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Home»Science»Plate tectonics could also be why Earth has life — and the important thing to discovering life elsewhere within the universe
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Plate tectonics could also be why Earth has life — and the important thing to discovering life elsewhere within the universe

VernoNewsBy VernoNewsOctober 4, 2025No Comments11 Mins Read
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Plate tectonics could also be why Earth has life — and the important thing to discovering life elsewhere within the universe
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Earth’s floor is a turbulent place. Mountains rise, continents merge and break up, and earthquakes shake the bottom. All of those processes outcome from plate tectonics, the motion of huge chunks of Earth’s crust.

This motion could also be why life exists right here. Earth is the one identified planet with plate tectonics and the one identified planet with life. Most scientists assume that is not a coincidence. By dragging large chunks of crust into the mantle, Earth’s center layer, plate tectonics pulls carbon from the planet’s floor and ambiance, stabilizing the local weather. It additionally pushes life-fostering minerals and molecules towards the floor. All of these elements add as much as a spot the place life thrives from ocean abysses to towering peaks.

However researchers do not know why or when plate tectonics began, making it laborious to find out how important this course of was to the evolution and diversification of life. Some assume plate motion fired up as little as 700 million years in the past, when easy multicellular life already existed. Others consider solely single-celled organisms reigned when Earth’s plates first cracked aside.


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The truth is, as new strategies enable scientists to look ever-deeper into the previous, some are actually arguing that plate tectonics emerged very quickly after Earth’s formation — maybe predating life itself. If this speculation is true, it could counsel that even essentially the most primitive life developed on an energetic planet — and meaning plate tectonics may very well be a necessary ingredient within the seek for alien life.

“The one means we are able to reliably see a long-term historical past is on our personal planet,” stated Jesse Reimink, a geoscientist who research early Earth historical past at The Pennsylvania State College. “We actually want to grasp the life cycle of a planetary physique earlier than we are able to do lots with the exoplanet information.”

Destruction of proof

Solely Earth has jigsaw-like tectonic plates that crash collectively and pull aside like bumper automobiles. The opposite rocky planets within the photo voltaic system have a single, inflexible shell of crust — a geological association that scientists name “stagnant lid” or “single lid” tectonics.

In plate tectonics, pancake-like chunks of brittle crust and higher mantle experience on the warmer, extra cellular mantle under. New crust types at midocean ridges, the place gaps between separating plates create house for magma from the mantle to rise. In a geologic balancing act, dense oceanic crust is destroyed at subduction zones, the place one plate slides beneath one other. The oldest identified little bit of oceanic crust, situated within the Mediterranean, dates to simply 340 million years in the past, making it far too younger to be helpful for pinpointing when plate tectonics arose.

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At Thingvellir Nationwide Park in Iceland, the rift between the North American and Eurasian tectonic plates is seen. (Picture credit score: Mlenny through Getty Photos)

Continental crust is lighter than oceanic crust and floats above the destruction wrought by subduction. However nonetheless, little or no stays from Earth’s early days, and what’s left is eroded and warped. Fewer than 7% of rocks on the floor immediately are older than 2.5 billion years. Return earlier than 4.03 billion years, to the Hadean eon, and the rock file has utterly vanished. The primary half billion years of Earth’s life left not a single little bit of basalt behind.

Due to this fixed planetary recycling, the oldest incontrovertible proof of plate tectonics — rocks fashioned solely in subduction zones — dates again solely round 700 million years. One other sturdy little bit of proof, items of oceanic crust pushed up on continental crust throughout subduction initiation, emerged globally round 900 million years in the past. On this geological time-frame, multicellular animals, similar to sea sponges and comb jellies, had been simply rising.

Some geoscientists assume plate tectonics has been working solely since that point. However extra suspect that plate tectonics emerged earlier, within the Archean eon, which ran from 4 billion to 2.5 billion years in the past. The proof relies largely on chemical analyses of rocks. For instance, round 3 billion years in the past, there are hints of an rising quantity of crust melted and reformed slightly than forming instantly from mantle rocks. Round 3.8 billion years in the past, a shift within the chemistry of Earth’s oldest minerals suggests a change from a steady, long-lived crust to a shorter-lived, extra modern-looking crust, maybe indicating the beginning of subduction. Although there isn’t a single agreed-upon date, the Archean seems promising as a time when large geological adjustments had been occurring on Earth.


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“It factors to a extremely essential transition,” stated Nadja Drabon, an Earth and planetary scientist at Harvard College who led the research indicating the change to shorter-lived crust.

A handful of sand

At any time when tectonics started, geoscientists agree that it most likely helped gasoline the evolution and complexity of life.

“There may very well be billions of planets with some type of primitive life, however the means to construct a radio transmitter or launch a rocket ship requires a sure set of circumstances that are solely prone to occur on a planet that has plate tectonics and each oceans and continents,” Robert Stern, a geoscientist on the College of Texas at Dallas, instructed Dwell Science.

In prehistoric animals, plate tectonic exercise has been tied to quicker charges of evolution, most likely as a result of geological actions break up up habitats and create new niches for all times to evolve.

A large brown fish suspended in water

The coelacanth’s evolution was seemingly pushed partly by plate tectonics, previous analysis suggests. (Picture credit score: loonger through Getty Photos)

Plate tectonics additionally could have enabled life to get better from devastating mass extinctions. For example, on the finish of the Permian interval, a mass extinction pushed by carbon-dioxide-spewing volcanic eruptions killed off 90% of species on Earth. Life on the planet in the end recovered as a result of weathering of continental rocks breaks down carbon-bearing minerals and washes them into the ocean, the place marine organisms flip them into reefs and shells that change into limestone and are finally subducted again into the planet’s inside. When the ambiance goes haywire, tectonics step by step shifts Earth again into an setting that is extra conducive to life.

