Canada’s Nuvvuagittuq Greenstone Belt Contains Fragments of Earth’s Oldest Crust, Research Reveals

Geologists have found significant evidence indicating the preservation of Hadean Rocks, with an age of 4.16 billion years. The Nuvvuagittuq Greenstone Belt offers a rare glimpse into the early Earth.



Canadian Nuvvuagittuq Green Stone Belt. Image credit: Jonathan O’Neill.

The earliest geological history of Earth remains largely unclear due to the scarcity of rocks and minerals from the Hadean period (over 4.3 billion years ago).

These ancient materials are often altered or destroyed as the planet’s crust undergoes continual recycling through various geological processes.

“One potential survivor of the Hadean era crustal rock is the Nuvvuagittuq Greenstone Belt,” stated Dr. Christian Saul, a senior author from the University of Ottawa and his colleagues.

“However, this perspective is contentious. Some researchers argue that the isotopic data backing these estimates might instead reflect later geological mixing rather than the true age of the layers.”

“If proven to be of Hadean origin, the Nuvvuagittuq Greenstone Belt would represent the oldest known preserved rock sequence on Earth.”

“This could yield critical insights into early geology and possible environments for the emergence of life.”

To refine the age of the Nuvvuagittuq Greenstone Belt, researchers concentrated on specific types of ancient rock intrusions known as metagabbro within the belt.

These intrusions intersect with ancient basaltic rocks, enabling the authors to utilize combined uranium-lead (U-Pb) dating to determine the minimum age limits of older layers, along with both short and long-lived samarium-neodymium (Sm-Nd) isotopic analysis.

Sm-Nd data yielded a consistent age of approximately 4.16 billion years, irrespective of the sample location or mineral composition.

The convergence of both isotope systems producing the same age in rocks with clear evidence of magma differentiation strongly supports their Hadean era crystallization.

This is in accordance with the Hadean Eon surviving within the Nuvvuagittuq Greenstone Belt.

“Studying these rocks allows us to trace back to the origins of our planet,” noted Dr. Jonathan O’Neill, a researcher at the University of Ottawa.

“This will enable us to gain a better understanding of how the first continent formed and help reconstruct the environment in which life emerged.”

Survey results published in the journal Science.

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C. Sole et al. 2025. Evidence of Hadean Mafic invasion in the Canadian Nuvvuagittuq Greenstone Belt. Science 388 (6754): 1431-1435; doi: 10.1126/science.ads8461

Source: www.sci.news

These Rocks May Be the Final Remnants of Earth’s Early Crust

Canadian Nuvvuagittuq Green Stone Belt may contain the world’s oldest rock

Jonathan O’Neill

About four billion years ago, magma from Earth’s mantle intruded the primitive crust of a nascent planet. Over the next period, nearly all of the planet’s early crust melted back into the mantle, leaving behind a small remnant near the site of this intrusion that still exists today.

This remnant is part of the Nuvvuagittuq Greenstone Belt along Hudson Bay’s coast in Canada. Recent analyses of the rock’s radioisotope signatures have sparked debates among geologists about whether it is indeed the oldest rock on Earth or simply very ancient.

In a study published in 2008, Jonathan O’Neill from the University of Ottawa and his team posited that the surrounding rocks could be as old as 4.3 billion years, dating back to the Hadean eon—just a few hundred million years after Earth’s formation.

While there have been discoveries of older mineral grains, these ancient Hadean rocks provide critical insights into Earth’s formative years, possibly shedding light on geological enigmas like the onset of plate tectonics and early ocean compositions.

The method used for dating the rocks has drawn controversy, particularly regarding the claimed age of 4.3 billion years. Traditionally, old rocks are dated utilizing a robust mineral known as zircon, but these volcanic rocks lack zircon. “No one can date these rocks using the popular techniques,” O’Neill remarks.

Instead, researchers analyzed the isotopes of neodymium and samarium within the rock. As samarium decays, it generates different isotopes of neodymium at predictable rates, allowing the ratio of isotopes to serve as a “clock” marking the time since the rock crystallized from magma. Interestingly, two isotopes of samarium can decay at differing rates, acting as two parallel chronometers. Disagreement arose among researchers about whether the rock was genuinely Hadean, as the two clocks provided inconsistent age estimates.

“I’m not convinced that most of the early Earth research community agrees,” states Richard Walker at the University of Maryland.

Currently, O’Neill’s team is assessing the neodymium and samarium isotopes in the rock formations dating back 4.3 billion years. By definition, such intrusions are younger than the surrounding rock layers, implying that dating an intrusion yields the minimum age for the enclosing rocks.

