Dawn of the Dinosaurs Triggered by Newly Discovered Mass Extinction Event

A life-scene from 232 million years ago, during the Carnian Pluvial Episode after which dinosaurs took over. A large rauisuchian lurks in the background, while two species of dinosaurs stand in the foreground. Credit: Davide Bonadonna

Huge volcanic eruptions 233 million years ago pumped carbon dioxide, methane and water vapour into the atmosphere. This series of violent explosions, on what we now know as the west coast of Canada, led to massive global warming. Our new research has revealed that this was a planet-changing mass extinction event that killed off many of the dominant tetrapods and heralded the dawn of the dinosaurs.

The best known mass extinction happened at the end of the Cretaceous period, 66 million years ago. This is when dinosaurs, pterosaurs, marine reptiles and ammonites all died out. This event was caused primarily by the impact of a giant asteroid that blacked out the light of the sun and caused darkness and freezing, followed by other massive perturbations of the oceans and atmosphere.

Geologists and paleontologists agree on a roster of five such events, of which the end-Cretaceous mass extinction was the last. So our new discovery of a previously unknown mass extinction might seem unexpected. And yet this event, termed the Carnian Pluvial Episode (CPE), seems to have killed as many species as the giant asteroid did. Ecosystems on land and sea were profoundly changed, as the planet got warmer and drier.

Huge volcanic eruptions changed life on Earth 233 million years ago.

On land, this triggered profound changes in plants and herbivores. In turn, with the decline of the dominant plant-eating tetrapods, such as rhynchosaurs and dicynodonts, the dinosaurs were given their chance.

The dinosaurs had originated some 15 million years earlier and our new study shows that, as a result of the CPE, they expanded rapidly in the subsequent 10 million to 15 million years and became the dominant species in the terrestrial ecosystems. The CPE triggered the “age of the dinosaurs” which lasted for a further 165 million years.

It wasn’t only the dinosaurs that were given a foothold. Many modern tetrapod groups, such as turtles, lizards, crocodiles and mammals date back to this newly discovered time of revolution.

Following the clues

This event was first noticed independently back in the 1980s. But it was thought that it was restricted to Europe. First, geologists in Germany, Switzerland, and Italy recognized a major turnover among marine faunas about 232 million years ago, termed the Rheingraben event.

Then in 1986, I recognized this independently as a global-scale turnover among tetrapods and ammonites. But at that time, the age dating was much weaker than now and it was impossible to be sure whether these were both the same event.

The jigsaw pieces started falling into place when an episode of about 1 million years of humid climates was recognized throughout the UK and parts of Europe by geologists Mike Simms and Alastair Ruffell. Then geologist Jacopo dal Corso spotted a coincidence in timing of the CPE with the peak of eruptions of the Wrangellia basalts.

Wrangellia is a term geologists give to a narrow tectonic plate that is attached to the west coast of the North American continent, north of Vancouver and Seattle.

Map showing the distribution of Wrangellia flood basalts in Alaska, Yukon and British Columbia. Credit: University of British Columbia (EOAS)

Finally, in a review of the evidence from Triassic-aged rocks, the signature of the CPE was detected – not only in Europe, but also in South America, North America, Australia and Asia. This was far from being a Europe-only event. It was global.

Volcanic eruptions

The massive Wrangellia eruptions pumped carbon dioxide, methane and water vapour into the atmosphere, leading to global warming and an increase in rainfall worldwide. There were as many as five pulses of eruptions associated with warming peaks from 233 million years ago. The eruptions led to acid rain as the volcanic gases mixed with rainwater to shower the Earth in dilute acid. Shallow oceans also became acidified.

The sharp warming drove plants and animals from the tropics and the acid rain killed plants on land, while ocean acidification attacked all marine organisms with carbonate skeletons. This stripped away the surfaces of the oceans and the land. Life may have begun to recover, but when the eruptions ceased, temperatures remained high while the tropical rainfall ceased. This is what caused the subsequent drying of the land on which the dinosaurs flourished.

Most extraordinary was the re-casting of the marine carbonate factory. This is the global mechanism by which calcium carbonate forms great thicknesses of limestones and provides material for organisms like corals and mollusks to build their shells. The CPE marked the start of modern coral reefs, as well as many of the modern groups of plankton, suggesting profound changes in ocean chemistry.

Summary of major extinction events through time, highlighting the new, Carnian Pluvial Episode at 233 million years ago. Credit: D. Bonadonna/ MUSE, Trento

Before the CPE, the main source of carbonate in the oceans came from microbial ecosystems, such as limestone-dominated mud mounds, on continental shelves. But after the CPE, it was driven by coral reefs and plankton, where new groups of micro-organisms, such as dinoflagellates, appeared and bloomed. This profound switch in fundamental chemical cycles in the oceans marked the beginning of modern marine ecosystems.

And there are going to be important lessons for how we help our planet recover from climate change. Geologists need to investigate the details of the Wrangellia volcanic activity and understand how these repeated eruptions drove the climate and changed the Earth’s ecosystems. There have been a number of volcanically-induced mass extinctions in the history of the Earth and the physical perturbations, such as global warming, acid rain, and ocean acidification, are among the challenges we see today.

Paleontologists will need to work more closely on the data from marine and continental fossil records. This will help us understand how the crisis played out in terms of the loss of biodiversity, but also to explore how the planet recovered.

Written by Michael J. Benton, Professor of Vertebrate Palaeontology, University of Bristol.

Originally published on The Conversation.

For more on this research, read Discovery of a New Mass Extinction – Carnian Pluvial Episode – 233 Million Years Ago.

DinosaursEvolutionExtinctionPaleontologyThe ConversationUniversity of Bristol
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  • Bill Simpson

    Interesting work. That area is still extremely dangerous, since it is overdue for a massive subduction zone quake, with subsequent tsunami, which will kill thousands when it does hit.

  • Alan

    False assumptions, it was asteroid that hit
    Earth that caused the “climate change”
    Get off insanity about blaming carbon Emissions
    On all that happening by deforestation
    And existing in universe of other entities
    Of which are more random and unpredictable.

  • Derek

    @Alan Are you suggesting that all climate change events occurring on Earth MUST have been driven by impact from an extraterrestrial object (asteroid, meteorite, or comet)? What makes you doubt that an entire volcano chain, pumping out copious amounts of greenhouse gases into the atmosphere (btw, NOBODY—not even modern climate change skeptics—will try to deny that CO2 is a greenhouse gas. Skeptics merely attempt claiming that humans aren’t putting out enough of it to make an impact; a skeptical claim which scientists worldwide had proven false, but I digress), can’t alter climatic conditions? Dr. Benton has included sources for his claims in this article (in the hyperlinked text scattered around the body of this article). Go read them for yourself. They seem to hold a bit more scientific weight than simply making an unfounded, baseless claim of the cause certainly having to have emanated from “[extraterrestrial] entities of which are more random and unpredictable [than volcanoes on Earth].”