Abstract
The “Rare Earth” hypothesis—put forward by Ward and Brownlee in their 2000 book of the same title—states that prokaryote-type organisms may be common in the universe but animals and higher plants are exceedingly rare. If this idea is correct, the search for extraterrestrial life is essentially the search for microorganisms. Various indicators may be used to detect extant or extinct microbial life beyond Earth. Among them are chemical biosignatures, such as biomolecules and stable isotope ratios. The present minireview focuses on the major problems associated with the identification of chemical biosignatures. Two main types of misinterpretation are distinguished, namely false positive and false negative results. The former can be caused by terrestrial biogenic contaminants or by abiotic products. Terrestrial contamination is a common problem in space missions that search for biosignatures on other planets and moons. Abiotic organics can lead to false positive results if erroneously interpreted as biomolecules, but also to false negatives, for example when an abiotic source obscures a less productive biological one. In principle, all types of putative chemical biosignatures are prone to misinterpretation. Some, however, are more reliable (“stronger”) than others. These include: (i) homochiral polymers of defined length and sequence, comparable to proteins and polynucleotides; (ii) enantiopure compounds; (iii) the existence of only a subset of molecules when abiotic syntheses would produce a continuous range of molecules; the proteinogenic amino acids constitute such a subset. These considerations are particularly important for life detection missions to solar system bodies such as Mars, Europa, and Enceladus.
Highlights
Life can leave different kinds of signatures
Chemical analysis by Raman spectroscopy revealed that morphologically similar structures from the same locality as the original specimens were quartz and haematite-filled fractures (Marshall et al, 2011; Marshall and Marshall, 2013)
The category of false positive biosignatures may be further subdivided into terrestrial biogenic contaminants and products of non-biological processes
Summary
Life can leave different kinds of signatures. Fossil evidence of microorganisms, for example, can be morphological (e.g., fossilized cells) or chemical (organic, mineralogical, elemental, isotopic; Westall and Cavalazzi, 2011). The category of false positive biosignatures may be further subdivided into terrestrial biogenic contaminants and products of non-biological processes This minireview gives examples of potential pitfalls in the search for extraterrestrial chemical biosignatures. On the other hand, make the compounds that they need in order to survive and compete” (Dorn, 2005) If this holds universally, which seems to be a reasonable assumption, the differences in the distribution patterns would be a powerful tool to identify extraterrestrial chemical biosignatures. Another approach uses the fact that abiotic synthesis yields a continuous range of members of a compound class, while organisms synthesize only a subset of the possible molecules (“Lego Principle”; McKay, 2004).
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