Latest Articles and News

The deep carbon cycle was one of Earth’s most essential processes, regulating the movement of carbon between the planet’s surface and its deep interior over millions to billions of years. While most people are familiar with the short-term carbon cycle—where carbon moves through plants, animals, and the atmosphere—the deep carbon cycle operates on a much larger scale, shaping Earth’s climate and geology. This blog will explore how the deep carbon cycle works, why it matters, and the critical role it plays in maintaining Earth’s long-term balance.

Workshop Delivers New Estimate of Global Carbon Degassing

Twenty-eight DCO members came together from 29 April  –  4 May, 2018 at the Carnegie Institution for Science in Washington, DC to calculate a new estimate of global carbon dioxide (CO2) degassing from large volcanic emitters, small volcanic sources and diffuse degassing from volcanic regions. The synthesis of massive amounts

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Job Opening: Postdoctoral Research Associate

Applications were invited for a highly qualified and motivated postdoctoral research scientist with a geologic background in computational geophysical fluid dynamics, whose primary responsibility will be to develop new codes to study carbon transport in numerical models of fluid flow in subduction zones.

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Melting Temperature of Earth’s Mantle Depends on Water

A joint study between Carnegie and the Woods Hole Oceanographic Institution has determined that the average temperature of Earth’s mantle beneath ocean basins was about 110 degrees Fahrenheit (60 Celsius) higher than previously thought, due to water present in deep minerals. The results are published in Science. Earth’s mantle, the

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Live Blog: Trail by Fire 1.5 expedition to South America

The atmosphere that allows our planet to sustain life formed from gases emitted by volcanoes early in Earth’s history. These volatile elements are constantly recycled back into the deep Earth at subduction zones, where tectonic plates sink into the mantle. During this process the sinking plate was subjected to increasing

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Deep Mantle Chemistry Surprise: Carbon Content not Uniform

Even though carbon was one of the most abundant elements on Earth, it was actually very difficult to determine how much of it exists below the surface in Earth’s interior. Research by Deep Carbon Observatory scientists Marion Le Voyer, Erik Hauri (Carnegie Institution for Science, USA), Katherine Kelley (University of

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Third International Diamond School at the University of Alberta, Canada

The Third International Diamond School took place at the University of Alberta, with the Deep Carbon Observatory as the main event sponsor (together with De Beers and IsoMass). The Third International Diamond School took place at the University of Alberta, with the Deep Carbon Observatory as the main event sponsor (together with De Beers

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