One of geology’s still puzzling questions is when Earth’s tectonic plates embarked on the process that shaped the continents to become as we know them today, with researchers adhering to several theories regarding when it happened.
A team of scientists has suggested an answer to the mystery of when the tectonic plates of Earth first began moving to help it evolve into what it is today.
The researchers, led by a group of scientists from Harvard, sought clues in ancient rocks from Australia and South Africa.
According to the study, entitled “Paleomagnetic evidence for modern-like plate motion velocities at 3.2 Ga” and published in Science Advances, these plates were moving at least 3.2 billion years ago.
This was established after analysis of one of the oldest fragments of the Earth’s crust, found in the Pilbra Craton in Western Australia. The data pointed to a latitudinal drift of around 2.5 centimeters annually occurring some 3.2 billion years ago.
The scientists believe this shift is the earliest existing proof that plate motion similar to that witnessed on Earth today took place between two to four billion years ago.
Hailing the research as supporting the theory that tectonic movement occurred on Earth in its early years, the scientist added:
Story Behind a Rock’s Magnetic History
The research began as far back as in 2017, when Fu and Brenner drilled for rock samples from a portion called the Honeyeater Basalt. These were brought back to labs and placed into magnetometers and demagnetizing equipment that shed light on the rock’s magnetic history – suggesting it was formed 3.2 billion years ago.
The team then used this information coupled with other research to date when the rocks shifted from one point to another, establishing the annual drift of 2.5 centimeters.
Fu and Brenner used the novel Quantum Diamond Microscope to confirm their findings.
Despite the fact that the time interval of the geological movement established by the study seems to prove their case, the team acknowledge that they cannot exclude the results to be due to a phenomenon called “true polar wander.”
This is something that can also cause the Earth’s surface to shift.
Plate Tectonics Timeline
When the first shifts first started in plate tectonics – key to the evolution of life and the development of the planet – is an issue that has been long debated in geology.
Today, our planet Earth’s outer shell consists of some 15 blocks of crust that continents and oceans sit on.
Overtime, movement of these plates shaped the location of the continents and aided the formation of new ones.
As the process pushed forth landforms like mountain ranges, it also exposed new rocks to the atmosphere. The latter resulted in chemical reactions that brought forward evolution of life, which is possible only in a stable climate – something these processes achieved on the surface of the Earth over billions of years.
Fu, an assistant professor of earth and planetary sciences in the Faculty of Arts and Science, Harvard University, added:
The new research could also be instrumental in understanding other worlds, beyond our planet, says Alec Brenner.
The two lead authors of the study, Alec Brenner and Roger Fu, are planning to continue studying data from the Pilbara Craton and other samples from around the world in future experiments.
Sourse: sputniknews.com
