EXTREMOPHILES as Astrobiological Models. Группа авторов
hydrothermal minerals by using sulfur as electron acceptors or donors (e.g., barite and pyrite), depending on the redox conditions. In the Rio Tinto subsurface, some of the reactions that followed the microbes to obtain energy mimic or are the reverse of the biochemical processes that would have appeared in a S and Fe world prebiotic scenario for an emergent metabolism [2.43] [2.104]. Therefore, there is a close connection between a substrate that promotes the geochemical cycles of S and Fe and the microbial metabolism that couples them to obtain energy in the most favorable ways. If life arose on Mars, the dominance of S and Fe geochemical processes rooted in an early metabolism very likely would have produced the same metabolic minerals in the interior of the red planet [2.43].
It is often claimed that acidic environments are inhospitable for the preservation of molecular traces of life since the highly oxidizing and aggressive pH would rapidly destroy the biological and organic compounds. The microscopic study of modern and ancient Rio Tinto materials [2.39] has shown that the high mineralization rates of the acidic solutions encourages the preservation of biological structures in great detail (Figure 2.6a, b1, b2). Paradoxically, in the molecular analysis of samples, the preservation of organic compounds was not considered under such low pH and high Eh conditions. Later on, the sample analysis of the different terrace and gossan levels showed that fragments of biomolecules and complex organic compounds are found in all deposits from the most modern sediments to the oldest materials of the acidic system. Using peptide extraction techniques on ancient acidic materials from the Rio Tinto terraces, Colín-García et al. [2.22] showed preservation of protein fragments during the last 2.1 million years. Such peptidic sequences provided qualitative information about the organisms in the past of the acidic system, which coincide with some microorganisms living in the modern system. Very recently, the sample analysis of surface and subsurface using TOF-SIMS detected diverse organic compounds that are associated with microbial structures (Figure 2.6a, c1 to c3). The preservation of molecular traces of life in acidic conditions is even more extraordinary as these rocks have been exposed to intense diagenesis that has changed the composition of the mineral matrix from sulfates to iron oxides under varying pH and Eh conditions. The occurrence of biomolecules and organic compounds of biological origin in the Rio Tinto rocks demonstrates the preservation of molecular traces of life in materials formed under extreme acidic conditions and despite exposure to drastic diagenesis.
The preservation of different biosignatures in the ancient acidic materials of Rio Tinto strongly supports that, if life emerged on Mars, traces of its activity in acidic deposits are just as likely to remain as they are in materials that formed under mildly neutral conditions in the red planet [2.28]. Given that acidic environments were abundant in the Late Noachian to Hesperian ages (more than 3.5 billion years ago), the next astrobiological missions should increase the chances of finding traces of life on the red planet by seeking them in acidic deposits.
Figure 2.6 Preservation of different traces of life in the oldest Rio Tinto terrace (a) that has been dated as 7 to 2.1 million years old [2.32, 2.37]. b1 and b2 show preservation of plants and micron-sized bacterial filaments, respectively. The analysis of the terrace samples by TOF-SIMS shows the detection of filament structures outlined by the distribution of the negative fragments of different lipids biomarkers like Myristic (c1), Pentadecanoic (c2), and Palmitic acids (c3). (Image credit: the authors).
2.9 Conclusions
In the last fifty years, important advances in microbiology have challenged the view generated by the Viking Missions, which were very pessimistic about the existence of life on Mars. Thanks to research on extremophiles, we now know that life is extremely robust and able to adapt to extraordinarily diverse conditions, which has increased the probability of finding life on other planetary bodies. Of the different extremophiles, acidophiles are of special interest because they are the only ones that create the extreme conditions of the environment in which they thrive. The characterization of the Rio Tinto basin, an extreme acidic environment 92 km long, has answered some basic questions, like the origin of the extreme acidic conditions of the ecosystem, the identification and isolation of the microorganisms responsible for creating these conditions and the generation of iron secondary minerals along the river, but it has also posed new ones, such as the paradox of the unexpectedly high level of diverse complex eukaryotic microorganisms or the need to explain the detection of functional activities in non-permissive environmental conditions, all of which are of astrobiological interest. The discovery of Noachian iron lithological units on Mars, similar to those produced biologically in the Tinto basin, have given Rio Tinto the status of geochemical and mineralogical terrestrial analogue that can lead to a more detailed vision of the possible geomicrobiological processes that may have driven the generation of iron oxides and sulfates on Mars.
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