How Massive Submarine Volcanism Could Explain Triassic Extinctions

New Research Reveals Japanese and Australian Geologists Uncover Evidence Linking Oceanic Igneous Provinces to Low-Order Extinction Events During the Triassic Period

Early Earth. Image credit: Peter Sawyer/Smithsonian Institution.

“Mass extinctions represent profoundly catastrophic events in the history of Earth,” stated Dr. Jiang Jun Huang along with a team of geologists from Jilin University and Curtin University.

“While numerous mass extinctions have shaped Earth’s evolutionary timeline, five major events are particularly notable.”

“These pivotal extinctions radically altered the trajectory of life on our planet.”

“Besides the five major mass extinction events, numerous sub-extinctions frequently occur, such as the Norian-Rhaetian extinction of the Triassic period.”

“Although the causes of five major extinction events are well documented, the triggers of smaller, lower-order extinctions remain largely speculative.”

In this groundbreaking study, the researchers investigated remnants of oceanic islands, seamounts, and plateaus on the Tibetan Plateau, mapping the evolution of the Meso-Tethyan and Neo-Tethyan oceans.

Throughout the Triassic, three significant episodes of oceanic large igneous provinces (LIPs) materialized between 250 and 248 million years ago, 233 and 231 million years ago, and 210 and 208 million years ago.

By synthesizing the geological records of these LIP episodes with extensive Triassic geological datasets, the team established a link between marine LIPs and at least four extinctions in marine life, which were spurred by subsequent anoxic-oxic events.

“Marine LIPs account for half of the identifiable geologically induced extinctions during the Triassic,” the scientists reported.

“This suggests that oceanic LIPs were the primary initiators of the Triassic extinction events.”

“Although eruptions related to oceanic LIPs are frequent, evidence for ancient occurrences may significantly diminish due to subduction processes during the closure of ocean basins.”

“This destruction complicates the identification of such records, and even when identified, interpreting and dating them accurately poses challenges.”

“Orogenic belts, remnants of long-extinct oceanic basins, may harbor many unidentified ‘ghost’ ocean LIPs, whose eruptions likely played a critical role in other Phanerozoic extinctions, which remain under-recognized in current Earth system models.”

The team’s study is published in the journal Geology.

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Jian Jun Fan et al., “Large Oceanic Igneous Provinces: A Major Driver of Repeated Triassic Extinctions,” Geology, published online on January 20, 2026. doi: 10.1130/G53406.1

Source: www.sci.news

How Ancient Mass Extinctions Revealed Earth’s Evolution into a Super Greenhouse

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Current forest die-offs due to global warming resemble those from the Permian and Triassic extinction events.

Ina Fassbender/AFP via Getty Images

Following a dramatic increase in carbon dioxide levels 252 million years ago, the death of forests resulted in enduring climate alterations, with the greenhouse effect persisting for millions of years.

Researchers striving to comprehend this phenomenon, which triggered the largest mass extinction in Earth’s history, caution that ongoing greenhouse gas emissions may lead to similar outcomes.

The extinction events of the Permian and Triassic are believed to have been triggered by extensive volcanic activity in what is now Siberia, elevating atmospheric CO2 concentrations.

The planet’s surface temperature soared by as much as 10°C, with average temperatures in the equatorial regions climbing to 34°C (93°F)—a rise of 8°C above the current average.

These extreme conditions persisted for roughly 5 million years, causing over 80% of marine species and upwards of 70% of terrestrial vertebrate families to become extinct, according to some estimates.

Although some scientists have recently posited that these mass extinction events may have limited effects on terrestrial ecosystems, Andrew Meldis from the University of Adelaide expresses confidence that life was nearly extinguished 252 million years ago.

“Small pockets of life might survive mass extinctions in isolated enclaves, but many areas within the Permian-Triassic fossil record reveal a complete ecosystem collapse,” notes Meldis.

He and his team scrutinized the fossil record to investigate why the Super Greenhouse event, which drives mass extinction, lasted five million years—far longer than the 100,000 years predicted by climate models.

The findings revealed that vast expanses of forests, originally with canopies of around 50 meters, were supplanted by resilient underground flora, typically ranging from 5 cm to 2 meters in height. Additionally, peat marshes, significant carbon storage ecosystems, vanished from tropical areas.

Employing computer models of Earth’s climatic and geochemical systems, researchers indicated that the depletion of these ecosystems contributes to elevated CO2 levels persisting for millions of years. This predominantly occurs because vegetation plays a crucial role in weathering, the mechanism that extracts carbon from the atmosphere and sequesters it in rocks and soil over extensive timescales.

