Enceladus’ sea floor has hydrothermal vents like ours

Authored by astronomy.com and submitted by Andromeda321

In 1977, a group of marine researchers discovered something they’d only before theorized: cracks in the ocean floor releasing heat, warming up (and often boiling) the ocean around it. They also found mollusks in them, and subsequent vents have yielded heat resistant microbes, giant tube worms, and more fantastic creatures living in what are essentially small, underwater volcanoes.

Now, NASA has announced that they have indirect evidence for hydrothermal vents beyond Earth. In its encounters with Saturn’s moon Enceladus, the Cassini craft found chemicals associated with these events. The results were published today in Science. It adds to the body of evidence that Enceladus could be ripe for life.

"Enceladus is too small to have retained the hydrogen from when it formed, so the hydrogen we see today is coming from inside Enceladus," Linda Spilker, project scientist on the Cassini mission, said in a press conference.

Enceladus, which is a tiny moon, took Cassini researchers by surprise when they discovered what seemed to be geysers of water emitting from the south pole in 2005. Subsequent investigations built a picture of the origin: liquid water under the surface of Enceladus, which led to the idea of an entire ocean under the surface. The heating mechanism, to date, has not been discovered.

The Ion Neutral Mass Spectrometer on the craft made the observation of molecular hydrogen in the ejecta from these geysers. According to principal investigator Hunter Waite of the Southwest Research Institute and his co-investigators, the source almost certainly has to be hydrothermal vents at Enceladus’ sea floor. This means there’s plenty of geological activity, increasing the chances for life.

Indeed, researchers published a paper last year suggesting that hydrothermal vents were the source of life on Earth, where chemical reactions fed these early microbes. If that’s the case on Enceladus, the ocean may have microbial life at the very least.

"The hydrogen could be a potential source of chemical energy for any microbes living in Enceladus' ocean," Spilker says.

Of course, it may be years or even decades until we know for sure — in September, NASA will intentionally crash Cassini into Saturn to make sure it doesn’t crash land into Titan or Enceladus and accidentally contaminate either potentially habitable moon with Earth bacteria.

All_of_the on July 7th, 2017 at 19:43 UTC »

Meanwhile, on Enceladus:

"Earth's oceans appear to have hydrothermal vents, similar to those on Enceladus."

trjones1 on July 7th, 2017 at 16:14 UTC »

I don't even care about Mars at this point, I just want a massive push to look for life on Enceladus.

Andromeda321 on July 7th, 2017 at 15:30 UTC »

Astronomer here! For those who are unaware, even indirect evidence of such hydrothermal vents like those in this paper can have huge implications for life on Enceladus. This is because on Earth we know there is life around our own hydrothermal vents, due to the energy they exert, so that definitely puts a huge plus in the "potential microbial life at least" column. Even more than we have for Europa, arguably, for which we do not yet have any evidence of hydrothermal vents, direct or indirect.

Unfortunately, we don't know what causes the heat on Enceladus to exist that causes liquid water to be present, and we are unlikely to know more about this mystery or its potential life in the future because there are no future missions planned after Cassini crashes into Saturn in a few months. :( So be prepared for at least a decade of speculation, likely more...

Edit: many are confusing Enceladus, which orbits Saturn, and Europa, orbiting Jupiter, and asking if the heat in Enceladus is from tidal effects. The answer is no- while some certainly is, it turns out Enceladus has more heat than expected if it was just tidal forces like Europa's case. Read about it here- https://www.nasa.gov/mission_pages/cassini/whycassini/cassini20110307.html