It's possible that life wiped itself out on Mars. It's not as crazy as it sounds.

While on Mars life did not evolve and persist.

Mars used to be warm and wet, according to evidence. Mars had surface water in the ancient Noachian Period. It doesn't mean that Mars was inhabited, but it is possible that it was.

A new study shows that early Mars may have been hospitable to organisms that thrive in extreme environments. There are places on the ocean floor where methane can be released and converted into a waste product. According to the study, methanogens may have lived underground on Mars.

The study is about early Mars habitability and global cooling by methanogens. It has been published in Nature Astronomy and is written by two people. The University of Arizona Department of Ecology and Evolutionary Biology has a professor named Ferrire and a former colleague named Sauterey.

According to the press release, the study shows that early Mars was likely to have been home to methanogenicbacteria. The authors aren't saying that life exists on the planet.

The paper states that the microbes would have thrived in the briny rock that protected them from the sun. The underground environment would allow methanogens to persist and provide a diffuse atmosphere.

H 2 and CO 2 can be found in hydrogenotrophic methanogens, which can be used to make methane as waste. This type of metabolism was the first to evolve on Earth. Its viability on early Mars has never been evaluated.

It has been this way until now.

There is a significant difference between ancient Mars and Earth. Most of the hydrogen on the planet is tied up in water. It was plentiful on Mars.

The methanogens needed hydrogen to thrive. It would have helped trap heat in the planet's atmosphere.

"Mars may have been a little cooler than Earth at the time, but not nearly as cold as it is now, with average temperatures most likely above the freezing point of water," said Ferrire.

While current Mars has been described as an ice cube covered in dust, we imagine early Mars as a rocky planet with a porous crust soaked in liquid water that likely formed lakes and rivers.

Water is either fresh or salt on the planet. It's possible that the distinction wasn't needed on Mars. All of the water was briny.

The models were used to evaluate methanogens on ancient Mars. They used a model of an ecological community of Earthlike microbes.

The researchers were able to predict if methanogen populations were able to survive. They were able to predict what the population would do to the environment.

Boris Sauterey, the paper's first author, said that after producing their model, they put it to work in the Martian crust.

We were able to evaluate the possibility of a Martian underground biosphere. How the chemistry of the Martian crust would have changed if a biosphere existed, and how the composition of the atmosphere would have changed.

"Our goal was to make a model of the Martian crust with its mix of rock and salty water, let gases from the atmosphere diffuse into the ground, and see if methanogens could live with that." The answer is that the microbes could have lived in the planet's crust.

How deep would you have to go to locate it? The researchers said it was a question of balance.

Mars' surface was still cold despite the atmosphere holding hydrogen and carbon. It is not as cold as modern Earth.

The deeper you go, the less hydrogen and carbon can be found.

The problem is that even on early Mars, it was still very cold on the surface.

The question is how deep the biology needs to go to find the right compromise between temperature and availability of molecule from the atmosphere to grow. The models we used found that the communities in the upper hundreds of meters were the most happy.

They would have been in the upper crust for a while. The communities would change the environment as they continued to take in hydrogen and carbon.

All of the above and below ground processes were modeled by the team. They predicted how the feedback would affect Mars.

As the methanogens changed the atmosphere's chemical makeup, they would initiate a global cooling. As the planet cooled, the briny water in the crust would freeze.

Mars' surface would eventually become uninhabitable due to cooling. The organisms would have been moved further underground as the planet cooled.

The atmosphere would be blocked from reaching those depths and the methanogens of energy would be starving.

Within a few tens or hundreds of thousands of years, the atmosphere of Mars would have been completely changed by biological activity. The planet's climate would have been cooled down if hydrogen were removed from the atmosphere.

An illustration shows the evolution of Martian ice coverage.
Each row represents the freezing point for a different type of brine. The orange color scale represents elevation. The superimposed white-shaded areas correspond to the surface ice's probability. (Boris Sauterey and Regis Ferrière)

What did the result look like? It's called extinction.

The problem these microbes would have faced is that Mars' atmosphere disappeared, so their energy source would have vanished, and they would have had to find an alternative source of energy.

They would have had to go much deeper into the ground. It's hard to say how long Mars would have been free of precipitation.

Future missions have the best chance of finding evidence of the planet's ancient life in certain places.

The authors say that the most productive populations would have been near the surface. Given the technology currently embarked on Martian rovers, the first few meters of the Martian crust are the most easy to explore.

Hellas Planitia is the best place to look for evidence of underground life because it is free of ice. The region is not suitable for rover exploration due to the powerful dust storms. If humans ever visit Mars, Hellas Planitia is an ideal location.

Life on ancient Mars has been around for a long time. The more interesting part of the research may be how early life changed. The development of more complex life occurred after that event.

Simple life forms were common on Early Earth. There was a new pathway to harness energy. Earth's first inhabitants thrived despite the lack of oxygen in the atmosphere. The cyanobacteria use photosynthesis for energy and produce oxygen as by-products.

The first tenants of Earth did not like oxygen. The mats created a region of oxygenated water around thebacteria, which they thrived in.

The oceans and atmosphere were oxygenated by cyanobacteria. Oxygen can't handle methanogens and Earth's other life forms.

The death of the primitive organisms comes close to being called an extinction by scientists. Modern-day Earth has environments that are oxygen-poor.

That was the world. There wasn't a new way to get energy on Mars. Mars became cold and lost its atmosphere. I wonder if Mars is dead now.

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There is a possibility that there is a source of hydrogen in Mars. The study showed that hydrogen could be obtained by breaking apart water molecule. Radiolysisysis has allowed isolated communities ofbacteria to persist for millions of years.

Life buried in the Earth's crust contains up to 400 times the carbon mass of humans, according to the Deep Carbon Observatory. The deepest part of the world's oceans is almost twice the volume of the world's deepest part.

Is there still life on Mars? There are methane detections that are not clear.

Many scientists believe that the Solar System's most likely place to harbor life is the planet Mars. I'm sorry, Europe. Maybe we will find it one day.

This article was published in the past. The original article is worth a read.