A new study shows that the breakdown of water molecules trapped in ancient Martian rocks likely produced enough chemical energy to sustain microorganisms for hundreds of millions of years beneath the Red Planet’s surface.
PROVIDENCE, R.I. [Brown University] — A new study shows evidence that ancient Mars probably had an ample supply of chemical energy for microbes to thrive underground.
“We showed, based on basic physics and chemistry calculations, that the ancient Martian subsurface likely had enough dissolved hydrogen to power a global subsurface biosphere,” said Jesse Tarnas, a graduate student at Brown University and lead author of a study published in Earth and Planetary Science Letters. “Conditions in this habitable zone would have been similar to places on Earth where underground life exists.”
Earth is home to what are known as subsurface lithotrophic microbial ecosystems — SliMEs for short. Lacking energy from sunlight, these subterranean microbes often get their energy by peeling electrons off of molecules in their surrounding environments. Dissolved molecular hydrogen is a great electron donor and is known to fuel SLiMEs on Earth.
This new study shows that radiolysis, a process through which radiation breaks water molecules into their constituent hydrogen and oxygen parts, would have created plenty of hydrogen in the ancient Martian subsurface. The researchers estimate that hydrogen concentrations in the crust around 4 billion years ago would have been in the range of concentrations that sustain plentiful microbes on Earth today.
The findings don’t mean that life definitely existed on ancient Mars, but they do suggest that if life did indeed get started, the Martian subsurface had the key ingredients to support it for hundreds of millions of years. The work also has implications for future Mars exploration, suggesting that areas where the ancient subsurface is exposed might be good places to look for evidence of past life.
Going underground
Since the discovery decades ago of ancient river channels and lake beds on Mars, scientists have been tantalized by the possibility that the Red Planet may once have hosted life. But while evidence of past water activity is unmistakable, it’s not clear for how much of Martian history water actually flowed. State-of-the-art climate models for early Mars produce temperatures that rarely peak above freezing, which suggests that the planet’s early wet periods may have been fleeting events. That’s not the best scenario for sustaining life at the surface over the long term, and it has some scientists thinking that the subsurface might be a better bet for past Martian life.
“The question then becomes: What was the nature of that subsurface life, if it existed, and where did it get its energy?” said Jack Mustard, a professor in Brown’s Department of Earth, Environmental and Planetary Sciences and a study coauthor. “We know that radiolysis helps to provide energy for underground microbes on Earth, so what Jesse did here was to pursue the radiolysis story on Mars.”
The researchers looked at data from the gamma ray spectrometer that flies aboard NASA’s Mars Odyssey spacecraft. They mapped out abundances of the radioactive elements thorium and potassium in the Martian crust. Based on those abundances, they could infer the abundance of a third radioactive element, uranium. The decay of those three elements provides the radiation that drives the radiolytic breakdown of water. And because the elements decay at constant rates, the researchers could use the modern abundances to calculate the abundances 4 billion years ago. That gave the team an idea of the radiation flux that would have been active to drive radiolysis.
The next step was to estimate how much water would have been available for that radiation to zap. Geological evidence suggests there would have been plenty of groundwater bubbling about in the porous rocks of the ancient Martian crust. The researchers used measurements of the density of the Martian crust to estimate roughly how much pore space would have been available for water to fill.
Finally, the team used geothermal and climate models to determine where the sweet spot for potential life would have been. It can’t be so cold that all water is frozen, but it also can’t be overcooked by heat from the planet’s molten core.
Combining those analyses, the researchers conclude that Mars likely had a global subsurface habitable zone several kilometers in thickness. In that zone, hydrogen production via radiolysis would have generated more than enough chemical energy to support microbial life, based on what’s known about such communities on Earth. And that zone would have persisted for hundreds of millions of years, the researchers conclude.
The findings held up even when the researchers modeled a variety of different climate scenarios — some on the warmer side, others on the colder side. Interestingly, Tarnas says, the amount of subsurface hydrogen available for energy actually goes up under the extremely cold climate scenarios. That’s because a thicker layer of ice above the habitable zone serves as a lid that helps to keep hydrogen from escaping the subsurface.
“People have a conception that a cold early Mars climate is bad for life, but what we show is that there’s actually more chemical energy for life underground in a cold climate,” Tarnas said. “That’s something we think could change people’s perception of the relationship between climate and past life on Mars.”
Exploration implications
Tarnas and Mustard say the findings could be useful in thinking about where to send spacecraft looking for signs of past Martian life.
“One of the most interesting options for exploration is looking at megabreccia blocks — chunks of rock that were excavated from underground via meteorite impacts,” Tarnas said. “Many of them would have come from the depth of this habitable zone, and now they’re just sitting, often relatively unaltered, on the surface.”
Mustard, who has been active in the process of selecting a landing site for NASA’s Mars 2020 rover, says that these kinds of breccia blocks are present in at least two of the sites NASA is considering: Northeast Syrtis Major and Midway.
“The mission of the 2020 rover is to look for the signs of past life,” Mustard said. “Areas where you may have remnants of this underground habitable zone — which may have been the largest habitable zone on the planet — seem like a good place to target.”
Other coauthors on the paper were Barbara Sherwood Lollar, Mike Bramble, Kevin Cannon, Ashley Palumbo and Ana-Catalina Plesa. The research was supported by the Mars Data Analysis Program (MDAP) (grant 522723), the Natural Sciences and Engineering Research Council of Canada (grant 494812) and a Brown University graduate fellowship.
Mosaico de  visto por la , 22 de febrero de 1980. 
En un nuevo estudio anunciado el lunes pasado y disponible en el volumen actual de ''Earth and Planetary Science Letters'', un equipo internacional liderado por investigadores de la  de Estados Unidos afirmó que  tuvo alguna vez la cantidad adecuada de  y la temperatura correcta para dar sustento a formas simples de vida, aunque no en su superficie. Hace tiempo, la capa subterránea y rocosa de Marte poseyó suficiente agua y  para mantener los mismos tipos de comunidades microbianas observadas en la .

