SERIES OF STEPS
The new equation breaks down the process of abiogenesis—the formation of life from nonliving components—into a series of simpler factors. Those factors incorporate the planet’s conditions, the ingredients needed to form life and the likelihood of those ingredients getting into the right configuration for life to emerge. As with the Drake equation, each of the terms is straightforward to describe, but each hides additional complexity and room for new research.
The formula is …
<N abiogenesis="" (t)=""> = Nb . 1/ <no> . fc . Pa . t
The average number of origin-of-life events for a given planet = (number of building blocks on planet) × 1/(average number of building blocks needed per “organism”) × (availability of building blocks during time t) × (probability of assembly in a given time) × time. Credit: Caleb Scharf and Lee Cronin
On the left, the equation considers the average (mean) expected number of origin-of-life events for a given planet. To get there, it takes into account the number of potential “building blocks” for life on the planet, the average number of building blocks needed to create a living system, the availability of those building blocks during a given time and the probability of that assembly happening during that time.
On Earth, building blocks for life take the form of amino acids, lipids and certain essential metals. Somewhere else, though, an entirely different set of ingredients could create enough complexity to form life—the equation doesn’t assume any specific set is necessary.
“We’re being kind of sneaky,” Scharf said. “I think it’s one of the beautiful things about it: If you write the equation this way, you don’t necessarily have to worry about all the fine, fine details, but what you do do is, you start to break open the factors that you might be able to put some numbers to.”
For instance, if you know the size of a planet and its composition, you can begin to estimate how many potential building blocks for life there are on the planet. To calculate whether those building blocks are actually available to form life, you’d have to know more about the conditions on the planet, such as its temperature, which could render some of the blocks unusable or inaccessible. For example, these blocks could be unusable or inaccessible if they’re always in gaseous form or if water is not readily available—although future research might show that life could emerge in more scenarios than scientists currently know about.
In that way, the equation “links where people in exoplanetary science may actually begin to get some data, on the size of planets, the composition, and so on, to the piece that we still don’t really understand but we know must have some kind of probability of happening”: how it is that life first begins, Scharf said.
A TRILLION TEST TUBES
The value Pa, which is the probability that life will assemble out of those particular building blocks over a given time, is murkier—and much more interesting. If the value of Pa is very low, it’s extremely unlikely that life will form even when the ingredients are there—potentially explaining why humans haven’t yet happened to create life in the lab, even if scientists have used the right ingredients, Scharf said. But a planet-wide “lab” would increase the odds that life-creating events will occur.
“We might have to wait 100 million years for it to fall into place just in a test tube,” Scharf said. “Whereas on a planet scale, you’ve got a trillion test tubes—probably even more than that. It’s conceivable that, using this equation, playing these games, is hinting at a possible explanation for why we haven’t seen life miraculously appearing in our laboratories, that … there’s some subtle thing that has to happen that really doesn’t happen often.”
And if the scale is larger than planetary, Scharf said, that could further increase the likelihood of life forming. Early Earth and Mars, for example, were cultivating their own, separate chemistries, but the early solar system was chaotic; impacts with other solar system bodies could have resulted in material exchanges between the two planets. That would have led to even more “test tubes“—the chemical mixing could have allowed even more interactions to occur, potentially hitting the right combination, Scharf said.
If multiple planets exchange materials, it could lead to a sort of “chemical amplification could, in principle, be hugely important,” he said. “It could be all the difference between getting life to occur or not, especially when we’re dealing with such tiny, tiny probabilities on the microscopic scale of something going right,” he added.