Detailed view of the Canada Nuvvuagittuq Green Stone Belt

David Hutt/Alamy

In the findings, the two chronological indicators tell the same tale, indicating the rocks’ age to be approximately 4.16 billion years. “Both clocks yield identical results,” O’Neill states. This consistency bolsters the theory that the surrounding rocks were indeed solidified during the Hadean eon, making them potentially the only known remnants of Earth’s ancient crust.

“I believe they present the strongest argument possible,” asserts Graham Pierson from the University of Alberta, Canada.

“The simplest interpretation of this data is that these represent the oldest rocks on Earth,” says Jesse Reimink at Pennsylvania State University. Nevertheless, he cautions that this may not be the final word on the subject, stating, “When it comes to the oldest rocks and minerals, absolute certainty is hard to come by.”

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Source: www.newscientist.com

Research on Modeling Unveils New Insights into Venus’ Crust

Planetary scientists initially believed that Earth’s outer crust would become thicker over time, particularly due to the perceived absence of forces pushing it back into the planet’s interior. However, researchers from Open University, NASA’s Johnson Space Center, and the Lunar and Planetary Institute suggest that processes involved in crustal transformation, centered around rock density and melting cycles, offer a different perspective.

An artistic interpretation of active volcanoes on Venus illustrates a subduction zone where the foreground crust of a topographical groove descends into the planet’s interior. Image credits: NASA/JPL-Caltech/Peter Rubin.

The earth’s crust is rock-like and composed of massive, slowly migrating plates that fold and create faults through a process known as plate tectonics.

For instance, when two plates collide, a lighter plate can slide over a denser plate, forcing it downward towards the underlying mantle.

This phenomenon, referred to as subduction, plays a crucial role in regulating the thickness of the Earth’s crust.

As the rocks penetrate deeper into the planet’s interior, they undergo transformations due to increased temperature and pressure, a process known as metamorphosis, which is one contributing factor to volcanic activity.

“Conversely, Venus consists of a singular skin with no signs of subduction seen in Earth’s plate tectonics,” noted Justin Filibert, PhD, associate director of NASA’s Johnson Space Center for Astromaterial Research and Exploration Sciences.

Through modeling, Dr. Filibert and his team found that Venus’s crust averages about 40 km (25 miles) thick, with some areas reaching up to 65 km (40 miles).

“This is surprisingly thin compared to Earth’s conditions,” Dr. Filibert remarked.

“Our model suggests that as the crust thickens, it becomes so dense at the bottom that it either breaks off to merge with the mantle or heats up enough to melt.”

“Thus, while Venus lacks movable plates, its crust still goes through metamorphosis.”

“This finding marks a significant advancement in understanding geological processes and planetary evolution.”

“The breaking and melting of crustal materials can reintroduce water and elements back into the planet’s interior, fueling volcanic activity.”

“We are developing a new model for how materials are recycled within the planet, providing insights into the processes that can trigger volcanic eruptions of lava and gases.”

“It reshapes our understanding of how Venus’ geology, crust, and atmosphere interact.”

“The forthcoming phase involves gathering direct data on Venus’s crust to test and refine these models.”

“The extent of volcanic activity on Venus remains uncertain.”

“While we postulate numerous volcanic phenomena, research indicates a need for extensive data to validate our assumptions.”

Relevant survey findings will be published in the journal Nature Communications.

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J. Semprich et al. 2025. The thickness of the earth’s crust and the transformation of Venus as a driver for recycling. Nat Commun 16, 2905; doi:10.1038/s41467-025-58324-1

Source: www.sci.news

Xavier Le Pichon, Renowned Geophysicist Who Pioneered Earth’s Crust Movement Modeling, Passes Away at 87

Xavier Le Pichon, a French geophysicist who revolutionized the way in which a pioneering model of the Earth’s tectonic plates was able to understand the movement of the Earth’s crust, and died on March 22 at his sister’s home in southern France. He was 87 years old.

His death was announced in a statement from Collegie de France, France’s premier educational institution. There, Dr. Le Picon was Professor Emeritus and Chairman of Geodynamics.

Dr. Le Picheon, who internized in Japanese concentration camps as a child, continued to build a second career as a deep sea explorer, working with Mother Teresa of India for a while. However, it was in the field of geodynamics that he made his biggest contribution. Use a computer to create a model of the Earth plate.

His formulation has six such plates, as he said when he won in 2002, “for what is essential to the structural symptoms of the Earth’s surface.” Balzan PrizeAwarded in science fields not covered by Nobel.

Plate tectonics with Earth’s surface studies is a “framework” for understanding earthquakes, volcanoes, and the Earth’s long-term “climate stability.” David BelkovichYale geophysicist. He added that Dr. Le Picon was one of the architects of the framework.

Professor Bercovici emailed him “one of the giants of the plate structure revolution, especially when practicing its mathematical theory.”

His work was built on the theory of plate tectonics developed by Princeton scientist W. Jason Morgan in 1967. “Now we are entering an age of quantification for tectonics,” wrote Dr. Le Picon.