With atmospheric CO2 levels rising rapidly, the parallels to the present are striking, asserts Meldis. As temperatures escalate, tropical and subtropical forests may find it increasingly challenging to adapt, potentially surpassing thresholds where vegetation ceases to maintain climate equilibrium.

Meldis explains that simply restoring former ecosystems will not lead to a “ping-pong effect.” He emphasizes that the atmosphere cannot be swiftly rejuvenated after the loss of the equatorial forest.

“You’re not transitioning from an ice house to a greenhouse and then back; the Earth will find a new equilibrium, which may differ significantly from prior states,” he elaborates.

Catlin Maisner, a researcher at the University of New South Wales—who was not involved in the study—describes reconstructing these events as analogous to “trying to assemble a jigsaw puzzle with many missing pieces,” yet acknowledges the team’s arguments as “plausible.”

However, she notes considerable uncertainty regarding oceanic processes during this period. “The ocean harbors far more carbon than land and atmosphere combined, and we still lack a comprehensive understanding of how marine biology, chemistry, and physical circulation were affected during that event,” cautions Meissner.

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  • Climate change/
  • Paleontology

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Source: www.newscientist.com

How did crocodile ancestors survive two mass extinctions?

Crocodylomorphs are surviving members of a 230 million-year-old lineage called Crocodylomorphs, a group that contains live crocodiles (i.e. crocodiles, alligators, garials). The crocodile ancestors continued with two mass extinction events: the final mass extinction (2014 million years ago) and the final mass extinction (approximately 66 million years ago). One of the secrets of crocodile longevity is their extremely flexible lifestyle, both in what they eat and in the habitat they get.

Approximately 215 million years ago, it is a land crocodile in what is now northwestern Argentina. Hemiprotostus leali Prepare to eat early mammal relatives Chaliminia musteloides. Image credit: Jorge Gonzalez.

“Many of the groups closely associated with crocodiles exhibited more diverse, more abundant and different ecology, but disappeared except for these few generalist crocodiles who live today,” said Dr. Keegan Melstrom, a researcher at the University of Utah.

“Extinction and survival rate are two aspects of the same coin. Through all mass extinctions, some groups can last and diversify. What can we learn by studying the deeper evolutionary patterns given by these events?”

The Earth has experienced five mass extinctions in its history. Experts claim we are alive throughout the sixth, driven by habitat destruction, invasive species and climate change. Identifying traits that increase survival rates during planetary upheavals could help scientists and conservationists better protect today’s vulnerable species.

Historically, the field has seen mammals as poster children to understand the survival of mass extinction.

Despite their resilience, research has largely ignored alligator clades.

In a new study, Dr. Melstrom and colleagues reconstructed the food ecology of crocodiles and identified the properties that helped several groups to persist and thrive through the final Triassic and mass extinction of the Tododonians.

“There’s a risk that we’ll draw a conclusion millions of years ago and try to apply it directly to conservation. We have to be careful,” said Professor Randy Ilmith at the University of Utah.

“If people study mammals and reptiles and find the same pattern in terms of extinction survival, they may predict that species with a generalist diet will be better.”

“That information helps to make predictions, but it’s rare that you can choose which individual species survive.”

Living crocodiles are famous for being semi-aquatic generalists who thrive in lakes, rivers, and swamps and waiting to ambush unsuspecting prey. Noisy people, they aren’t. Young people enjoy tadpoles, insects, crustaceans and more before graduating to a larger fare, including fish, deer and even fellow crocodiles.

However, today’s crocodile’s uniform lifestyle obscures the massive dietary ecology that crocodiles flourished in the past.

A broader evolutionary group, including early crocodiles and many other extinct strains, Pseudosuchia ruled the land during the late Triassic period (237-2014 million years ago).

Early crocodiles were small to medium-sized creatures, rare in the ecosystem, and were mainly carnivorous animals that ate small animals.

In contrast, other pseudosu bone groups dominated the land, occupying a broad ecological role, exhibiting diverse body types and sizes of vertigo.

Despite their superiority, once a serious extinction hit, the non-crocodylomorph fake su did not survive.

Hypercarnivore crocodile also seemed to die, while generalists on earth went through it.

The authors assume that this ability to eat almost anything allowed them to survive, but many other groups have become extinct.

“Then it becomes a banana. Aquatic high carnivores, terrestrial generalists, terrestrial carbides, terrestrial herbivores – crocodiles have evolved a huge number of ecological roles throughout the age of dinosaurs,” Dr. Melstrom said.

Something happened in the late Cretaceous period and the crocodile faded.

Diverse ecology-focused lineages have begun to disappear even among the generalists on the ground.

