Scientists found that cooling coincided with a large-scale volcanic event, which restricted the flow of ocean water and the associated heat that it carried from the equator towards the North Pole region. (Representational Image/IStock)
London:
A large-scale volcanic event during the Jurassic Period may have caused the 'ice-age' that took place on Earth around 170 million years ago, a new study has found.
Researchers have found evidence of a large and abrupt cooling of the Earth's temperature during the Jurassic Period, which lasted millions of years.
Scientists found that the cooling coincided with a large-scale volcanic event - called the North Sea Dome - which restricted the flow of ocean water and the associated heat that it carried from the equator towards the North Pole region.
The team suggests that it is this volcanic event, preventing the ocean flow, rather than a change in carbon dioxide (CO2) in the atmosphere (which causes today's climate change), that led to an extended Ice age in a period more synonymous with very warm conditions.
"We tend to think of the Jurassic as a warm 'greenhouse' world where high temperatures were governed by high atmospheric carbon dioxide contents," said Stephen Hesselbo, professor at Camborne School of Mines in UK.
"This new study suggests that re-organisation of oceanic current patterns may also have triggered large scale climate changes," said Hesselbo.
Rather than the seven continents that cover Earth's surface today, during the Jurassic Period there was one single 'supercontinent', called Pangaea.
This supercontinent had a broad seaway across it that connected a north polar sea to a warm equatorial ocean, called Tethys.
The team of scientists spent 10 years constructing a record of seawater temperature change using fossil mollusc shells.
They found that during the same period that the North Sea Dome event occurred, the Earth experienced a significant and fast cooling in temperature.
The team has hypothesised that this volcanic event restricted the poleward flow of ocean water and associated heat, flipping the northern hemisphere from a very warm climate to a cold climate state.
The evidence indicates that this cold period lasted many millions of years, until the North Sea Dome subsided.
"Although we have known about the occurrence of cold periods during greenhouse times for a while, their origins have remained mysterious," said Hesselbo.
"This work suggests a mechanism at play that may also have been important for driving other climate change events in the Jurassic and at other times in the Earth's history," he said.
The study was published in the journal Nature Communications.
Researchers have found evidence of a large and abrupt cooling of the Earth's temperature during the Jurassic Period, which lasted millions of years.
Scientists found that the cooling coincided with a large-scale volcanic event - called the North Sea Dome - which restricted the flow of ocean water and the associated heat that it carried from the equator towards the North Pole region.
The team suggests that it is this volcanic event, preventing the ocean flow, rather than a change in carbon dioxide (CO2) in the atmosphere (which causes today's climate change), that led to an extended Ice age in a period more synonymous with very warm conditions.
"We tend to think of the Jurassic as a warm 'greenhouse' world where high temperatures were governed by high atmospheric carbon dioxide contents," said Stephen Hesselbo, professor at Camborne School of Mines in UK.
"This new study suggests that re-organisation of oceanic current patterns may also have triggered large scale climate changes," said Hesselbo.
Rather than the seven continents that cover Earth's surface today, during the Jurassic Period there was one single 'supercontinent', called Pangaea.
This supercontinent had a broad seaway across it that connected a north polar sea to a warm equatorial ocean, called Tethys.
The team of scientists spent 10 years constructing a record of seawater temperature change using fossil mollusc shells.
They found that during the same period that the North Sea Dome event occurred, the Earth experienced a significant and fast cooling in temperature.
The team has hypothesised that this volcanic event restricted the poleward flow of ocean water and associated heat, flipping the northern hemisphere from a very warm climate to a cold climate state.
The evidence indicates that this cold period lasted many millions of years, until the North Sea Dome subsided.
"Although we have known about the occurrence of cold periods during greenhouse times for a while, their origins have remained mysterious," said Hesselbo.
"This work suggests a mechanism at play that may also have been important for driving other climate change events in the Jurassic and at other times in the Earth's history," he said.
The study was published in the journal Nature Communications.
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