Geoscientists Discover Pulsating Mantle Plume Beneath Remote Area of Ethiopia

According to a study led by researchers at the University of Southampton, these pulses are gradually tearing apart the African continent, resulting in the formation of a new sea basin.

Variation of geochemical and geophysical properties around distant triangles. Image credit: Watts et al, doi: 10.1038/s41561-025-01717-0.

The AFAR region stands out as a unique site on Earth where three structural lifts converge: the main Ethiopian rifts, the Red Sea rifts, and the Gulf of Aden lifts.

Geologists have speculated for some time that a thermal upwelling from the mantle, commonly referred to as plumes, exists beneath this area and promotes the extension of the crust along with the formation of upcoming sea basins.

However, the details regarding the structure of this upwelling and its behavior beneath the lifting plate have remained largely unknown until now.

“Our findings indicate that the mantle below the region is uniform but not stationary; it exhibits a pulsing nature that carries a unique chemical signature,” explained Dr. Emma Watts, who led the study at the University of Southampton and is currently at Swansea University.

“These rising pulses from the partially melted mantle are directed by the overlying filling plate.”

“This insight is crucial for understanding the interaction between the Earth’s interior and its surface.”

Dr. Watts and her team collected over 130 volcanic rock samples from remote areas and significant Ethiopian rifts.

Additionally, they utilized existing data and sophisticated statistical modeling to examine the structure of the crust and mantle, along with the melts within.

Their research reveals a single asymmetric plume beneath the distant region, showcasing distinct chemical bands that recur throughout the lift system, akin to geological barcodes.

These patterns vary in spacing according to the structural conditions of each lift arm.

“The observed chemical stripes imply that the plume pulsates like a heartbeat,” remarked Professor Tom Gernon from the University of Southampton.

“These pulses seem to behave differently based on the thickness of the plate and the rate at which it is pulled apart.”

“In faster-spreading rifts like the Red Sea, the pulsation occurs more efficiently and regularly, similar to a pulse flowing through a narrow artery.”

The findings illustrate that the mantle plume beneath the distant region is dynamic, reacting to the tectonic plate above it.

Dr. Derek Kiel, a researcher at the University of Southampton and the University of Florence, stated:

“This has significant implications for interpreting processes related to surface volcanism, seismic activity, and continental splitting.”

“Our work indicates that deep mantle upwellings flow beneath the tectonic plate, concentrating volcanic activity in the thinnest areas.”

“Understanding the rate and manner of mantle flow beneath the plate is crucial for further research.”

“Collaborating with experts from various fields within the institution, as we did for this project, is vital for uncovering the processes that occur beneath the Earth’s surface and their link to recent volcanic activity,” Dr. Watts emphasized.

“It’s challenging to see the broader picture, akin to assembling a puzzle without all the pieces unless we employ diverse techniques.”

study published in the journal Natural Earth Science.

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ej watts et al. Mantle upwelling at an afor triple junction influenced by the dynamics of the overriding plate. Nat. Geosci Published online on June 25, 2025. doi:10.1038/s41561-025-01717-0

Source: www.sci.news

Hydrogen Cyanide Detected in Enceladus’ Plume by Planetary Researchers

Using data from NASA’s Cassini mission, planetary scientists have detected several compounds critical to the habitability of Saturn’s icy moon Enceladus, including hydrogen cyanide, acetylene, propylene, and ethane. . These compounds may support living microbial communities or drive complex organic syntheses leading to the origin of life.

Diagram of Enceladus’ plume activity.Image credit: Peter other., doi: 10.1038/s41550-023-02160-0.

“Our study provides further evidence that Enceladus hosts some of the most important molecules for both producing the building blocks of life and sustaining life through metabolic reactions,” said Harvard University Ph.D. said Jonah Peter, a student in the program.

“Not only does Enceladus appear to meet the basic requirements for habitability, but we are also wondering how complex biomolecules are formed there and what kinds of chemical pathways are involved. I got an idea about it.”

“The discovery of hydrogen cyanide was particularly exciting because it is the starting point for most theories about the origin of life.”

As we know, life requires building blocks such as amino acids, and hydrogen cyanide is one of the most important and versatile molecules required for the formation of amino acids.

Peter and his colleagues refer to hydrogen cyanide as the Swiss Army knife of amino acid precursors because its molecules stack up in different ways.

“The more we tested alternative models and tried to poke holes in the results, the stronger the evidence became,” Peter said.

“Ultimately, it became clear that there was no way to match the plume composition without including hydrogen cyanide.”

Saturn’s moon Enceladus with plumes. Image credit: NASA / JPL-Caltech / SSI / Kevin M. Gill.

In 2017, planetary scientists discovered evidence of chemistry on Enceladus that could help sustain life in the ocean, if it exists.

The combination of carbon dioxide, methane, and hydrogen in the plume suggested methanogenesis, a metabolic process that produces methane.

This process is widespread on Earth and may have been important for the origin of life on Earth.

Peter and his co-authors found evidence for additional energetic chemical sources that are far more powerful and diverse than methane production.

They discovered a series of oxidized organic compounds, showing scientists that Enceladus’ underground ocean potentially has many chemical pathways to support life. That’s because oxidation promotes the release of chemical energy.

“If methane production is like a small clock battery in terms of energy, then our findings suggest that Enceladus’ ocean could provide large amounts of energy for any life that might exist. This suggests that we may be able to provide something similar to car batteries,” said Dr. Kevin Hand, a researcher at NASA’s Jet Propulsion Laboratory.

Unlike previous studies that used laboratory experiments and geochemical modeling to recreate the conditions Cassini found on Enceladus, the authors relied on detailed statistical analysis.

They examined data collected by Cassini’s ion and neutral mass spectrometers, which study the gas, ions, and ice grains around Saturn.

By quantifying the amount of information contained in the data, the authors were able to uncover subtle differences in how well different compounds explain the Cassini signal.

“There are a lot of potential puzzle pieces that can be put together when trying to reconcile observed data,” Peter said.

“We used mathematics and statistical modeling to identify the combination of puzzle pieces that best matched the plume’s composition and made the most of the data without over-interpreting the limited data set.”

of findings It was published in the magazine natural astronomy.

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JS Peter other. Detection of HCN and diverse redox chemistries in Enceladus plumes. Nat Astron, published online on December 14, 2023. doi: 10.1038/s41550-023-02160-0

Source: www.sci.news