ZME Science
No Result
View All Result
ZME Science
No Result
View All Result
ZME Science

Home → Environment → Environmental Issues

The most devastating mass extinction in Earth’s history happened much faster

Tibi PuiubyTibi Puiu
February 12, 2014
in Environment, Environmental Issues, Geology, News
A A
Share on FacebookShare on TwitterSubmit to Reddit

Some 252 million years ago,  96 percent of marine species and 70 percent of life on land became extinct following a yet unconfirmed series of cataclysmic events. Around this time, billions and billions of organisms were killed and life on Earth faced its most dire moments. This is known as the end-Permian extinction, and many theories have been devised trying to explain what triggered this massive die-off. A new geological analysis by scientists at MIT provides a refined time frame during which the extinction took place. Apparently, the extinction happened much faster than previously believed. Moreover, armed with this information, scientists may now test some of the leading hypotheses that try to explain the extinction.

Artist impression of how the landscape must have looked like during the end-Permian extinction. Photo: JOSÉ-LUIS OLIVARES/MIT
Artist impression of how the landscape must have looked like during the end-Permian extinction. Photo: JOSÉ-LUIS OLIVARES/MIT

Sam Bowring, the Robert R. Shrock Professor of Earth and Planetary Sciences at MIT, and team first traveled to Meishan, China in 2006. Here, geologists from all over the world have made various trips since the area holds invaluable clues  in its layers of sedimentary rock. On section of rock, in particular, is thought to delineate the end of the Permian, and the beginning of the Triassic, based on evidence such as the number of fossils found in surrounding rock layers.

A massive die-off

Their first sample analysis suggested that the  end-Permian likely lasted less than 200,000 years, as reported in 2011. Using a more refined technique, Bowring now says that they’ve reached a more accurate time-frame.  Rock samples collected from five volcanic ash beds at the Permian-Triassic boundary were pulverized, so that  tiny zircon crystals containing a mix of uranium and lead could be gathered. The researchers then separated the the lead from the uranium  and measured the ratios of both isotopes to determine the age of each rock sample.

The new measurements reveal a more precise age model for the end-Permian extinction. It likely lasted for  60,000 years — with an uncertainty of 48,000 years . In geological terms, this is nothing more than the blink of an eye. Apparently, this was too fast for most life on Earth to adapt. The samples also confirmed what was known for a while: the extinction was preceded by a sharp increase in carbon dioxide in the oceans.

What’s the killer?

Some  10,000 years before the die-off, a massive and sudden influx of carbon dioxide was released into the atmosphere, poisoning life on land and acidifying the world’s oceans. Most of the carbon was absorbed by the oceans which act like huge heat-sinks, increasing sea temperatures by as much as 10 degrees Celsius – too hot for anything to survive. It took life on Earth ten million years to recover from this event. It’s important to note that ocean acidification is happening today at a growing rate due to global warming and man-made carbon emissions.

[ANOTHER THEORY] Permian extinction caused by ‘lemon juice’ acid rain [?]

What triggered this dramatic cataclysm? The leading theory is that it was caused by long-lasting volcanic eruptions from the Siberian Traps, a region of Russia whose steplike hills are a result of repeated eruptions of magma. The eruption  released volatile chemicals, including carbon dioxide, into the atmosphere and oceans, covering an estimated five million cubic kilometers.

RelatedPosts

CIA requested to be more transparent about climate change
Record level atmospheric CO2. Reaches 400 ppm for the first time in 3 million years
Melting ice is causing the ocean to sink, worrying new study reports
This map shows what your city’s climate will be like in 2080

The new refined timeline adds weight to this theory, but it’s still too early to tell for sure. Next, Bowring plan to determine an equally precise timeline for the Siberian Traps eruptions. If the eruptions and the eruption timeline overlap, than scientists can infer with a degree of confidence that indeed that’s what caused the extinction.

“We’ve refined our approach, and now we have higher accuracy and precision,” Bowring says. “You can think of it as slowly spiraling in toward the truth.”

The report was published in the Proceedings of the National Academy of Science. 

Tags: global warmingocean acidificationpermian extinction

ShareTweetShare
Tibi Puiu

Tibi Puiu

Tibi is a science journalist and co-founder of ZME Science. He writes mainly about emerging tech, physics, climate, and space. In his spare time, Tibi likes to make weird music on his computer and groom felines. He has a B.Sc in mechanical engineering and an M.Sc in renewable energy systems.

Related Posts

Environmental Issues

The oceans are so acidic they’re dissolving the shells of marine creatures

byMihai Andrei
3 days ago
Science

With our current path, the planet is set to warm by 3 degrees Celsius. Here’s what that means

byMihai Andrei
5 months ago
Climate

Climate heating is killing the young, not the oldest

byMihai Andrei
5 months ago
Climate

First Ice-Free Day in the Arctic Could Happen by 2027, Study Warns

byMihai Andrei
6 months ago

Recent news

Science Just Debunked the ‘Guns Don’t Kill People’ Argument Again. This Time, It’s Kids

June 13, 2025

It Looks Like a Ruby But This Is Actually the Rarest Kind of Diamond on Earth

June 12, 2025

ChatGPT Got Destroyed in Chess by a 1970s Atari Console. But Should You Be Surprised?

June 12, 2025
  • About
  • Advertise
  • Editorial Policy
  • Privacy Policy and Terms of Use
  • How we review products
  • Contact

© 2007-2025 ZME Science - Not exactly rocket science. All Rights Reserved.

No Result
View All Result
  • Science News
  • Environment
  • Health
  • Space
  • Future
  • Features
    • Natural Sciences
    • Physics
      • Matter and Energy
      • Quantum Mechanics
      • Thermodynamics
    • Chemistry
      • Periodic Table
      • Applied Chemistry
      • Materials
      • Physical Chemistry
    • Biology
      • Anatomy
      • Biochemistry
      • Ecology
      • Genetics
      • Microbiology
      • Plants and Fungi
    • Geology and Paleontology
      • Planet Earth
      • Earth Dynamics
      • Rocks and Minerals
      • Volcanoes
      • Dinosaurs
      • Fossils
    • Animals
      • Mammals
      • Birds
      • Fish
      • Amphibians
      • Reptiles
      • Invertebrates
      • Pets
      • Conservation
      • Animal facts
    • Climate and Weather
      • Climate change
      • Weather and atmosphere
    • Health
      • Drugs
      • Diseases and Conditions
      • Human Body
      • Mind and Brain
      • Food and Nutrition
      • Wellness
    • History and Humanities
      • Anthropology
      • Archaeology
      • History
      • Economics
      • People
      • Sociology
    • Space & Astronomy
      • The Solar System
      • Sun
      • The Moon
      • Planets
      • Asteroids, meteors & comets
      • Astronomy
      • Astrophysics
      • Cosmology
      • Exoplanets & Alien Life
      • Spaceflight and Exploration
    • Technology
      • Computer Science & IT
      • Engineering
      • Inventions
      • Sustainability
      • Renewable Energy
      • Green Living
    • Culture
    • Resources
  • Videos
  • Reviews
  • About Us
    • About
    • The Team
    • Advertise
    • Contribute
    • Editorial policy
    • Privacy Policy
    • Contact

© 2007-2025 ZME Science - Not exactly rocket science. All Rights Reserved.