Rock and Roil: Meteorites Hitting Early Earth's Oceans May Have Helped Spawn Life

Did heat, pressure and carbon from meteorite impacts create biological precursors?















Share on Tumblr



SPICE FOR THE SOUP? A new study generates biological precursors by simulating the impact of carbon-bearing meteorites into early Earth's oceans. Image: ©iStockphoto.com/thecarlinco

  • What a Plant Knows

    How does a Venus flytrap know when to snap shut? Can it actually feel an insect’s tiny, spindly legs? And how do cherry blossoms know when to bloom? Can they...

    Read More »

Many theories about the origins of life on Earth posit that prebiotic compounds may have arrived from outer space on asteroids or comets. But a new study suggests that extreme chemical reactions fired up by meteorite impacts may have jump-started life in the early oceans, rather than delivering its building blocks preformed. Meteorites striking the primordial oceans, the paper's authors say, could have supplied significant amounts of carbon, critical to life, and created a sort of chemical pressure cooker by the force of their impacts to synthesize the foundations of biological molecules.

The researchers report in Nature Geoscience today that they replicated the impact of a chondrite, a common type of meteorite, striking the ocean at about 1.25 miles (two kilometers) per second. The team did this by subjecting chemical constituents of chondrites (iron, nickel and carbon), as well as water and nitrogen, believed to be plentiful in the early atmosphere, to shock compression. The resulting pressures and temperatures, which likely exceeded 5,000 degrees Fahrenheit (2,760 degrees Celsius), yielded a variety of organic (carbon-based) compounds, such as fatty acids and amines. And when ammonia, which a previous study showed impacts could produce, was added to the starting mix, the experiment also yielded glycine (a simple amino acid).

Study co-author Toshimori Sekine, a researcher at the National Institute for Materials Science in Tsukuba, Japan, says he was surprised by the output from the experiment, adding that "there are many additional molecules we found but didn't analyze yet." Lead author Yoshihiro Furukawa, a PhD candidate at Tohoku University in Sendai, Japan, says that in light of the results, "we can say those ocean impact events [were] very effective processes for the production of various biomolecules on the early Earth." He is quick to note, though, that it is unclear how much or how many of these biomolecules would be needed to initiate life.

To ensure the organic compounds were produced by the shock of the simulated impact (and not outside sources), Furukawa's group used carbon 13, a rare isotope of the element, in the meteorite proxy. The fact that the detected molecules were enriched with carbon 13 rather than the more common carbon 12, the authors say, rules out the possibility of contamination.

"It's neat to show that you could harness the energy of impacts to create organic bonds," says Jennifer Blank, an astrobiologist at the SETI Institute in Mountain View, Calif. But she fears that theories of life's origin may never move beyond the hypothetical. "As someone in the general field, one of the frustrations, of course, is that we're never going to know the answer," she says. "But as another mechanism for contributing to the inventory of organic compounds, this is cool."

Astronomer Donald Brownlee of the University of Washington concurs, noting that while most theories propose that organic molecules arrived from space or were formed by Earthly processes, "it is interesting to consider that they could be made here because material is falling in from space." At the same time, Brownlee wonders whether a meteorite large and powerful enough to penetrate the atmosphere and strike the ocean at high speed might preclude the formation of organics. "If the body is too large," he says, "generated materials are probably destroyed by impact processes."

The study by Sekine, Furukawa and their colleagues is a kind of oceanic, kinetic-impact analogue to the Miller–Urey experiment, a legendary 1953 demonstration by the late chemist, Stanley Miller of the University of Chicago, who, along with colleague Harold Urey, showed that an electric discharge applied to suspected components of the early atmosphere yielded a bounty of amino acids. In October, marine chemist Jeffrey Bada of the Scripps Institution of Oceanography in La Jolla, Calif., and his colleagues published a reanalysis of some of Miller's samples from a different experimental setup. Bada and his collaborators found even more organic material than Miller himself had announced—22 amino acids and five amines.

Sekine cautions that the meteorite-impact theory is not ready to supplant the vaunted Miller–Urey experiment. He says that the new study's results merely "open up a door to discuss the possibility" of meteorite impacts as an originator for life on Earth. "We do need to test the possibility for the formation of more complicated amino acids," he says.



8 Comments

Add Comment
View
  1. 1. hotblack 09:32 PM 12/7/08

    Nope. Jesus did it.

