Mars 2023: Inhabitants Wanted
Mars One will establish a permanent human settlement on Mars. We invite you to participate by sharing our vision with your friends, and, perhaps, by becoming the next Mars astronaut yourself.

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lagomblr:

amazing: the space we live in

(via andromeda1023)

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We are all stardust - and now we might be starting to be able to tell which star. 

“Sediment in a deep-sea core may hold radioactive iron spewed by a distant supernova 2.2 million years ago and preserved in the fossilized remains of iron-loving bacteria. If confirmed, the iron traces would be the first biological signature of a specific exploding star.” 

http://www.nature.com/news/supernova-left-its-mark-in-ancient-bacteria-1.12797 

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weareallstarstuff:

Cassiopeia

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hotpielookedlikehotpie:

all these years, all these memories, there was you. you pull me through time.

(via annadraconida)

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GAS CLOUD BEING SUCKED INTO THE MILKY WAY’S BLACK HOLE

Like other galaxies, the Milky Way has at its centre a black hole, known as Sagittarius A* (SgrA*). This black hole has the mass of four million solar masses. A cloud of ionised gas and dust was spotted earlier this year falling towards SgrA*. At the time, it was suggested that this cloud formed when gas streaming from two nearby stars collid
ed. However new research suggests this cloud might be the visible trail of a planet-forming disk which surrounds a young, low-mass star; this disc will be devoured by the black hole before it can evolve into a solar system.

Modelling work by Ruth Murray-Clay and Avi Loeb of the Harvard-Smithsonian Centre for Astrophysics in Cambridge, Massachusetts suggests that planets can form within the powerful gravitational field of a giant black hole. They investigated whether the cloud’s mixture of gas and ionised dust might come from a planet-forming disk surrounding a single young star. Murray-Clay and Loeb’s model showed that gravitational interactions dislodged a young, low-mass star orbiting near the ring’s inner edge. This star, which is now heading for Sagittarius A* in an elliptical orbit, is too faint to be detected. The proto-planetary dust cloud is being disrupted and the researchers are able to detect this debris. There is a ring of young stars that orbits at about 0.03 parsecs (one-tenth of a light year) from Sagittarius A*. Young stars have been observed throughout the Galaxy to often have planet-forming disks.

The main theoretical problem with the model is that Murray-Clay and Loeb’s calculations show that there is only a 0.1% chance a recently dislodged star would have the same orbit as the gas cloud. The model predicts that the gas cloud should have a dense core, which would show by an increase in brightness when the cloud gets closer to the black hole. If the model is shown to be correct, then it would suggest that young low mass stars that remain in the ring have disks that are strong enough to create planets.

Even though material could start falling onto the accretion disk surrounding the black hole by the end of 2013, it will take 20-40 years for all of it to be swallowed. The type of activity shown by the material falling in – whether as bursts, steady brightening, or a jet of hot gas - will give researchers insights into why Sagittarius A* is so inactive compared with other supermassive black holes. Although the planetary cloud is headed for destruction, the star is likely to survive, as the tidal forces from the black hole are strong enough to strip gas away from the star but not to pull the star itself apart.

The image is an artist’s impression of the protoplanetary disc being pulled into SgrA*.

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IS IT POSSIBLE FOR BASIC LIFE TO EXIST ON TITAN?

Saturn’s sixth and largest moon Titan has an average surface temperature of 94.2611Kelvin (-178.889°C or -290°F). Nitrogen comprises 98.4% of the atmosphere. Water is perpetually frozen; it can almost be considered a mineral. The seas of Titan are made up of hydrocarbons like methane, ethane, and some propane. The land masses are composed of frozen water and ammonia, which also exist in liquid states below Titan’s crust, much like silica and iron exist in liquid form below Earth’s crust.

Titan may still contain many of the components for life. Scientists have known for thirty years that complex carbon compounds called tholins exist on comets and in the atmosphere of the outer planets. In theory tholins could interact with water in a process called hydrolysis to produce complex molecules similar to those found on the early Earth; these compounds are called prebiotic. Titan is thought to be made mainly of ice; some of this ice may melt during meteor impacts or underground processes, producing ice volcanoes that eject lava made of ammonia mixed with water. Tholins could potentially react with this liquid water exposed by meteor impacts or ice volcanoes and produce probiotic organic molecules before the water freezes. Catherine Neish, a graduate student working on her doctorate in planetary science at the University of Arizona, showed that over a period of days, compounds similar to tholins can be hydrolysed at near-freezing temperatures. Liquid water exposed on Titan is believed to persist for hundreds to thousands of years.

Another study used data from NASA’s Cassini spacecraft. The craft detected large molecules at altitudes of some 965 km above Titan’s surface; but these molecules remained unidentified because of limitations of the craft’s instruments. Sarah Hörst, a graduate student in planetary science at the University of Arizona, led the research team that replicated the atmosphere of Titan in a large chamber at the temperatures present in the moon’s upper atmosphere. They used radio energy at a power level comparable to a moderately bright light bulb to simulate the sun’s ultraviolet light. UV light breaks up molecules like molecular nitrogen or carbon monoxide in Titan’s atmosphere, which leaves the individual atoms to choose different partners with which to form new molecules. The tiny aerosol particles produced by the experiment were run through a mass spectrometer, which is used to show the chemical formulae that make up the molecules within the aerosols. Hörst then ran these formulae past a roster of molecules known to be biologically important for life on Earth. She got 18 hits; 4 were nucleotides whose combinations form an organism’s genetic information encoded in DNA. It seemed it was more important for some form of oxygen to be present in the ingredients than it was for water to be present.

Billions of years ago Earth’s upper atmosphere may also have been the source for these “prebiotic” molecules, amino acids and the so-called nucleotide bases that make up DNA. Oxygen in early Earth history would have been in the form of carbon dioxide and carbon monoxide from volcanic activity, as well as from water released by volcanism and meteor and comet impacts. The oxygen on Titan seems to be coming from Enceladus, another moon of Saturn that is home to icy geysers that eject ice into space near its south pole. The water molecules ejected from Enceladus’ geysers can be carried great distances through Saturn’s system; some oxygen bearing minerals from this find their way to Titan.

It has been suggested by various scientists that Pitch Lake, in Trinidad and Tobago, is the closest thing on Earth to the kind of hydrocarbon lakes found on Saturn’s moon Titan. Single celled organisms like archaea and bacteria co-exist, thriving in the oxygen-free environment, eating hydrocarbons and respiring with metals: https://www.facebook.com/
photo.php?fbid=391607137567003&set=a.352867368107647.80532.352857924775258&type=3&theater.

-TEL

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