Killer 'triple burp' of methane caused
massive global warming
Space Ref.com
Source: Open University
September 15, 2005
Open University researchers have uncovered startling new evidence about an
extreme period of a sudden, fatal dose of global warming some 180 million years
ago during the time of the dinosaurs. The scientists' findings could provide
vital clues about climate change happening today and in the future.
The OU Department of Earth Sciences team, PhD student Dave Kemp and
supervisors Drs. Angela Coe and Anthony Cohen, along with Dr. Lorenz Schwark of
the University of Cologne, discovered evidence suggesting that vast amounts of
methane gas were released to the atmosphere in three massive 'methane burps' or
pulses. The addition of methane, a greenhouse gas, to the atmosphere had a
severe impact on the environment, warming Earth about 10 C, and resulting in
the extinction of a large number of species on land and in the oceans.
Dr Angela Coe says: "We've known about this event for a few years through
earlier work by our team and others, but there's been a great deal of
uncertainty about its precise size, duration, and underlying cause. What
our present study shows is that this methane release was not just one event,
but 3 consecutive pulses. Importantly, our data demonstrate that each
individual pulse was very rapid. Also, whilst the methane release was
very quick, we've found that the recovery took much longer, occurring over a
few hundred thousand years".
The methane came from gas hydrate, a frozen mixture of water and methane
found in huge quantities on the seabed. This hydrate suddenly melted, allowing
the methane to escape. The OU researchers based their findings on geochemical
analyses of mudrocks that are preserved along the Yorkshire coast near Whitby,
UK, and date from the Jurassic Period of geological time.
Dave Kemp, whose PhD is funded by the Natural Environment Research Council
(NERC), says: "The methane was released because slight wobbles in the Earth's
orbit periodically bring our planet closer to the Sun, warming the oceans
sufficiently to melt the vast reserves of hydrate. We believe that this effect
was compounded by warming from greenhouse gases from volcanoes. After the
methane was released into the atmosphere from the seabed it reacted rapidly
with oxygen to form carbon dioxide. Carbon dioxide is also a powerful
greenhouse gas that persists in the atmosphere for many hundreds of years, and
it was this gas which caused such a massive global warming effect".
Dr Anthony Cohen adds: "One of the most important aspects of the study is
that it provides an accurate timescale for how the Earth, and life, reacted to
a sudden increase in atmospheric carbon dioxide. Today we are releasing
large amounts of carbon dioxide to the atmosphere, primarily through the
burning of fossil fuels. It is possible that the rate at which carbon dioxide
is being added to the atmosphere now actually outstrips the rate at which it
was added 180 million years ago. Given that the effects were so devastating
then, it is extremely important to understand the details of past events in
order to better comprehend present-day climate change. With this
information, we are better informed about what action needs to be taken to
mitigate or avoid some of the potential detrimental future effects".
Editor's Notes
The research done by The Open University scientists is published in full by
Nature magazine on 15 September 2005.
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