    Reply | Report Abuse | Link to this
  2. 2. kat in reply to hotblack 12:07 AM 12/8/08

    r u seriously going to say that

    Reply | Report Abuse | Link to this
  3. 3. wchoi 12:00 PM 12/8/08

    Hi

    Reply | Report Abuse | Link to this
  4. 4. redfoxone 05:49 PM 12/8/08

    Yup, its all in the Bible! good reading!

    www.anonymity.at.tc

    Reply | Report Abuse | Link to this
  5. 5. cd19 09:52 AM 12/9/08

    And God saw that it was good. What fools to think everything developed itself. Git offa yore hosses named Vanity. God made y'all too, and the hosses. I can prove mine. How 'bout yourn? Signed cd19@verizon.net

    Reply | Report Abuse | Link to this
  6. 6. nfiertel 09:35 PM 12/9/08

    The question as to whether the meteorite impact would sterilise the materials formed breaking them back down to simple compounds from complex ones created during the initial imapact presumes I think that we are dealing with an atomsphere of similar density to that of present day earth which was not at all the case. No doubt, the atmosphere of the earth was very dense wtih carbon dioxide, non organically produced methane and nitrogen and no oxygen at all in its free or molecuiar form. The high atmospheric density I suggest would affect the arrival velocity of any meteor resulting in a teminal velocity and thus the possibility that organics thus produced would survive in part due to the energy dissipating effects of high density atmospheric shock waves created during the passage to the oceans or outer crust. Considering the billions of hits the earth would sustain during its formation, even inefficient production of organics along with electrostatic events such as lightning already shown to produce aminos adds simply one more scenario for the production of such precursors to simple life. The fact is..life does exist here and likely billions of other places as this scenario of meteor/lightning is a kind of universal mechanical method for planetary production, atmospheric evolution and so forth. What is needed is just the right arrangement vis a vis planetary orbit and solar radiation allowing liquid water to settle in a stable pattern on that planet and throw in a billion or so years and anything that can happen is likely to happen. Add a few billion more years and one might find some life form who thinks that all of this happened because some mythic spirit waved a wand...or maybe another planet would have a more intelligent life structure that can see that such an idea is silly beyond discussion.

    Reply | Report Abuse | Link to this
  7. 7. fred 12:24 AM 12/13/08

    This is in many ways similar to the Miller-Urey experiment in that the "secret sauce" appears to be pressure and usable energy. In this case impact pressure, and in Miller-Urey, the instantaneous pressure gradients from the electrical spark.

    Jennifer Blank, who has a comment in the above article, performed a similar impact experiment at Lawrence-Livermore in 2002 creating peptides from The Miller-Urey amino acids. But then for some strange reason she walked away without continuing her experiments.

    That is, as far as know she never experimented further to see if, in the same manner (using impact pressure), she could create proteins from, say, Miller-Urey amino acids and the peptides she had previously created. And then from there, who knows what? It's a pity. I'm curious about it.

    Reply | Report Abuse | Link to this
  8. 8. bendezuprieto 10:24 PM 2/4/09

    It Is a very interesting hypotesis, but be very dificult if not imposible to proove.

    Reply | Report Abuse | Link to this
Leave this field empty

Add a Comment

You must sign in or register as a ScientificAmerican.com member to submit a comment.
Click one of the buttons below to register using an existing Social Account.

More from Scientific American

See what we're tweeting about

Scientific American Editors

More »

Free Newsletters


Get the best from Scientific American in your inbox

Solve Innovation Challenges

Powered By: Innocentive

  SA Digital
  SA Digital

Science Jobs of the Week

Email this Article

Rock and Roil: Meteorites Hitting Early Earth's Oceans May Have Helped Spawn Life

X
Scientific American Magazine

Subscribe Today

Save 66% off the cover price and get a free gift!

Learn More >>

X

Please Log In

Forgot: Password

X

Account Linking

Welcome, . Do you have an existing ScientificAmerican.com account?

Yes, please link my existing account with for quick, secure access.



Forgot Password?

No, I would like to create a new account with my profile information.

Create Account
X

Report Abuse

Are you sure?

X

Institutional Access

It has been identified that the institution you are trying to access this article from has institutional site license access to Scientific American on nature.com. To access this article in its entirety through site license access, click below.

Site license access
X

Error

X

Share this Article

X