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The Sciences

How to Build Aliens in the Lab

To find life on Earth, follow the water. But what about on other planets?

By Kiona N. SmithJune 26, 2019 5:00 PM
DSC-LA0719 01 oil droplets
(Credit: Derivative of “Oil Abstract, Alternate” by Tim Sackton)

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Earth is teeming with life — and water makes it all possible. But elsewhere in the cosmos, life might be built from different chemicals that dissolve and assemble in some other liquid: perhaps methane, kerosene, or even chloroform. For now, it’s not feasible for humans to set foot on those worlds and see what’s there, but researchers are exploring some possibilities in labs here on Earth. 

The idea of a strange parallel form of life, whose cells do the same basic things as ours using a completely different chemistry, isn’t new to science. Isaac Asimov first broached the subject in his 1962 essay “Not as We Know It: The Chemistry of Life.” And in 2004, the same year the Cassini spacecraft entered Saturn’s orbit, biochemist Steven Benner proposed in a paper in Current Opinion in Biological Chemistry that on a world like Saturn’s moon Titan, life might use liquid hydrocarbons as a solvent (a liquid that can dissolve other substances), the way water is used on Earth.

With new exoplanets joining the roster of known worlds every day, it’s likely that some of them have oceans (or at least warm puddles) of hexane, ethers, chloroform, or other exotic liquids that might serve as the basis for life as we don’t yet know it. 

Gathering the Pieces

In such alien oceans, the chemistry of life on Earth just wouldn’t work. Water is a polar molecule; its oxygen end has a slight negative charge, while its hydrogen end has a slight positive charge. Those charges affect the kinds of chemical bonds that can happen in water. The structure of molecules like DNA and proteins depends on water’s polar hydrogen bonds.

Most hydrocarbons (compounds made of hydrogen and carbon, such as methane and ethane) are nonpolar — there’s no charge at either end of the molecule. So it’s impossible to form the same kinds of bonds in these chemicals as in water. That’s why if you want to create life in Titan’s methane lakes, you’re going to have use a different set of building blocks altogether.

Chemists and biologists from across the United States — led by organic chemist Paul Bracher at Saint Louis University and funded by a three-year grant from the National Science Foundation — have formed a team to explore what the building blocks of truly alien life might be made of. Using computer simulations and hands-on lab work, they’re exploring how molecules bond in liquid hydrocarbons such as hexane, ethers, and chloroform. Their work falls right on the border between sciences, where chemistry becomes biology. 

“It’s like trying to build a car in your backyard out of lawn mower parts, versus having the Maserati factory build a supercar. Life as we know it is the supercar, and we are trying to hack together something that looks like it, out of a different set of parts, to see what we can learn about putting it together,” says Chris Butch of the Earth Life Science Institute. Butch, a computational chemist, will use digital simulations to help understand the details of the chemistry his colleagues will observe in the lab.

So which parts do you need to scavenge from your metaphorical lawn mower to build something that looks like a Maserati? The two most important components you need to build a cell are a molecule that can carry information, like DNA or RNA, and some combination of molecules that can form a membrane. The team’s goal is to see what other molecules might interact in ways that mimic the basic processes of life, but using different machinery. To accomplish this, they’re using shorter, simpler versions of the complex polymers that come together to carry out the chemical processes of life. Their experiments include coaxing the building blocks of life as we know it into oil “membranes,” modifying the structure of DNA and RNA, and creating their own genetic molecules from scratch. 

The Boundaries of Life

Picture an alien sea, where droplets of hydrocarbons float suspended in water. “As long as there are waves crashing on a shore, or some kind of weather, then if oil floats to the top, it’s going to be consistently mixed into the water phase in a droplet form,” says Connecticut State University biochemist Sarah Maurer, whose area of interest is cell membranes and containers.

If you want life, you’ve got to contain all the chemistry that happens in a cell, separating it from the outside environment. In the cells of every living thing on Earth, oily membranes provide that container. Membranes play an important role in powering the cell’s functions; they’re involved in the chemical reactions that allow plant and animal cells to produce energy. And those chemical reactions depend on the basic fact that the membrane is an oily structure interacting with a watery cell inside of it.

DSC-LA0719 03 hydrothermal vents
Hydrothermal vents form when seawater enters fissures in the ocean floor, is heated by the hot magma beneath, and boils back up through the cracks. The vents are often teeming with life, including microorganisms that convert minerals and other chemicals into energy. Such vents could provide a hospitable environment for life elsewhere in the universe as well. (Credit: Pacific Ring of Fire 2004 Expedition/NOAA Office of Ocean Exploration/Bob Embley, NOAA PMEL)

But the team won’t be using methane or ethane, the liquid hydrocarbons that fill Titan’s lakes, for its experiments. Those substances are liquids only when exposed to incredibly cold temperatures like those found on Titan’s surface, not those usually found in chemistry labs on Earth. Instead, the researchers are sticking with hydrocarbons like hexane, which is a good analogue for methane but stays in liquid form at room temperature, as well as chloroform and others. The boundaries of these droplets — where oil meets water — serve as a simple analogue for the early development of cell membranes. 

