Abstract

Effects of perchlorate salts prevalent on the surface of Mars are of significant interest to astrobiology from the perspective of potential life on the Red Planet. Halorubrum lacusprofundi, a cold-adapted halophilic Antarctic archaeon, was able to grow anaerobically on 0.04 M concentration of perchlorate. With increasing concentrations of perchlorate, growth was inhibited, with half-maximal growth rate in ca. 0.3 M NaClO4 and 0.1 M Mg(ClO4)2 under aerobic conditions. Magnesium ions were also inhibitory for growth, but at considerably higher concentrations, with half-maximal growth rate above 1 M. For a purified halophilic β-galactosidase enzyme of H. lacusprofundi expressed in Halobacterium sp. NRC-1, 50% inhibition of catalytic activity was observed at 0.88 M NaClO4 and 0.13 M Mg(ClO4)2. Magnesium ions were a more potent inhibitor of the enzyme than of cell growth. Steady-state kinetic analysis showed that Mg(ClO4)2 acts as a mixed inhibitor (KI = 0.04 M), with magnesium alone being a competitive inhibitor (KI = 0.3 M) and perchlorate alone acting as a very weak noncompetitive inhibitor (KI = 2 M). Based on the estimated concentrations of perchlorate salts on the surface of Mars, our results show that neither sodium nor magnesium perchlorates would significantly inhibit growth and enzyme activity of halophiles. This is the first study of perchlorate effects on a purified enzyme. Key Words: Halophilic archaea—Perchlorate—Enzyme inhibition—Magnesium. Astrobiology 18, 412–418.

Highlights

  • Halophiles have long been proposed as candidates for survival on Mars since they have evolved to grow in high salt concentrations and multiple extreme conditions on Earth (Landis, 2001; DasSarma, 2006)

  • Our results show that this polyextremophilic halophile and its model enzyme, while exhibiting sensitivity to these ions, retain their ability to function in their presence at high concentrations far above what is likely to be encountered on the surface of our sister planet

  • We investigated the effects of sodium and magnesium perchlorate salts prevalent on Mars on growth and enzyme function of a cold-adapted extreme halophile from Antarctica

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Summary

Introduction

Halophiles have long been proposed as candidates for survival on Mars since they have evolved to grow in high salt concentrations and multiple extreme conditions on Earth (Landis, 2001; DasSarma, 2006). A few halophiles, including halophilic archaea, are adapted to cold temperatures, including subzero temperatures, with the freezing point of water depressed by high salinity (Reid et al, 2006) As a result, these extremophilic microbes may represent potential models for life on Mars where these stressors are commonly found. The presence of oxidizers was first suspected during the NASA Viking lander missions of the 1970s (Klein, 1978) This was later confirmed by the Phoenix lander mission where perchlorate concentrations of 0.4–0.6 wt % (3.3 mM Mg2+, 2.4 mM ClO4-) were detected by the onboard Wet Chemistry Lab (Hecht et al, 2009) and confirmed by the Sample Analysis at Mars instrument on the Mars Curiosity rover (Glavin et al, 2013). The Horowitz Crater had larger recurring slope lineae indicative of the potential for liquid water and spectra consistent with martian soil mixed with sodium perchlorate (Ojha et al, 2015)

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