Until the 1980s, the icy satellites of the outer planets were scarcely thought of as places where life could ever have existed. Few could have imagined that one of them, Europa, would within twenty years have become the rival of Mars as a priority for astrobiological study. This course recounts the history of our changing perceptions of the icy satellites, examines the available evidence for their internal structures, and considers the niches offered for life to begin and to be sustained. In this context, the 'habitable zone' embraces settings devoid of both sunlight and an atmosphere. These are areas where life could survive on the energy from chemical reactions made possible by the discharge of hot chemically enriched fluids through vents on the floor of an ocean capped by a thick layer of ice. Note that 'ice' does not necessarily mean just frozen water. In the outer Solar System, although H2O is usually the dominant component, ice can incorporate other frozen volatiles such as NH3, CO2, CO, CH4 and N2.
This OpenLearn course is an adapted extract from the Open University course S283 Planetary science and the search for life .
OpenLearn - Icy bodies: Europa and elsewhere Except for third party materials and otherwise, this content is made available under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 Licence, full copyright detail can be found in the acknowledgements section. Please see full copyright statement for details.