Scientists have uncovered evidence of a long-lost underwater collision that occurred over 100 million years ago, dramatically altering the landscape of Earth’s deep interior. This ancient event, hidden beneath the waves of the eastern Pacific Ocean, has left its mark on the very fabric of our planet, shaping the mysterious structures that lie thousands of miles below our feet.
A team of researchers, led by Jingchuan Wang from the University of Maryland, used advanced seismic imaging techniques to peer into Earth’s mantle, the layer between the crust and the core. Their findings, published in Science Advances, reveal an unexpected anomaly in the mantle transition zone, a region located roughly 250 to 400 miles beneath the surface.
This anomaly takes the form of an unusually thick section of the mantle transition zone located east of the East Pacific Rise – the world’s fastest-spreading underwater mountain range. The thickened area, spanning about 1,200 miles, is accompanied by faster-than-average seismic velocities, suggesting the presence of colder material.
What could cause such a cold spot deep within the Earth?
The researchers propose an intriguing explanation: the remnants of an ancient tectonic plate that sank into the mantle during the Mesozoic era, between 250 and 120 million years ago.
“This thickened area is like a fossilized fingerprint of an ancient piece of seafloor that subducted into the Earth approximately 250 million years ago,” Wang says in a university release. “It’s giving us a glimpse into Earth’s past that we’ve never had before.”
This sunken plate, part of what geologists call the Phoenix Plate, likely dove beneath another oceanic plate in a process known as intraoceanic subduction. As it sank, it carried cooler material from the surface into the depths of the mantle, leaving behind a lasting thermal signature that we can detect today.
The discovery of this ancient subduction zone is particularly exciting because it helps explain a puzzling gap in one of Earth’s most enigmatic deep structures – the Large Low Shear Velocity Province (LLSVP) beneath the Pacific Ocean. LLSVPs are massive, continent-sized regions in the lowermost mantle characterized by slow seismic velocities. The Pacific LLSVP has long been known to have a curious gap in its eastern portion, and now we may know why.
As the ancient Phoenix Plate sank deeper into the mantle, it appears to have split the eastern arm of the Pacific LLSVP, much like a ship’s bow cutting through water. This interaction between the sinking plate and the LLSVP offers new insights into the dynamic processes shaping Earth’s deep interior.
“We found that in this region, the material was sinking at about half the speed we expected, which suggests that the mantle transition zone can act like a barrier and slow down the movement of material through the Earth,” Wang explains. “Our discovery opens up new questions about how the deep Earth influences what we see on the surface across vast distances and timescales.”
Source: https://studyfinds.org/mysterious-sunken-seafloor/?nab=0