“The University of Rochester has a great opportunity to develop a new world of geophysics,” said John Taldono, professor of geophysics at the University of Rochester.

Dr. Pichon came to view the Earth as “an extraordinary creature with ocean and continental movement.”

After years of studying the ocean and its floors, including Columbia University, Dr. Lupicheon achieved a breakthrough in the mid-1960s. He called the “incredibly unpleasant” months of cruise hosted by Columbia, and observed a 37,000-mile-long ridge in the South Atlantic and Southwest Indian oceans.

The object was to detect seismic activity along the coat of arms of the ridge and test predictions made in the 1950s by Jean Pierre Rothet, another French scientist. “We went zigzag on this famous earthquake line for nine months,” Dr. Le Picon wrote in his 2003 book, Plate Tectonics: The Insider’s History of Modern Theory of the Earth.

The trip confirmed it and he continued to earn his Ph.D. Based on that study, at the University of Strasbourg in 1966.

“As such, the central ridge has achieved a victory over tectonics, becoming the most important structure in the world due to stroke,” he wrote.

But this was in the early 1960s, and he ran “in what we call “fixed mentors,” things weren’t moving.” Like he put it down On the 2009 episode of the podcast “Being With Krista Tippett.”

“The Earth was considered everything to be a static place,” he said. “Things were moving up and down, but never sideways. The continent was always there. The ocean was always there.”

Dr. Le Picon initially defended these concepts, but he realized they were wrong. He returned from the lab one day and told his wife, “My paper’s conclusions are wrong.”

Rather, I felt that he was an American geologist. Harry Hess The assumption in 1962 that the seabed had continued expansion was correct. After all, there was seismic activity along the top of the ridge. Measuring magnetic anomalies along the ridge is important in proofing Dr. Hess’s hypothesis.

Dr. Le Pichon recalled his Eureka moment in an episode of the podcast. “I worked all night on a computer, and one night I put it all together and found out that Hawaii approaches Tokyo at 8 centimeters each year.”

He recalls what he told her: “I discovered how the Earth works. I really know that now.” And I was so excited. ”

His passion for what was happening under the ocean developed quickly. After growing up in what was a French protectorate in Vietnam at the time, he was interrupted by his family during World War II when Japan invaded.

“When I was in the concentration camp, we were on the Pacific coast, and I was wondering what was under the water, and I was on the beach,” Dr. Le Picon said in 2009.

After publishing his groundbreaking paper in 1968, Columbia and Massachusetts Institute of Technology presented the first quantitative global model of plate boundaries and movement, offering him a teaching position. However, he instead led the Institute of Oceanography in Brittany, France, where he began his second career as an underwater ocean explorer, advancing into the depths of small submarines on joint Franco-American expeditions.

In 1973, he said he had taken such a ship 3,000 meters below him while exploring the ridges in the Mid-Atlantic Ocean.

“I had the impression that I was a religious man and had the return to Genesis,” he added. Other sea floor trips in Greece and Japan followed.

Dr. Lupichon, a Roman Catholic who attended Mass every day since childhood, experienced what was called a “great crisis in my life” in 1973 and worked for Mother Teresa in the city of Calcutta, India.

“I was very immersed in my research. I wasn’t looking at anyone else anymore,” he said. “In particular, I didn’t see people suffering and difficulties. It was a very strong crisis.”

His experience in Calcutta changed him by his account, and then he, his wife and his children engaged in charity and charity in the French Lach community for people with intellectual disabilities. They lived there for nearly 30 years. He and his family then find a similar community and help them live there.

Xavier Thaddée Le Pichon was born on June 18, 1937 in Quy Nhon, Vietnam, France, to Jean Louis Le Pichon and Helene Pauline (Tyl) Le Pichon, rubber plantation managers.

The family moved to France in 1945, with Xavier attending the Institute of Cherbourg Saint Paul and the Lyce Sainte Geneviève in Versailles. In 1960 he received his Bachelor of Engineering from the Institut de Physique Du Globe He received a Fulbright Fellowship in Strasbourg to study at Columbia University’s Lamont Daughertier Observatory.

His original works will be carried out over the next decade, and in 1973 he wrote with Jean Bonnin and Jean Franciteau.

In the 1970s and 1980s, Dr. Le Picheon taught at the Sorbonne and Ecole Normal Superfoil. He became a professor at the French Collège de France in 1986 and remained there until his retirement in 2008. Besides Balzan, he won many awards and was a member of the National Academy of Sciences in the United States.

He was survived by his wife Bridget Suzanne (Barselmee) le Pichon, a pianist. His children, Jean Baptist, Marie, Emmanuel, Raffaère, Jean Marie and Pierre Guien. 14 grandchildren; 5 great grandchildren.

