A rocky relationship: A history of Earth's continents breaking up and getting back together

Earth
A composite image of the Western hemisphere of the Earth. Credit: NASA

A new study of rocks that formed billions of years ago lends fresh insight into how Earth's plate tectonics, or the movement of large pieces of Earth's outer shell, evolved over the planet's 4.56-billion-year history.

A report of the findings, published August 7 in Nature, reveals that, contrary to previous studies that say has operated throughout Earth's history or that it emerged only 0.7 billion years ago, tectonics actually evolved over the last 2.5 billion years. This new timeline impacts researchers' models for understanding how Earth has changed.

"One of the key ways to understand how Earth has evolved to become the planet that we know is plate tectonics," says Robert Holder, a Postdoctoral Fellow in Earth and Planetary Sciences at Johns Hopkins University and the paper's first author.

Plate tectonics dictates how continents drift apart and come back together, helps explain where volcanoes and earthquakes occur, predicts cycles of erosion and ocean circulation, and how life on Earth has evolved.

In a bid to resolve the mystery of how and when plate tectonics emerged on Earth, Holder and the research team examined a global compilation of metamorphic rocks that formed over the past 3 billion years at 564 sites. Metamorphic rocks are rocks that, through the process of being buried and heated deep in the Earth's crust, have transformed into a new type of rock. Scientists can measure the depth and temperatures at which metamorphic rocks form, and thereby constrain at in Earth's crust. Because plate tectonics strongly influences heat flow, ancient metamorphic rocks can be used to study plate tectonics in Earth's past.

The research team compiled data on the temperatures and depths at which the formed and then evaluated how these conditions have changed systematically through geological time. From this, the team found that plate tectonics, as we see it today, developed gradually over the last 2.5 billion years.

"The framework for much of our understanding of the world and its geological processes relies on plate tectonics," says Holder. "Knowing when plate tectonics began and how it changed impacts that framework."

Clarity on when plate tectonics began and whether it was different in Earth's past can help scientists better understand why we find certain rocks and minerals where we do and how they formed, says Holder.


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More information: Metamorphism and the evolution of plate tectonics, Nature (2019). DOI: 10.1038/s41586-019-1462-2 , https://nature.com/articles/s41586-019-1462-2
Journal information: Nature

Citation: A rocky relationship: A history of Earth's continents breaking up and getting back together (2019, August 7) retrieved 23 August 2019 from https://phys.org/news/2019-08-rocky-relationship-history-earth-continents.html
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Aug 08, 2019
The data is convincing, using T/P distributions, where T/P is low near a subduction zone and high further away so giving a bimodal distribution when plate tectonics operate. The unimodal distribution splits up at the time when the atmosphere is oxygenated (giving snowball Earths) and the bimodal modern plate tectonics stabilize when animals evolve (correlated with another snowball Earth episode). But their T/P data suggests rather that secular cooling of the upper mantle is the cause. This gives thinner ocean plates that dives deeper as they are forced under thicker land plates.

In any case they see more diversified sediments as cooling proceeds which is good for diversifying life, and we know it frees more phosphorous which is good for productivity [ https://www.lpi.u...n-event/ ], so perhaps the correlation with atmosphere oxygenation simply follows contingent on all that.

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