and satellites in the Solar System and for exoplanets.
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© 2014 Springer-Verlag Berlin Heidelberg
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Pinti, D.L. (2014). Permafrost. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1172-3
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DOI: https://doi.org/10.1007/978-3-642-27833-4_1172-3
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Publisher Name: Springer, Berlin, Heidelberg
Online ISBN: 978-3-642-27833-4
eBook Packages: Springer Reference Physics and AstronomyReference Module Physical and Materials ScienceReference Module Chemistry, Materials and Physics
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Latest
Permafrost- Published:
- 25 November 2021
DOI: https://doi.org/10.1007/978-3-642-27833-4_1172-4
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Original
Permafrost- Published:
- 02 May 2015
DOI: https://doi.org/10.1007/978-3-642-27833-4_1172-3