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A huge discovery just 39 light years from Earth could totally change the future search for alien life.

Scientists have just spotted something absolutely incredible in our own celestial neighborhood. They’ve found a large super-Earth exoplanet called 1132b orbiting a red dwarf star just 39 light years away that they believe could have its own atmosphere, which could be a game-changer in the search for life.

Scientists figured this out by measuring subtle shifts in stellar light as the planet crosses over the red dwarf, using data from the European Southern Observatory’s telescope and the GROND imager to bolster their claims. It’s not quite the same as discovery life, but finding a planet with an atmosphere like Earth’s is truly a major accomplishment, as it’s something scientists have never found before, even though they’ve found plenty of planets.

It’s hard to determine whether this atmosphere has a chemical composition conducive to life, obviously, but it’s still a big step that could lead to discoveries of other planets with atmospheres. An atmosphere is important because it protects the surface and potential life forms from radiation from the sun.

A 2016 Harvard statement follows below.

The distant planet GJ 1132b intrigued astronomers when it was discovered last year. Located just 39 light-years from Earth, it might have an atmosphere despite being baked to a temperature of around 450 degrees Fahrenheit. But would that atmosphere be thick and soupy or thin and wispy? New research suggests the latter is much more likely.

Harvard astronomer Laura Schaefer (Harvard-Smithsonian Center for Astrophysics, or CfA) and her colleagues examined the question of what would happen to GJ 1132b over time if it began with a steamy, water-rich atmosphere.

Orbiting so close to its star, at a distance of just 1.4 million miles, the planet is flooded with ultraviolet or UV light. UV light breaks apart water molecules into hydrogen and oxygen, both of which then can be lost into space. However, since hydrogen is lighter it escapes more readily, while oxygen lingers behind.

“On cooler planets, oxygen could be a sign of alien life and habitability. But on a hot planet like GJ 1132b, it’s a sign of the exact opposite – a planet that’s being baked and sterilized,” said Schaefer.

Since water vapor is a greenhouse gas, the planet would have a strong greenhouse effect, amplifying the star’s already intense heat. As a result, its surface could stay molten for millions of years.

A “magma ocean” would interact with the atmosphere, absorbing some of the oxygen, but how much? Only about one-tenth, according to the model created by Schaefer and her colleagues. Most of the remaining 90 percent of leftover oxygen streams off into space, however some might linger.

“This planet might be the first time we detect oxygen on a rocky planet outside the solar system,” said co-author Robin Wordsworth (Harvard Paulson School of Engineering and Applied Sciences).

If any oxygen does still cling to GJ 1132b, next-generation telescopes like the Giant Magellan Telescope and James Webb Space Telescope may be able to detect and analyze it.

The magma ocean-atmosphere model could help scientists solve the puzzle of how Venus evolved over time. Venus probably began with Earthlike amounts of water, which would have been broken apart by sunlight. Yet it shows few signs of lingering oxygen. The missing oxygen problem continues to baffle astronomers.

Schaefer predicts that their model also will provide insights into other, similar exoplanets. For example, the system TRAPPIST-1 contains three planets that may lie in the habitable zone. Since they are cooler than GJ 1132b, they have a better chance of retaining an atmosphere.

The following is from the abstract of the most recent paper.

Detecting the atmospheres of low-mass low-temperature exoplanets is a high-priority goal on the path to ultimately detect biosignatures in the atmospheres of habitable exoplanets. High-precision HST observations of several super-Earths with equilibrium temperatures below 1000K have to date all resulted in featureless transmission spectra, which have been suggested to be due to high-altitude clouds. We report the detection of an atmospheric feature in the atmosphere of a 1.6 Mearth transiting exoplanet, GJ 1132b, with an equilibrium temperature of ~600K and orbiting a nearby M dwarf. We present observations of nine transits of the planet obtained simultaneously in the griz and JHK passbands. We find an average radius of 1.43 +/- 0.16 Rearth for the planet, averaged over all the passbands, and a radius of 0.255 +/- 0.023 Rsun for the star, both of which are significantly greater than previously found. The planet radius can be decomposed into a “surface radius” at ~1.375 Rearth overlaid by atmospheric features which increase the observed radius in the z and K bands. The z-band radius is 4sigma higher than the continuum, suggesting a strong detection of an atmosphere. We deploy a suite of tests to verify the reliability of the transmission spectrum, which are greatly helped by the existence of repeat observations. The large z-band transit depth indicates strong opacity from H2O and/or CH4 or a hitherto unconsidered opacity. A surface radius of 1.375 +/- 0.16 Rearth allows for a wide range of interior compositions ranging from a nearly Earth-like rocky interior, with ~70% silicate and ~30% Fe, to a substantially H2O-rich water world.
http://www.morningticker.com/2017/04/shocking-discovery-near-our-solar
-system-floors-scientists/

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