The release of methane from the seafloor was much slower than previously thought during a rapid global warming event 56 million years ago, suggests new research led by University of Southampton.
The findings could allow scientists to better understand the potential effects of rising ocean temperatures worldwide on current and future climate change.
“Our results show that hydrate melting can indeed be triggered by ocean temperature change, but the result is not necessarily a rapid outburst of methane,” said professor Tim Minshull from Ocean and Earth Science at University of Southampton.
During the Paleocene-Eocene Thermal Maximum (PETM), temperatures in the deep ocean rose by about five degrees Celsius and sea surface temperatures increased by up to nine degrees Celsius.
This hot period lasted for about 100,000 years and caused the extinction of many species.
Based on evidence from tiny fossils deposited in sediments at the bottom of the ocean, current theories suggest that at the same time as the warming, there was a massive release of methane gas from the solid earth into the ocean and atmosphere.
A large proportion of the Earth’s methane is stored beneath the oceans in the form of an ice-like material called hydrate.
Using computer models, the researchers simulated the effects of PETM ocean warming on sediments that may have contained methane hydrate and tracked how methane transport mechanisms would have affected its release into seawater.
“The methane gas formed by hydrate melting below the sea floor takes time to travel up to the seabed, and on the way it can refreeze or dissolve and then be consumed by microbes that live below the seabed,” informed Minshull.
Only a fraction of the methane may escape into the ocean and the part that does escape may take thousands of years to do so.
“To explain the geological observations by melting of hydrate, much more hydrate must have been present globally than is perhaps reasonable for such a warm late Palaeocene Ocean,” added co-author professor Paul Wilson.
Special transport routes would have been needed – perhaps cracks and fissures – to allow the methane to rise to the seabed quickly.
Observations of present-day hydrate melting and methane release in several parts of the world have led to suggestions that this process might be happening right now, the authors noted in a study published in the journal Geophysical Research Letters.