Rapid climate change 56 million years ago explained

London: The release of methane from the seafloor was much slower than previously thought during a rapid global warming event 56 million years ago that caused the extinction of many species, a new study has found.

The study led by researchers at the University of Southampton in the UK could allow scientists to better understand the potential effects of rising ocean temperatures worldwide on current and future climate change. Around 56 million years ago, 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.

The PETM 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, which record information about the chemical composition of the ocean in their shells, 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. This hydrate can melt if the ocean above warms, and melting of hydrate provides a widely accepted mechanism for the methane outburst.

However, the research from the University of Southampton and the National Oceanography Centre casts doubt on this mechanism. Using computer models of the warming process, 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.

"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 lead author of the study, Tim Minshull, Professor at Southampton. "This is because 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," Minshull said.

"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," he said. "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," said Professor Paul Wilson from Southampton.

"And special transport routes would have been needed - perhaps cracks and fissures - to allow the methane to rise to the seabed quickly," he added. The study appears in the journal Geophysical Research Letters.