The dinosaurs were wiped out by a deadly combination of sulphur gases and climate cooling following a massive asteroid impact, new research suggests.

Experts say the gases were ejected into Earth’s atmosphere following the Chicxulub impact, then circled the globe for years which in turn cooled the planet.

This contributed to the mass extinction of life around 66 million years ago, according to University of St Andrews researchers, who said the dinosaurs were ‘just really unlucky’.

Although catastrophic for the dinosaurs and other life, the impact of a six-mile-wide asteroid in what is now the Yucatan Peninsula allowed for the diversification of mammals, including primates.  

The dinosaurs were wiped out by a deadly combination of sulphur gases and climate cooling following a massive asteroid impact, new research suggests

The dinosaurs were wiped out by a deadly combination of sulphur gases and climate cooling following a massive asteroid impact, new research suggests

The Cretaceous-Paleogene extinction

When did it happen?

66 million years ago

How many species went extinct?

76 per cent of all life on Earth 

What was the cause?

A giant asteroid impact 

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Dr Aubrey Zerkle, of the School of Earth and Environmental Sciences at the University of St Andrews, said: ‘One reason this particular impact was so devastating to life seems to be that it landed in a marine environment that was rich in sulphur and other volatiles. 

‘The dinosaurs were just really unlucky.’

The research, which was carried out alongside Syracuse University, New York, the University of Bristol, and Texas A&M University, was aimed at exploring the consequences of the Chicxulub asteroid impact. 

Sulphate aerosols had long been implicated as a primary forcing agent of the mass extinction event, which marked the end of the Cretaceous period and the start of the Paleogene period on Earth, but to what extent was not known.

The new research was able examine the rare sulphur isotopes in material ejected by the impact and deposited in a nearby sea now represented by rocks found along the Brazos River in Texas.

Dr James Witts, of the School of Earth Sciences as the University of Bristol, said: ‘Our data provided the first direct evidence for the massive amounts of sulphur released by the Chicxulub impact.

‘It’s amazing to be able to see such rapid and catastrophic global change in the geological record.’

Pictured is Darting Minnow Creek in Rosebud, Texas, where the Chicxulub impact sequence is exposed

Pictured is Darting Minnow Creek in Rosebud, Texas, where the Chicxulub impact sequence is exposed

The new research was able examine the rare sulphur isotopes in material ejected by the impact and deposited in a nearby sea now represented by rocks found along the Brazos River in Texas

The new research was able examine the rare sulphur isotopes in material ejected by the impact and deposited in a nearby sea now represented by rocks found along the Brazos River in Texas 

Atmospheric sulphur in the stratosphere scattered incoming solar radiation and prolonged planetary-scale cooling for many years after the original impact, causing acid rain and reducing the light available for photosynthesis, which is vital for plant life and marine plankton that form the base of the food chain.

Christopher Junium, of the Department of Earth and Environmental Sciences at Syracuse University, said: ‘The initial effects of the impact were caused by rock dust, soot and wildfires, but the sulphur aerosols extended the time period over which life would have suffered from extreme cooling, reduced sunlight and acidification of the land surface and oceans, and it was this extended duration of cooling that likely played a central role in the severity of the extinction.’

According to the authors, their findings suggest that the presence of sulfur can be attributed solely to the Chicxulub impact, rather than the previously theorised effects of contemporaneous volcanism in the Deccan Traps Large Igneous Province. 

The Cretaceous period, the third and final period of the Mesozoic Era, lasted from around 145 to 66 million years ago and featured a warm climate with reptiles and dinosaurs dominating the planet.

Its end was marked by the Cretaceous-Paleogene extinction event, a sudden mass extinction event which also marked the start of the Cenozoic Era in which we still live today. 

The research has been published in the journal PNAS

KILLING OFF THE DINOSAURS: HOW A CITY-SIZED ASTEROID WIPED OUT 75 PER CENT OF ALL ANIMAL AND PLANT SPECIES

Around 66 million years ago non-avian dinosaurs were wiped out and more than half the world’s species were obliterated.

This mass extinction paved the way for the rise of mammals and the appearance of humans.

The Chicxulub asteroid is often cited as a potential cause of the Cretaceous-Paleogene extinction event.

The asteroid slammed into a shallow sea in what is now the Gulf of Mexico.

The collision released a huge dust and soot cloud that triggered global climate change, wiping out 75 per cent of all animal and plant species.

Researchers claim that the soot necessary for such a global catastrophe could only have come from a direct impact on rocks in shallow water around Mexico, which are especially rich in hydrocarbons.

Within 10 hours of the impact, a massive tsunami waved ripped through the Gulf coast, experts believe.

Around 66 million years ago non-avian dinosaurs were wiped out and more than half the world's species were obliterated. The Chicxulub asteroid is often cited as a potential cause of the Cretaceous-Paleogene extinction event (stock image)

Around 66 million years ago non-avian dinosaurs were wiped out and more than half the world’s species were obliterated. The Chicxulub asteroid is often cited as a potential cause of the Cretaceous-Paleogene extinction event (stock image)

This caused earthquakes and landslides in areas as far as Argentina. 

While investigating the event researchers found small particles of rock and other debris that was shot into the air when the asteroid crashed.

Called spherules, these small particles covered the planet with a thick layer of soot.

Experts explain that losing the light from the sun caused a complete collapse in the aquatic system.

This is because the phytoplankton base of almost all aquatic food chains would have been eliminated.

It’s believed that the more than 180 million years of evolution that brought the world to the Cretaceous point was destroyed in less than the lifetime of a Tyrannosaurus rex, which is about 20 to 30 years.

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This post first appeared on Dailymail.co.uk

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