Study shows erosion of ozone layer responsible for mass extinction event

Normal and malformed spores from East Greenland.

Researchers at the University of Southampton have shown that an extinction event 360 million years ago, that killed much of the Earth's plant and freshwater aquatic life, was caused by a brief breakdown of the ozone layer that shields the Earth from damaging ultraviolet (UV) radiation. This is a newly discovered extinction mechanism with profound implications for our warming world today.

There have been a number of mass extinction in the geological past. Only one was caused by an asteroid hitting the Earth, which was 66 million years ago when the dinosaurs became extinct. Three of the others, including the end Permian Great Dying, 252 million years ago, were caused by huge continental scale volcanic eruptions that destabilised the Earth's atmospheres and oceans.

Now, scientists have found evidence showing it was high levels of UV radiation which collapsed forest ecosystems and killed off many species of fish and tetrapods (our four limbed ancestors) at the end of the Devonian geological period, 359 million years ago. This damaging burst of UV radiation occurred as part of one of the Earth's climate cycles, rather than being caused by a huge volcanic eruption.

The ozone collapse occurred as the climate rapidly warmed following an intense ice age and the researchers suggest that the Earth today could reach comparable temperatures, possibly triggering a similar event. Their findings are published in the journal Science Advances.

The team collected rock samples during expeditions to mountainous polar-regions in East Greenland, which once formed a huge ancient lake bed in the arid interior of the Old Red Sandstone Continent, made up of Europe and North America. This lake was situated in the Earth's southern hemisphere and would have been similar in nature to modern day Lake Chad on the edge of the Sahara Desert.

Other rocks were collected from the Andean Mountains above Lake Titicaca in Bolivia. These South American samples were from the southern continent of Gondwana, which was closer to the Devonian South Pole. They held clues as to what was happening at the edge of the melting Devonian ice sheet, allowing a comparison between the extinction event close to the pole and close to the equator.

Back in the lab, the rocks were dissolved in hydrofluoric acid, releasing microscopic plant spores (like pollen, but from fern like plants that didn't have seeds or flowers) which had lain preserved for hundreds of millions of years. On microscopic examination, the scientists found many of the spores had bizarrely formed spines on their surface—a response to UV radiation damaging their DNA. Also, many spores had dark pigmented walls, thought to be a kind of protective 'tan', due to increased and damaging UV levels.

The scientists concluded that, during a time of rapid global warming, the ozone layer collapsed for a short period, exposing life on Earth to harmful levels of UV radiation and triggering a mass extinction event on land and in shallow water at the Devonian-Carboniferous boundary.

Prof John Marshall (left), taking samples in Spitsbergen.Prof John Marshall (left), taking samples in Spitsbergen.

Following melting of the ice sheets, the climate was very warm, with the increased heat above continents pushing more naturally generated ozone destroying chemicals into the upper atmosphere. This let in high levels of UV-B radiation for several thousand years.

Lead researcher Professor John Marshall, of the University of Southampton's School of Ocean and Earth Science, who is a National Geographic Explorer, comments: "Our ozone shield vanished for a short time in this ancient period, coinciding with a brief and quick warming of the Earth. Our ozone layer is naturally in a state of flux—constantly being created and lost—and we have shown this happened in the past too, without a catalyst such as a continental scale volcanic eruption."

During the extinction, plants selectively survived, but were enormously disrupted as the forest ecosystem collapsed. The dominant group of armoured fish became extinct. Those that survived—sharks and bony fish—remain to this day the dominant fish in our ecosystems.

These extinctions came at a key time for the evolution of our own ancestors, the tetrapods. These early tetrapods are fish that evolved to have limbs rather than fins, but still mostly lived in water. Their limbs possessed many fingers and toes. The extinction reset the direction of their evolution with the post-extinction survivors being terrestrial and with the number of fingers and toes reduced to five.

Cartoon showing the hypotheses processes that led to ozone breakdown and plant extinctions. High continental summer temperatures (A) cause increased transport of water vapour into the stratosphere together with naturally occurring fluorocarbons. These fluorocarbons catalytically promote the breakdown of ozone (B) leading to increased UV-B radiation getting to the Earth’s surface. This UV-B radiation (C) damages the DNA of the cells of spores and pollen before they can form the protective resistant outer wall layer that are the fossil parts we can recover. The DNA damage is expressed as damage to the spines that cover the outer wall of the spores. The DNA damage also makes the parent plants unable to reproduce successfully and they become globally or locally extinct collapsing the forest ecosystem. Collapsing the ecosystem exposes the paleosols beneath the forest to erosion and there is a nutrient flush to the oceans. Sea-levels had rapidly risen following collapse of the latest Devonian ice sheets and shallow shelf seas (D) have developed around the Devonian land areas. Plankton productivity by prasinophyte algae was high in these nutrient rich shelf-seas and with slow water circulation the water columns were stratified. The lower stratified water layer lacked oxygen and therefore preserved any organic matter that fell through it with the seabed sediment having high contents of organic carbon. This organic carbon had ultimately come from photosynthesis that used atmospheric carbon dioxide. This process removed carbon dioxide from the atmosphere and led to global cooling. So, as the warm post glacial climate cycle passed its peak the ozone layer could rebuild and surviving plants and animals became re-established into very different ecosystems.

Professor Marshall says his team's findings have startling implications for life on Earth today: "Current estimates suggest we will reach similar global temperatures to those of 360 million years ago, with the possibility that a similar collapse of the ozone layer could occur again, exposing surface and shallow sea life to deadly radiation. This would move us from the current state of climate change, to a climate emergency."

The remote locations visited in East Greenland are very difficult to access, with travel involving light aircraft capable of landing directly on the tundra. Transport within the vast field area was by inflatable boats equipped with outboard motors, all of which had to fit in the small aircraft.

All field logistics was organised by CASP, an independent charitable trust based in Cambridge specialising in remote geological fieldwork. Mike Curtis, Managing Director of CASP says: "We have a history of assisting research geologists such as John Marshall and colleagues to access remote field areas and we are particularly pleased that their research has proved to have such potentially profound implications."

More information: J.E.A. Marshall el al., "UV-B radiation was the Devonian-Carboniferous boundary terrestrial extinction kill mechanism," Science Advances (2020). DOI: 10.1126/sciadv.aba0768 ,

Journal information: Science Advances

Provided by University of Southampton

Video can be accessed at source link below.


By University of Southampton
(Source:; May 27, 2020;
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