Mass extinctions and climate change: why the speed of rising greenhouse gases matters
Coral bleaching is the 'canary in the coal mine' and suggests the present rate of climate change is too fast for many species to adapt, write Katrin Meissner and Kaitlin Alexander.
Published on the 24 Mar 2016 by Katrin Meissner and Kaitlin Alexander
OPINION: We now know that greenhouse gases are rising faster than at any time since the demise of dinosaurs, and possibly even earlier. According to research published in Nature Geoscience this week, carbon dioxide (CO₂) is being added to the atmosphere at least ten times faster than during a major warming event about 50 million years ago.
In the past, rapid increases in greenhouse gases have been associated with mass extinctions. It is therefore important to understand how unusual the current rate of atmospheric CO₂ increase is with respect to past climate variability.
Into the ice ages
There is no doubt that atmospheric CO₂ concentrations and global temperatures have changed in the past.
During this time, the Earth oscillated between cold ice ages and warm “interglacials”. To move from an ice age to an interglacial, you need to increase CO₂ by roughly 100 ppm. This increase repeatedly melted several kilometre-thick ice sheets that covered the locations of modern cities like Toronto, Boston, Chicago or Montreal.
The most prominent of these events was the Palaeocene Eocene Thermal Maximum (PETM). This event resulted in one of the largest known extinctions of life forms in the deep ocean. Atmospheric temperatures increased by 5-8C within a few thousand years.
The new research, led by Professor Richard Zeebe of the University of Hawaii, analysed ocean sediments to quantify the lag between warming and changes in the carbon cycle during the PETM.
Although climate archives become less certain the further we look back, the authors found that the carbon release must have been below 1.1 billion tonnes of carbon per year. That is about one-tenth of the rate of today’s carbon emissions from human activities such as burning fossil fuels.
What happens when the brakes are off?
Although the PETM resulted in one of the largest known deep sea extinctions, it is a small event when compared to the five major extinctions in the past.
The Permian-Triassic Boundary extinction, nicknamed “The Great Dying”, wiped out 90% of marine species and 70% of land vertebrate families 250 million years ago. Like its four brothers, this extinction event happened a very long time ago. Climate archives going that far back lack the resolution needed to reliably reconstruct rates of change.
There is, however, evidence for extensive volcanic activity during the Great Dying, which would have led to a release of CO₂ as well as the potential release of methane along continental margins. Ocean acidification caused by high atmospheric CO₂ concentrations and acid rain have been put forward as potential killer mechanisms.
These past warming events occurred without human influence. They point to the existence of positive feedbacks within the climate system that have the power to escalate warming dramatically. The thresholds to trigger these feedbacks are hard to predict and their impacts are hard to quantify.
Some examples of feedbacks include the melting of permafrost, the release of methane hydrates from ocean sediments, changes in the ocean carbon cycle, and changes in peatlands and wetlands. All of these processes have the potential to quickly add more greenhouse gases to the atmosphere.
Given that these feedbacks were strong enough in the past to wipe out a considerable proportion of life forms on Earth, there is no reason to believe that they won’t be strong enough in the near future, if triggered by sufficiently rapid warming.
Today’s rate of change in atmospheric CO₂ is unprecedented in climate archives. It outpaces the carbon release during the most extreme abrupt warming events in the past 66 million years by at least an order of magnitude.
We are therefore unable to rely upon past records to predict if and how our ecosystems will be able to adapt. We know, however, that mass extinctions have occurred in the past and that these extinctions, at least in the case of the PETM, were triggered by much smaller rates of change.
Katrin Meissner is Associate Professor, Climate Change Research Centre, UNSW.
Kaitlin Alexander is a PhD Candidate, Climate Change Research Centre and ARC Centre of Excellence for Climate System Science, UNSW.