Due to the mass extinction event of Cretatuas (separated by meteors that killed non-bird dinosaurs), most of the survivors are semi-predictive generalists and a group of aquatic carnivorous animals.

Nearly all 26 live crocodiles today are semi-rated generalists.

How do scientists analyze food on menus that are millions of years old? They analyze the shape of fossilized teeth and skulls to collect the basics of the animal’s diet.

The author visited museum collections of zoology and paleontology across seven countries and four continents to obtain the necessary fossil specimens.

They examined skulls of 99 extinct alligator species and 20 living crocodile species, creating a fossil dataset that spans 230 million years of evolutionary history.

They previously had built a living database of non-crocodilians, including 89 mammals and 47 lizard species.

The specimens represent a variety of vegetative ecology, ranging from strict carnivorous to mandatory herbivores and a wide variety of skull shapes.

As semiac ambush predators, today’s crocodiles primarily occupy a similar ecological role in many different environments.

They continue to have a very flexible diet. Perhaps it is a remnant of their deep, diverse evolutionary past.

For endangered crocodile people, such as Cuban crocodiles in the Himalayas’ hills and the swamps of the country’s Zapata, dietary flexibility may give us an opportunity to continue our current sixth mass extinction.

The biggest challenges these species face are habitat loss and human hunting.

“I hope that, rather than thinking about ferocious beasts or expensive handbags, when I see living crocodiles and crocodiles, people will appreciate their astonishing 20 million years of evolution and how they survived so many turbulent events in Earth’s history,” Professor Ilmith said.

“Crocodiles are equipped to survive many future changes if they are willing to help maintain their habitat.”

result It will be displayed in the journal Paleontology.

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Keegan M. Melstrom et al. 2025. For a while, Crocodile: Crocodile’s resilience to mass extinction. Paleontology 68(2): E70005; doi: 10.1111/pala.70005

This article is a version of a press release provided by the University of Utah.

Source: www.sci.news

A nearby supernova explosion could have triggered multiple mass extinctions on Earth

New research from Keele University and Universidad de Alicante shows that near Earth explosion Giant O and B type stars It occurs at a rate of 2.5 per billion years. This result supports the view that such an event may have caused one or more of the mass extinction events recorded on Earth.

Among the puppies in the constellation, I have the impression of the artist Zeta Puppis, an O-shaped star about 1,400 light years away. Image credit: Tahina Ramiaramanantsoa.

Astronomers at Kiel and Alicante University believe that the explosion of supernova near Earth could condemn both the late Devonian and Ordovician extinction events that occurred 372 and 445 million years ago, respectively.

Ordovician extinction killed 60% of marine invertebrates when life was largely confined to the ocean, and the late Devonian wiped out about 70% of all species, leading to a major change in the species of fish present in ancient seas and lakes.

Previous studies have not been able to identify a clear cause of either event, but are thought to be related to Earth's ozone layer depletion, which may have been caused by supernova.

A new study found that the velocity supernova that occurs near our planet coincides with the timing of both mass extinctions.

“Supernova explosions bring heavy chemical elements to interstellar media, which are used to form new stars and planets,” said Dr. Alexis Quintana, PhD from Kiel University, the lead author of the study.

“However, if planets, including Earth, are too close to events of this type, this can have devastating effects.”

“Supernova explosions are some of the most energetic explosions in the universe,” said Dr. Nick Wright, PhD from Keel University.

“If a large star explodes as a supernova close to Earth, the results will be devastating for life on Earth. This study suggests that this may already be happening.”

An artist impression of HR 6819, a close binary consisting of deleted B-shaped stars (background) and rapidly rotating BE stars (foreground). Image credit: ESO/L. Calsada.

Astronomers came to their conclusion after conducting a large-scale census of OB stars in the sun of Kiloparscheck (approximately 3,260 light years).

They studied the distribution of these stars to learn more about how clusters of stars and galaxies form using themselves as benchmarks, and the rate at which these stars form in our galaxies.

The census allowed researchers to calculate the rate at which supernovas occur within galaxies, which are important for supernova observations, and the rates that are important for the production of large-scale star rests, such as black holes and neutron stars throughout the universe.

Data will also help in the future development of gravitational wave detectors, a useful tool for scientists studying the structure and origin of the universe.

As part of this, the researchers calculated the supernova rate within the 20 parsecs (65 light years) of the Sun and compared this to the approximate velocity rate of mass extinction events on Earth that were previously attributed to nearby supernovas.

This exclusion events linked to other factors such as asteroid impacts and ice ages.