Maurer’s experiments won’t produce anything you could reasonably call a cell membrane, but they just might shed some light on the basic chemistry that can occur at the boundary of oil and water.

“We kind of need this oil phase in our cells to drive energy generation,” says Maurer, “and so it makes sense that you could, in some way, make an oil droplet have functionality that’s similar to an aqueous cell by using the surface of the oil droplet to drive reactions.”

This team isn’t the first to think about the idea of alien cell membranes. In a 2015 Science Advances paper, planetary scientist Jonathan Lunine of Cornell University, working with two chemical engineers (none of the three is involved in Bracher’s project), used digital modeling to determine that vinyl cyanide — a compound made of nitrogen, carbon, and hydrogen, also called acrylonitrile — could theoretically form rudimentary barriers in methane. 

“To call it a membrane would be to give it too much credit, but it’s at least something [that] kind of encloses and could create a kind of container,” Lunine says. In 2016, he and chemist Martin Rahm (then at Cornell, and currently at Chalmers University of Technology) digitally modeled compounds of hydrogen cyanide, showing they could bind together to form sheets and rolls in a simulated hydrocarbon sea. And then in 2017, another paper published in Science Advances announced the discovery of evidence for vinyl cyanide on Titan, marking a step forward in the search for molecules capable of supporting life on the distant moon.

SIDEBAR: Water and Life

Water is a polar molecule consisting of two hydrogen atoms and one oxygen atom. The oxygen atom in one water molecule tends to be attracted to a hydrogen atom in a neighboring water molecule, and vice versa, giving water its unique properties. These properties are essential for the chemistry of life on Earth.

For the chemical processes of life to happen, molecules must be able to connect, separate, and reconnect in specific ways. Think about DNA replication, for instance. The base pairs that make up the genetic code bond when their negatively charged hydrogen atoms are attracted to positively charged atoms in another nucleotide. Those bonds hold the two strands of the double helix together, but because the hydrogen in water molecules also bonds this way, it’s relatively easy for enzymes to “unzip” the double helix for replication, then bind the two new strands together again. 

However, the molecules of life won’t work in hydrocarbons the way they do in water. That’s because most hydrocarbons don’t tend to form hydrogen bonds. But it’s possible that other molecules floating around in a lake of methane could bond and react in ways that let them carry out the basic chemical functions of life. 

Back on Earth, Maurer’s experiment is simple. She and her colleagues want to see if they can get compounds to cross that oil-water boundary at all. They’ll start with the familiar genetic molecules DNA and RNA, but these will need some help crossing over. The backbone of nucleic acids like DNA and RNA is a chain of smaller molecules called phosphates, which have a slight negative charge. But negatively charged molecules are less likely to interact with oil than with water, so our familiar genetic molecules may not move into the oil droplets very readily. 

However, other molecules might pair with the nucleic acids and help sneak them across the boundary. Biochemical companies have developed molecules called transection agents, which help move nucleic acids through membranes, and one of the team’s goals is to look for combinations of DNA and transection agents that can migrate into the hydrocarbon droplets and remain stable.

“That’s basically saying, ‘Can we tease our biology into functioning at some level in these strange environments?’ ” says Georgia Tech molecular biologist Loren Williams, who is especially interested in how polymers behave in liquid chloroform.

The team also wants to swap out the nucleic acids’ phosphorus for silicon, creating a molecule that dissolves more easily in hydrocarbons. They also plan to test an alternative genetic molecule using so-called “non-canonical nucleotides,” substituting other chemicals for the familiar adenine, thymine, guanine, and cytosine. 

And then there are the really exotic ideas. Bracher’s group at Saint Louis University is working on a completely synthetic molecule that will work like DNA but be made of completely different molecules that form a different type of chemical bond. Instead of the hydrogen bonds that link DNA base pairs, Bracher’s version would use base pairs that share molecules called thioesters. 

DSC-LA0719 04 Titan surface
Ice made of hydrocarbons, rather than water, floats on the surface of a lake on Titan in this artist’s concept. Using Cassini data, scientists have confirmed the presence of ethane in lakes on the cloudy moon, which contains the only known surface liquid in the solar system, aside from Earth. (Credit: NASA/JPL-Caltech/USGS)

There’s reason to think it could work. In 2015, Benner, who founded the Foundation for Applied Molecular Evolution in 2001 and is not involved in Bracher’s project, tested a version of DNA with an ether backbone in a solvent of kerosene. He found that this combination wouldn’t work to form life on a place nearly as cold as Titan, but on some so-called “warm Titan” exoplanets, it might be a good option. 

“Given how many exoplanets we’re finding around distant stars, chances are there are going to be other worlds like Titan that could have something interesting going on,” says Bracher.

Playing with the Building Blocks

From there, one of the next steps is to see how the building blocks of alien life might evolve. Chemistry is subject to natural selection: Systems and structures that are better at replicating themselves tend to outcompete others. That process may be how molecular systems evolve toward greater complexity, eventually producing the specialized systems of molecules and reactions that form cells.

