Oxygen is not a prerequisite for all living systems. While it is sometimes concluded that free oxygen is needed for all but the simplest organisms, less efficient metabolic processes coupled with higher food collection efficiency—or a more sluggish metabolism—would seem to do just as well. Earth is the only planet in the solar system on which molecular oxygen is known to be present in large amounts. Since plant photosynthesis is the primary source of atmospheric oxygen, it seems safe to infer that no other planet has large-scale plant photosynthesis accompanied by the production of oxygen.
The possibility of the existence of extraterrestrial life raises the important question of man's being able to detect it. Research on extraterrestrial life detection is predicated on the ability to develop ways to detect it even when the living systems are based on principles entirely different from those on Earth.
The substitution of various molecules for those of known biological significance to living organisms as we know them has been investigated; the substitution of NH2 for OH in ammonia-rich environments leads to a diverse, and biologically very promising, chemistry. The hypothesis that silicon may replace carbon does not support the construction of extraterrestrial genetics based on silicon compounds. (Silicon compounds participate in redistribution reactions which tend to maximize the randomness of silicon bonding, and the stable retention of genetic information over long time periods is thus very improbable.)
Evidence relevant to life on Mars has been summarized by Sagan (ch. 1 of [ref.10]):
The Origin of Life
In the past decade, considerable advances have been made in our knowledge of the probable processes leading to the origin of life on Earth. A succession of laboratory experiments has shown that essentially all the organic building blocks of contemporary terrestrial organisms can be synthesized by supplying energy to a mixture of the hydrogen-rich gases of the primitive terrestrial atmosphere. It now seems likely that the laboratory synthesis of a self-replicating molecular system is only a short time away from realization. The syntheses of similar systems in the primitive terrestrial oceans must have occurred—collections of molecules which were so constructed that, by the laws of physics and chemistry, they forced the production of identical copies of themselves out of the building blocks in the surrounding medium. Such a system satisfies many of the criteria for Darwinian natural selection, and the long evolutionary path from molecule to advanced organism can then be understood. Since nothing except very general primitive atmospheric conditions and energy sources are required for such syntheses, it is possible that similar events occurred in the early history of Mars and that life may have come into being on that planet several billions of years ago. Its subsequent evolution, in response to the changing Martian environment, would have produced organisms quite different from those which now inhabit Earth.
Simulation Experiments
Experiments have been performed in which terrestrial micro-organisms have been introduced into simulated Martian environments, with atmospheres composed of nitrogen and carbon dioxide, no oxygen, very little water, a daily temperature variation from +20° to -60° C, and high ultraviolet fluxes. It was found that in every sample of terrestrial soil used there were a few varieties of micro-organisms which easily survived on "Mars." When the local abundance of water was increased, terrestrial micro-organisms were able to grow. Indigenous Martian organisms may be even more efficient in coping with the apparent rigors of their environment. These findings underscore the necessity for sterilizing Mars entry vehicles so as not to perform accidental biological contamination of that planet and obscure the subsequent search for extraterrestrial life.
Direct Searches for Life on Mars
The early evidence for life on Mars—namely, reports of vivid green coloration and the so-called "canals"—are now known to be largely illusory. There are three major areas of contemporary investigation: visual, polarimetric, and spectrographic.
As the Martian polar ice cap recedes each spring, a wave of darkening propagates through the Martian dark areas, sharpening their outlines and increasing their contrast with the surrounding deserts. These changes occur during periods of relatively high humidity and relatively high daytime temperatures. A related dark collar, not due to simple dampening of the soil, follows the edge of the polar cap in its regression. Occasional nonseasonal changes in the form of the Martian dark regions have been observed and sometimes cover vast areas of surface.
Observations of the polarization of sunlight reflected from the Martian dark areas indicate that the small particles covering the dark areas change their size distribution in the spring, while the particles covering the bright areas do not show any analogous changes.
Finally, infrared spectroscopic observations of the Martian dark areas show three spectral features which, to date, seem to be interpretable only in terms of organic matter, the particular molecules giving rise to the absorptions being hydrocarbons and aldehydes. [However, see p. 7 and Rea et al. ([ref.9]).]
Taken together, these observations suggest, but do not conclusively prove, that the Martian dark areas are covered with small organisms composed of familiar types of organic matter, which change their size and darkness in response to the moisture and heat of the Martian spring. We have no evidence either for or against the existence of more advanced life forms. There is much more information which can be garnered from the ground, balloons, Earth satellites, Mars flybys, and Mars orbiters, but the critical tests for life on Mars can only be made from landing vehicles equipped with experimental packages....
Results of Kaplan et al. ([ref.31]) indicate that Mars has no detectable oxygen, but does contain small amounts of water vapor, more abundant carbon dioxide, possibly a large surface flux of solar ultraviolet radiation, and estimated daily temperature variations of 100° C at many latitudes. Studies have shown that terrestrial micro-organisms can survive these extremely harsh environments. Furthermore, a variety of physiological and ecological adaptations might enable the biota to survive the low nighttime temperatures and intracellular ice crystallization.
Less evidence is available to support the possibility of extraterrestrial life on other planets. The Moon has no atmosphere, and extremes of temperature characterize its surface. However, the Moon could have a layer of subsurface permafrost beneath which liquid water might be trapped. The temperatures of these strata might be biologically moderate.
Studies by Davis and Libby ([ref.32]) on the atmosphere of Jupiter support the possibility of the production of organic matter in its atmosphere in a manner analogous to the processes which may have led to the synthesis of organic molecules in the Earth's early history. It is difficult to assess the possibility that life has evolved on Jupiter during the 4- or 5-billion-year period in which the planet has retained a reducing atmosphere.
The question of extraterrestrial life and of the origin of life is interwoven. Discovery of the first and analysis of its nature may very well elucidate the second.
The oldest form of fossil known today is that of a microscopic plant similar in form to common algae found in ponds and lakes. Scientists know that similar organisms flourished in the ancient seas over 2 billion years ago. However, since algae are a relatively complex form of life, life in some simpler form could have originated much earlier. Organic material similar to that found in modern organisms can be detected in these ancient deposits as well as in much older Precambrian rocks.