How Earth recycles continents deep underground
Scientists have uncovered new evidence that Earth's continents are continuously reworked deep beneath the surface, offering fresh insight into how continents have evolved over billions of years.
The Archaean is a geologic eon of Earth history spanning approximately 4.0 to 2.5 billion years ago, following the Hadean and preceding the Proterozoic. It is characterized by high heat flow, a largely anoxic atmosphere, and the stabilization of the first substantial continental crust, dominated by granite–greenstone terranes and high-grade gneiss complexes. Plate tectonic processes were likely more vigorous due to higher mantle temperatures, influencing crustal growth and metamorphism. The Archaean also encompasses the earliest widely accepted evidence of life, primarily prokaryotic microorganisms, preserved in stromatolites and microfossils, which played a foundational role in shaping subsequent biospheric and geochemical evolution.
Scientists have uncovered new evidence that Earth's continents are continuously reworked deep beneath the surface, offering fresh insight into how continents have evolved over billions of years.
Earth Sciences
May 20, 2026
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An international team of researchers' analysis of minerals from the Pilbara region of Western Australia has given new insight into how ancient continents on Earth formed as far back as 3.5 billion years ago. Professor Tony ...
Earth Sciences
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Astrobiology
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An international team led by researchers from the National Museum of Natural Sciences (MNCN-CSIC) has identified a key mechanism that has shaped Earth's continents over billions of years. This mechanism is the deep re-lamination ...
Earth Sciences
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Earth Sciences
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Earth Sciences
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The rocks beneath our feet are leaving a hidden signature in the shells of marine snails along Australia's ancient coastline, according to new research led by Adelaide University scientists. A study published in Proceedings ...
Ecology
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Western Australian hydrothermal and magmatic deposits that formed several hundred kilometers apart more than two and half billion years ago share more commonalities than previously thought.
Earth Sciences
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Oxygen is a vital and constant presence on Earth today. But that hasn't always been the case. It wasn't until around 2.3 billion years ago that oxygen became a permanent fixture in the atmosphere, during a pivotal period ...
Evolution
Feb 6, 2026
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117
More than 3.5 billion years ago, the Earth was not the hospitable world we know today. The atmosphere lacked oxygen, the seas were acidic and rich in iron, and volcanic activity roared across a barren landscape. Yet, in this ...
Evolution
Jan 23, 2026
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