Michael Travisano, an evolutionary biologist with a background in astrophysics, plans to simulate that process on the team’s array of molecules. In this case, selection will be based on whether or not a molecule, or set of molecules, can move back and forth across the barrier between oil and water. The results will tell the team which types of molecular structures or bonds are best suited to the simulated environment. “That’s sort of the stuff of natural selection,” says Travisano. 

Maurer is interested in whether the molecules will be able to support basic chemical reactions inside the hydrocarbon droplets. The base pairs in DNA, for example, “recognize” each other by finding which base “fits” well enough to form a bond with another — adenine to thymine and cytosine to guanine. If alternative versions of those molecules can recognize each other and form bonds in other solvents, that’s an encouraging sign that basic biochemistry could be possible in alien seas.

Of course, such a system is not even close to a working cell, and it would still be missing some important building blocks for life. In cells on Earth, proteins called enzymes help reactions happen fast enough to be useful. The team doesn’t have alternative enzymes to go with its membranes and genetic material, though.

“We have backbones we’re making, and we’re going to have base pairs, but the problem is we don’t have an enzyme that will replicate it because the backbone chemistry is not the same,” says Williams. “We really have to start at a more basic chemical level and try to work forward as far as we can.”

Looking for Alien Life

“A lot of this is going to be exploratory science,” says Butch. “I think it’s a really cool idea for just pushing the boundaries of what our assumptions about the transition from chemistry to biology actually looks like.” In other words, no synthetic alien organism is going to crawl out of the test tube. 

“I don’t think that we’re going to discover the origin of life in the next three years or that we’re going to figure out exactly how life could develop [on other worlds] in nonpolar solvents in the next three years,” says Bracher. “What this project is really about is starting to figure out how the rules of the game might change from life as we know it in water to some new form of life that works in oil and nonpolar solvents, whether here on Earth or on distant planets.”

DSC-LA0719 05 Europa, Iapetus, Enceladus, Triton
While Titan is a major focus of the search for life in the solar system, there are other icy worlds where life might thrive: Europa, Iapetus, Enceladus, and Triton are among the candidates that could host life. (Credits, from top: NASA/JPL/DLR; NASA/JPL/Space Science Institute (2); NASA/A. Tayfun Oner)

What that will tell us, Bracher and his colleagues hope, is whether the precursors of biochemistry might be able to take shape in an ocean made of something other than water. If the answer is yes, then that means our current search for life has a huge blind spot.

“Our problem with looking for life is that we are looking for our life, largely. ‘Follow the water’ might find some life, but it might not find other kinds of life,” says Williams. By demonstrating that at least basic biochemistry can arise in other liquids, the team may help open new habitable zones, or at least keep some interesting places from being ruled out. 

The results could provide useful ideas about not only where, but how to look for life as we don’t know it. For instance, Earth’s atmosphere is rich in oxygen because plants and cyanobacteria release it as a product of photosynthesis. If Bracher and his team can identify potential molecular building blocks for alien cells, they might also be able to predict which chemicals those cells breathe out into the atmosphere of their home world. 

DSC-LA0719 08 titan infograph
Complex Chemistry on Titan:Titan’s thick haze at lower altitudes is the result of chemical reactions between incoming energy (sunlight and energetic particles from Saturn) and molecules in the moon’s upper atmosphere such as nitrogen and methane. These reactions — which incorporate elements such as carbon, hydrogen, and nitrogen — create lighter carbon chain molecules (middle box) that eventually form larger organic molecules that scientists believe sink to the moon’s surface. However, not all of these reactions are known or understood yet, and the signs of life may be buried within data yet to be analyzed from the Cassini mission. — Alison Klesman (Image credit: Roen Kelly/DISCOVER, after ESA)

In 2005, astrobiologist Chris McKay worked out how organisms on Titan might metabolize acetylene or ethane, and realized that they’d leave a noticeable signature in Titan’s atmosphere — which, it turns out, may actually be present, though the evidence isn’t yet clear. The Cassini and Huygens probes observed both the lack of an ethane layer around the moon and a lack of acetylene on its surface, though both were expected. The depletion of these substances could be due to a “biological sink” — life consuming them and leading to their absence.

This kind of research can guide how we comb through the reams of data already in hand from missions like Cassini, says Lunine. “No one’s really looked through the data very carefully for them, so one can go back now, seeing that they have these interesting properties, and really try to dig through the data to see if it’s actually there,” he says.

Ultimately, tinkering with alien biochemistry is a step into the unknown, and although the team has some ideas about what to expect, they’re also prepared for surprises along the way.

“My expectation is that a lot of things that we think are challenges to life will turn out to not be, and things we don’t realize are difficulties will all of a sudden [turn out to] be incredibly hard,” says Travisano. “It will be interesting what doesn’t work and what does. Expect surprises.”   


Kiona N. Smith is a science and technology journalist, science history blogger, and science correspondent for Ars Technica.

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