In lectures and interviews, Dr. Le Picon linked his discoveries to his Catholic faith as a scientist and the prayer work it stimulated. The bridge between them was his concept of “vulnerability,” and he said, “is the essence of men and women, at the heart of humanity.”

The earth is also vulnerable. “I have a very close relationship with the Earth, so I think a little like a mother,” he said in 2009.

Sheila McNeill and Daphne Angles Contributed research.

Source: www.nytimes.com

Newly Uncovered Massive Energy Reserve Found Beneath Earth’s Crust

The issue of energy consumption and its sources has always been a significant concern in the context of the climate crisis. In response, efforts are being made to utilize cleaner and newer fuels. Recently, a groundbreaking discovery of vast reservoirs of hydrogen energy hiding beneath the Earth’s surface has emerged, prompting questions about its potential impact.

Naturally occurring geological hydrogen is formed through Earth’s geochemical processes and has been identified in limited locations such as Albania and Mali. Research published in the journal Scientific Progress suggests that these reserves are widespread globally.

The study posits that if just 2 percent of the underground hydrogen could be extracted, it could yield 1.4 × 10^16 Joules of energy, equivalent to the world population’s energy consumption in 35 minutes. This amount of energy exceeds that of all natural gas reserves on Earth and could aid in achieving net-zero carbon goals.

While current methods for obtaining hydrogen involve fossil fuels or water-intensive electrolysis processes with a carbon footprint, extracting geological hydrogen is a comparatively low-carbon process, albeit currently practiced only in Mali.

Researchers at the U.S. Geological Survey have developed a model combining knowledge of hydrogen occurrence and geological data to explore these reservoirs on a global scale, estimating a substantial amount of hidden hydrogen beneath the Earth’s surface.

However, experts are hesitant about committing resources to extraction due to the scale and infrastructure required, as highlighted by geoscientist Professor Bill McGuire from University College London (UCL). He emphasizes the abundance of renewable energy sources like wind and solar and questions the necessity of tapping into another finite resource.

About our experts

Professor Bill McGuire is a volcanologist, climatologist, and author currently serving as Professor of Geophysics and Climate Hazards at UCL. His works include books on natural disasters, environmental change, and climate solutions.

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Source: www.sciencefocus.com

Animal life discovered in the crust beneath deep-sea hydrothermal vents by researchers

Marine biologists have discovered adult tubeworms and other extrusive animals beneath the ocean floor of the East Pacific Ridge, a volcanically active and rapidly spreading ridge with numerous hydrothermal vents.



East Pacific Rise, subseafloor vents on the seafloor surface and crust on the outskirts of Fava Flow. Image credit: Bright others., doi: 10.1038/s41467-024-52631-9.

The East Pacific Rise is a volcanically active ridge located where two plates meet at the floor of the Pacific Ocean.

It contains many hydrothermal vents, which are openings in the ocean floor that form where ocean water and magma meet beneath the Earth's crust.

“It was once thought that the ocean-floor crust beneath hydrothermal vents was inhabited only by microorganisms and viruses,” says researcher Monika Breit of the University of Vienna and colleagues.

“But there are animals on the ocean floor that look like giant tube worms. Liftia Pachyputira Thrive. “

“The larvae are thought to disperse into the water column, even though they have never been observed there.”

“We hypothesized that these larvae migrate beneath the ocean floor via vent fluids.”

Dr. Bright and his co-authors sailing on the Schmidt Oceanographic Research Vessel Falcor (also)used the remotely operated vehicle SuB-astian to undertake a series of dives into a hydrothermal vent site located at a depth of 2,515 meters in the East Pacific Ridge.

The vehicle's arm was used to expose part of the ocean's crust, which revealed a warm, warm habitat that is home to a variety of species previously found only on the ocean floor, including giant tube worms and migratory animals such as earthworms and snails. A fluid-filled cavity was revealed.

Larvae from seafloor communities can colonize these subseafloor habitats, demonstrating the complex connectivity between seafloor and subseafloor ecosystems.

An animal habitat has been discovered beneath the ocean floor of the Earth's crust, but its extent is currently unknown, raising the urgency of its protection against potential future environmental changes.

“The presence of adult tubeworms suggests that the larvae dispersed through the recharge zone of the hydrothermal circulation system,” the authors said.

“Given that many of these animals are hosts to dense bacterial communities that oxidize reduced chemicals and fix carbon, subseafloor expansion of animal habitats may be localized. and regional geochemical flux measurements.”

“These findings highlight the need to protect vents, as the extent of these habitats has not yet been fully determined.”

team's work appear in the diary nature communications.

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M. Bright others. 2024. Animals that live in the crust beneath the shallow ocean floor of deep-sea hydrothermal vents. Nat Commune 15, 8466; doi: 10.1038/s41467-024-52631-9

Source: www.sci.news