Zircon crystals and magmas unveil contemporary insights into the traditional plate tectonic exercise that occurred on Earth billions of years in the past.
Earth is an ever-evolving and perpetually reworking planet. The creation of mountains, oceans, and volcanic eruptions all reveal the continual fluctuation of our planet’s floor. Central to those transformations is the potent pressure of plate tectonics, which entails the motion of Earth’s crustal plates. This basic mechanism has not solely sculpted our planet’s current panorama but additionally stays influential in figuring out its future.
However, what was plate tectonic exercise like in the course of the early phases of Earth’s historical past? Did this course of happen when life is believed to have originated?
“The dynamic tectonic nature of the modern Earth is one of the reasons why life exists today,” says Wriju Chowdhury, a postdoctoral analysis affiliate within the lab of Dustin Trail, an affiliate professor of earth and environmental sciences on the University of Rochester. “Exploring the geodynamics and the lithological diversity of the early Earth could lead to revelations of how life first began on our planet.”
Chowdhury is the primary creator of a paper printed in Nature Communications that outlines how Rochester researchers used small zircon crystals to unlock information about magmas and plate tectonic activity in early Earth. The research provides chemical evidence that plate tectonics was most likely occurring more than 4.2 billion years ago when life is thought to have first formed on our planet. This finding could prove beneficial in the search for life on other planets.
Plate tectonics power the creation and destruction of Earth’s crust
Plate tectonics on modern Earth is “extremely important,” Trail says, because it is “the dominant mechanism for the creation and destruction of Earth’s crust.”
Earth is the only known planet that has a mobile upper crust that is cyclically destroyed and created. The process delivers critical elements, such as iron and magnesium, from the interior of the earth to its surface and controls Earth’s water and carbon cycles. But, more importantly to geologists, plate tectonics melts and mixes rocks to create magmas with specific chemical makeups, depending on the rocks involved and the location where the “destruction” occurred. The chemical makeup of magma can therefore indicate the style of tectonics that created it.
Ancient crystals as tiny time capsules
Chowdhury and his colleagues conducted their research using zircons—tiny crystals in rocks that are like small time capsules. The zircons contain trace amounts of chemical elements, locked into the crystals at the time when the crystals were formed. The researchers date the zircons and then work backward, with zircons revealing information about the chemical makeup of the parent magmas from which the zircons crystallized. Researchers then use information about the magmas to reconstruct the physical and chemical environment—and to infer plate tectonic styles—of the early Earth, during the time when the zircons formed. In this case, the zircons were around 3.8 to 4.2 billion years old.
According to Chowdhury, most researchers infer information about early Earth using zircons to create probabilistic models to present different tectonic scenarios. Chowdhury and his colleagues went a step further to describe not only the zircons but also the parent magmas.
“Parent magmas are much more direct and reliable because they are closer to the source—the actual tectonic style,” Chowdhury says. “Our study describes the silicon and oxygen isotopic content of the zircons and the trace element content of the parental magmas, which has not been combined and presented before.”
Chowdhury, Trail, and their colleagues found chemical similarities between early Earth magmas and modern magmas created at tectonically active plate boundaries such as the Cascade and Aleutian Island chains or areas in Japan and the Andes Mountains.
“This suggests tectonic continuity from the ancient to modern times,” Trail says. “That is, our study shows the earth, billions of years ago, might have operated similarly as it does today.”
A key characteristic of a habitable planet
The researchers did not determine whether life existed when plate tectonics began—“neither life nor tectonics have an accurate start date yet,” Chowdhury says, noting that the geology community is divided on these points. But the new data provides chemical evidence suggesting that plate tectonics could have been occurring more than 4.2 billion years ago.
Whatever the case, he continues, plate tectonics is a key reason why Earth currently has a temperate living environment—and could be an important factor in the search for habitable living environments on other planets.
“The chances for life to originate increase manifold if there is some planetary dynamism,” he says.
Reference: “Eoarchean and Hadean melts reveal arc-like trace element and isotopic signatures” by Wriju Chowdhury, Dustin Trail, Martha Miller, and Paul Savage, 28 February 2023, Nature Communications.
The study was funded by the National Science Foundation and NASA.