Whereas almost all geoscientists agree with the concept, with out plate tectonics, life on Earth is perhaps restricted to primitive organisms, a small group of researchers is now suggesting that plate tectonics may have emerged even earlier — maybe contributing to the origin of life itself by bringing minerals that help life from the planet’s inside to the crust.

That is difficult territory, pushing researchers again earlier than 4 billion years in the past, into the Hadean eon. The one direct proof of the primary 500 million years of Earth’s existence is the presence of zircons, minerals that survive melting at mantle temperatures and pressures. Although the rocks as soon as containing these minerals have melted away, the zircons — that are smaller than grains of sand — stay.

“They’re teeny-tiny, and we simply throw the kitchen sink at them attempting to get each final little piece of knowledge we are able to get from them,” Drabon instructed Dwell Science.

A microscope image of a blue crystal

A 4.4 billion-year-old zircon from Jack Hills, Australia. As a result of zircons do not soften at mantle temperatures, they supply a snapshot of early Earth that resists destruction. (Picture credit score: John Valley, College of Wisconsin-Madison)

These zircons from the Hadean are sparse; all of them discovered worldwide may seemingly slot in a thimble. But this handful has proven that Earth had an ocean as early as 4.4 billion years in the past — simply 200 million years after the planet fashioned and never lengthy earlier than the ancestor of all life immediately existed. By as early as 600 million years after Earth fashioned, in keeping with a research printed in June, the planet had each land and recent water.

To some researchers, this means Earth’s crust could have been recycling within the Hadean. Water weakens the crust, creating the potential for breakage and thus subduction, stated Jun Korenaga, a geophysicist at Yale College. As a result of water is important for plate tectonics, the query turns into, “Why cannot now we have plate tectonics if we had floor water?” Korenaga stated.

In experimental work printed in 2023, researchers melted rocks at excessive pressures and located that situations that mimic subduction create rocks just like Earth’s oldest rocks. Korenaga additionally argues that plate tectonics is the one efficient technique to scale back the quantity of carbon dioxide in early Earth’s ambiance from the degrees discovered on Venus to the extra reasonable concentrations that existed by the start of the Archean on Earth.

Intriguingly, one other essential occasion occurred throughout the Hadean that makes Earth undeniably completely different from its rocky neighbors: About 100 million years after Earth first coalesced, a planet-size physique slammed into it, completely shattering and melting each our bodies and flinging off the fabric that will change into the moon. A paper printed earlier this yr modeled this impression and located that the blending of the 2 our bodies may have created plumes of scorching materials in Earth’s mantle which will have kicked off subduction round 200 million years later.

New Supercomputer Simulation Sheds Gentle on Moon’s Origin – YouTube
New Supercomputer Simulation Sheds Light on Moon’s Origin - YouTube


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“Why is Earth the one rocky planet to have plate tectonics?” stated Qian Yuan, lead creator of that paper and a postdoctoral fellow in geodynamics on the California Institute of Know-how. “I believe the moon-forming large impression may very well be the primary issue.”

However not everyone seems to be satisfied by this story. A Hadean begin to plate tectonics is an intriguing thought, T. Mark Harrison, a professor emeritus of geoscience at UCLA, instructed Dwell Science, however the proof continues to be pretty minimal. He worries that geoscientists on all sides of the difficulty are overconfident of their claims. “However the very last thing we’d like is a brand new type of groupthink primarily based on, actually, a thimble-full of sand grains,” Harrison wrote in an article with the appropriately blunt title “We do not know when plate tectonics started.”

Life on different worlds

If plate tectonics fuels life, and even simply complicated life, the seek for different organisms among the many stars could lead humanity to a geologically energetic planet.

Sadly, we won’t but detect plate tectonics on far-off exoplanets, stated Tobias Meier, an professional on mantle dynamics on the College of Oxford. However in 2021, Meier and his crew used thermal information and pc modeling to find out that the rocky exoplanet LHS 3844 b, which sits 49 light-years from Earth, might need an energetic mantle and shifting crust.

An illustration of a small black planet with a crackled surface near a fiery star

Researchers suspect exoplanet LHS 3844b, situated 49 light-years from Earth, might also have plate tectonics. (Picture credit score: NASA, ESA, CSA, Dani Participant (STScI))

LHS 3844 b is not prone to host life. It orbits very near its star and has no ambiance. Half of the planet is in everlasting daylight, with a temperature of 1412 levels Fahrenheit (767 levels Celsius), whereas the opposite is a frigid minus 429 F (minus 273 C) at night time. It is this temperature distinction between the 2 sides of the planet that drives mantle movement in LHS 3844 b, Meier and his colleagues reported in 2021. If actual, that model of plate tectonics seems nothing like Earth’s. But it surely exhibits the range of planetary geology that would lurk elsewhere within the cosmos.

“In the long run, understanding what causes tectonics and whether or not it may function on completely different planets will assist us perceive whether or not these planets shall be liveable,” Meier stated.

Extra highly effective telescopes such because the James Webb Area Telescope could result in higher hints of exoplanet geology within the close to future. However Earth’s shut neighbors deserve scrutiny, too, stated Craig O’Neill, a geophysicist at Queensland College of Know-how in Australia. Venus is correct subsequent door, and it is nonetheless controversial whether or not it had tectonics up to now. Understanding its present, single-lid geology may assist scientists determine why the 2 planets’ fates diverged, and whether or not plate tectonics could clarify why one planet hosts life and the opposite seemingly does not.

“A variety of the event of the place we will go in plate tectonics goes to come back from wanting up,” O’Neill instructed Dwell Science, “slightly than navel-gazing in.”

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