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Research group Marine Isotope Geochemistry


Dr Jack Longman

Institute for Chemistry and Biology of the Marine Environment


  • Picture of several trilobite fossils which have long spines at their sides.

    Abrupt climate change at the end of the Ordovician Period (~450 million years ago) caused the second largest mass extinction in Earth history, including the demise of the trilobite, Selenopeltis (pictured, in Oxford University Museum of Natural History). Photo: Dr. Tom Gernon/University of Southampton

  • Aufgeschnittener Bohrkern mit heller Ascheschicht in der Mitte.

    Volcanic deposits both on land and on the seafloor are rapidly weathered, releasing nutrients like phosphorus to the oceans. A light ash layer is visible in this drill core from the Caribbean island of Montserrat. Foto: Dr. Tom Gernon/University of Southampton

How volcanic eruptions drove severe mass extinctions

Volcanism probably triggered a period of global cooling that caused one of the most severe mass extinctions in Earth history. A new study by Jack Longman and colleagues is looking at the mechanisms behind this event.

Volcanism probably triggered a period of global cooling that caused one of the most severe mass extinctions in Earth history. A new study by Jack Longman and colleagues is looking at the mechanisms behind this event.

Scientists at the University of Oldenburg and the University of Southampton have discovered that two intense periods of volcanism triggered a period of global cooling which caused one of the most severe mass extinctions in Earth history.

The researchers, working with colleagues at the University of Leeds and the University of Plymouth, studied the effects of volcanism on ocean chemistry during a period of extreme environmental change around 450 million years ago. Their findings are published in the journal Nature Geoscience.

This period brought about intense planetary cooling, which culminated in a glaciation and the major ‘Late Ordovician Mass Extinction’. This extinction led to the loss of about 85 percent of species dwelling in the oceans, reshaping the course of evolution of life on Earth.

“It’s been suggested that global cooling was driven by an increase in phosphorus to the oceans” says Dr Jack Longman, lead author of the study based at the University of Oldenburg, and previously a postdoctoral researcher at Southampton. “Phosphorus is one of the key elements of life, determining the pace at which tiny aquatic organisms like algae are produced”. These organisms then settle to the seabed and bury organic carbon, ultimately reducing levels of carbon dioxide (CO2) in the atmosphere, which then causes cooling.

Two distinct phases of extinction

“The unresolved puzzle is why glaciation and extinction occurred in two distinct phases at this time, separated by about 10 million years”, states Dr Tom Gernon, Associate Professor at the University of Southampton and co-author of the study. “That requires some mechanism to pulse the supply of phosphorus, which is hard to explain”.

The team identified that two exceptionally large pulses of volcanic activity across the globe, occurring in  parts of present-day North America and South China coincided very closely with the two peaks in glaciation and extinction. “But intense bursts of volcanism are more typically linked to massive CO2 release, which should drive global warming, so another process must be responsible for sudden cooling events”, explains Dr Gernon.

This prompted the team to consider whether a secondary process—natural breakdown or ‘weathering’ of the volcanic material—may have provided the surge in phosphorus need to explain the glaciations.

Release of phosphorus to the oceans

“When volcanic material is deposited in the oceans it undergoes rapid and profound chemical alteration, including release of phosphorus to the oceans,” states co-author Professor Martin Palmer from the University of Southampton. “So, it is seemed viable hypothesis and certainly one worth testing”.

“This led our team to study volcanic ash layers in much younger marine sediments to compare their phosphorus contents before and after they were modified by interactions with seawater” said Dr Hayley Manners, a lecturer in Organic Geochemistry at the University of Plymouth. Equipped with this information, the team were better placed to understand the potential geochemical impact of extensive volcanic layers from enormous eruptions during the Ordovician.

“This prompted us to develop a global biogeochemical model to understand the knock-on effects on the carbon cycle of rapidly adding a surge of phosphorus leached from volcanic deposits into the ocean”, says Dr Ben Mills, Associate Professor at the University of Leeds and co-author on the study.

The team discovered that widespread blankets of volcanic material laid down on the seafloor during the Ordovician Period would have released sufficient phosphorus into the ocean to drive a chain of events, including climatic cooling, glaciation, widespread low oxygen levels in the ocean, and mass extinction.

No cure for the current climate crisis

Whilst it might be tempting to think that seeding the oceans with phosphorus may help solve the current climate crisis, the scientists caution that this may have more damaging consequences. “Excess nutrient runoff from sources like agricultural fertilisers is a major cause of marine eutrophication – excessive plant and algae growth, which can cause substantial damage to ecosystems at the present day”, cautions Dr Mills.

The scientists conclude that whilst on short timescales massive volcanic eruptions can warm the climate via CO2 emissions, equally they can drive global cooling on multimillion-year timescales. “Our study may prompt reinvestigations of other mass extinctions during Earth history”, concludes Dr Longman.

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