"Con base en cálculos químicos y de física básica, demostramos que la antigua subsuperficie marciana probablemente tuvo suficiente hidrógeno disuelto para proporcionar una  global en el subsuelo", reportó Jesse Tarnas, autor principal y estudiante de posgrado en Brown. El artículo no afirma que existió , sino que es muy probable que las condiciones adecuadas para la vida hayan perdurado por un tiempo prolongado. Esta zona habitable, localizada por debajo de la entonces congelada superficie marciana, habría alcanzado varios kilómetros dentro de la superficie, potencialmente protegida por el hielo.

El estudio mostró que, durante el periodo Noachiano (entre 4100 y 3700 millones de años atrás), la radiólisis, proceso por el que la radiación rompe las moléculas del agua, produjo suficiente  (H2) para permitir la vida de organismos microbianos mientras permanecieran dentro del área justo debajo de la . La concentración de hidrógeno en el agua subterránea podría haber variado entre aproximadamente 35 y 55  por litro, dependiendo de si el agua del antiguo Marte era caliente o fría, respectivamente. Incluso podría haber sido mayor si el medio de la subsuperficie contuvo suficiente sal. Los investigadores llegaron a este cálculo al establecer tres factores. 

Primero, revisaron los datos obtenidos por el espectrómetro de  abordo de la nave  de la . A partir de ellos dedujeron la cantidad de elementos radioactivos que habrían estado presentes en la corteza de Marte durante el periodo Noachiano y, por tanto, cuánta radiación habría estado disponible para separar las moléculas de agua y producir hidrógeno. Posteriormente, con base en los , determinaron cuánta agua subterránea habría existido. En tercer lugar, emplearon modelos climáticos y geotérmicos para precisar la cantidad de agua en estado líquido y a una temperatura adecuada para los seres vivos.

En ambientes subterráneos de la Tierra, los ecosistemas microbianos litoacutotróficos del subsuelo (SLiMEs, por sus siglas en inglés), los ecosistemas se sustentan en microbios que obtienen electrones de moléculas circundantes y no de plantas que aprovechan la luz solar por medio de la . El hidrógeno molecular es un  especialmente bueno. John Mustard, profesor en la Universidad Brown y uno de los autores del artículo, pertenece a un equipo que diseña la próxima misión del , programada para 2020. Mustard y Tarnas recomiendan que el rover estudie los sitios de colisión de meteoros, que podrían contener rocas excavadas de esta posible profundidad probablemente habitable y que podrían contener rastros de vida antigua.