Aliens could be on Mars, most believe. Water on Mars has enough oxygen to theoretically support aerobic respiration, suggests a new research challenging traditional beliefs about the Red planet’s habitability. The new finding runs contrary to the current, accepted view of Mars and its potential for hosting habitable environments.
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NASA’s Jet Propulsion Laboratory (JPL) and scientists from the California Institute of Technology (Caltech) calculated that if liquid water exists on Mars, it could — under specific conditions — contain more oxygen than previously thought.
According to the study reported in the journal Nature Geoscience, the levels could even theoretically exceed the threshold needed to support simple aerobic life.
Researchers have long dismissed the idea that liquid water on Mars might be oxygenated, given that Mars’s atmosphere is about 160 times thinner than that of Earth and is mostly carbon dioxide.
“Oxygen is a key ingredient when determining the habitability of an environment, but it is relatively scarce on Mars,” said Woody Fischer, a Professor at Caltech.
For the study, the team developed a chemical model describing how oxygen dissolves in salty water at temperatures below the freezing point of water. Then, they examined the global climate of Mars and how it has changed over the past 20 million years.
“The briny water will also be abundant in calcium and magnesium which boost bone and metabolism,” said Vlada Stamenkovic from the JPL.
"Moreover, about 6.5 per cent of the total Martian surface area could support far higher dissolved oxygen concentrations, enabling aerobic oases sufficient to sustain the respiration demands of more complex multicellular organisms such as sponges," he added.
The team found that, at low-enough elevations (where the atmosphere is thickest) and at low-enough temperatures (where gases like oxygen have an easier time staying in a liquid solution), an unexpectedly high amount of oxygen could exist in the water — a value several orders of magnitude above the threshold needed for aerobic respiration in Earth’s oceans today.
Further, the locations of those regions have shifted as the tilt of Mars’s axis has changed over the past 20 million years. During that time, the highest oxygen solubility has occurred within the past five million years.
(With inputs from agencies)