Comparing these datasets, experts found that their studies support the theory that supernova explosions are responsible for both the late Devonian and Ordovician extinction events.

“We calculated the supernova rate close to Earth, and we found that it coincides with the speed of mass extinction events on our planet, which are related to external forces such as supernova,” Dr. Wright said.

Astronomers believe it occurs in galaxies like the Milky Way at about one or two supernovas, or even lower speeds, but the good news is that there are only two nearby stars that can reach the supernova within the next million years or so.

“But both of these are over 500 light years from the US, and computer simulations have previously suggested that supernovaes at distance from Earth are likely to not affect our planet,” the author said.

Their study It will be published in Monthly Notices from the Royal Astronomical Society.

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Alexis L. Quintana et al. 2025. Census of AB stars within 1 kpc and collapse rate of star formation and core collapse Supernova rate. mnrasin press; arxiv: 2503.08286v1

Source: www.sci.news

Research: Collaboration between oceans and continents led to Mesozoic marine extinctions

in paper Published in the journal Nature ChemistryScientists have proposed a new explanation for a series of severe environmental crises known as marine anoxia, which occurred between 185 and 85 million years ago (during the Mesozoic era) when the amount of dissolved oxygen in the oceans became extremely low.

Oceanic anoxia was a geologically abrupt phase of extreme oxygen depletion in the oceans that disrupted marine ecosystems and led to evolutionary shifts. These events, which usually lasted about 1.5 million years, occurred frequently during the Mesozoic Era, between about 183 and 85 million years ago. One hypothesis suggests that anoxia resulted from increased chemical weathering of the Earth's surface on a greenhouse world with high volcanic carbon emissions. Gernon othersA combination of plate reconstructions, tectonic geochemical analyses and global biogeochemical modelling tested this hypothesis. Image courtesy of the University of Southampton.

“Ocean anoxia is like hitting the reset button on the Earth's ecosystems,” said Prof Tom Gernon, from the University of Southampton.

“The challenge was to understand what geological forces pushed the button.”

The researchers investigated the influence of plate tectonic forces on ocean chemistry during the Jurassic and Cretaceous periods, collectively known as the Mesozoic Era.

“This period in Earth's history is also known as the Age of the Dinosaurs and is well exposed along the cliffs of the Jurassic Coast on the south coast of England, Whitby in Yorkshire and Eastbourne in East Sussex,” Prof Gernon said.

Scientists have combined statistical analysis and advanced computer modelling to investigate how the ocean's chemical cycle may have responded to the breakup of the supercontinent Gondwana, the giant landmass once home to dinosaurs.

“During the Mesozoic Era, the continents broke apart and intense volcanic activity occurred around the world,” Prof Gernon said.

“As the plates shifted and new ocean floor was formed, phosphorus, a nutrient essential to life, was released in large quantities into the ocean from weathered volcanic rocks.”

“Importantly, we found evidence of multiple instances of chemical weathering on both the ocean floor and the continents, alternating between destroying the oceans — like a geological tag team.”

The authors find that the timing of these weathering waves coincides with most of the marine anoxic events in the rock record.

They argue that phosphorus that entered the ocean through weathering acted as a natural fertilizer, promoting the growth of marine life.

However, this fertilization phenomenon came at a great cost to marine ecosystems.

“Increased biological activity caused huge amounts of organic matter to sink to the seafloor, consuming huge amounts of oxygen,” said Prof Benjamin Mills, from the University of Leeds.

“This process ultimately left large swaths of the ocean anoxic, or 'dead zones' where oxygen was depleted and most marine life died.”

“The anoxic conditions typically lasted for one to two million years and had profound effects on marine ecosystems, the effects of which are still felt today.”

“The organic-rich rocks that accumulated during these events are the source of the world's largest commercial oil and gas reserves to date.”

The findings explain the causes of extreme biological chaos during the Mesozoic Era and highlight the devastating effects of nutrient overload on marine environments today.

“Studying geological events provides valuable insights that help us understand how Earth will respond to future climatic and environmental stresses,” Professor Gernon said.

Overall, the results reveal stronger-than-expected connections between Earth's solid interior and its surface environment and biosphere, especially during periods of tectonic and climatic upheaval.

“It is remarkable how a series of events occurring inside the Earth can have such profound, often devastating, effects on the surface,” Prof Gernon said.

“Continental breakup could have profound effects on evolutionary processes.”

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TM Gernon othersSolid Earth forcing of Mesozoic oceanic anoxia. National GeographyPublished online August 29, 2024, doi: 10.1038/s41561-024-01496-0

This article has been adapted from an original release from the University of Southampton.

Source: www.sci.news