The study includes the first detailed reconstruction of the Southern Ocean density of the period and identified how it changed as the Earth warmed. It suggests a massive reorganisation of ocean temperature and salinity, but finds that this was not the driver of increased concentration of carbon dioxide in the atmosphere. The study, led by researchers from the University of Cambridge, is published in the journal Proceedings of the National Academy of Sciences.

The ocean is made up of different layers of varying densities and chemical compositions. During the last ice age, it was thought that the deepest part of the ocean was made up of very salty, dense water, which was capable of trapping a lot of CO₂. Scientists believed that a decrease in the density of this deep water resulted in the release of CO₂ from the deep ocean to the atmosphere.

However, the new findings suggest that although a decrease in the density of the deep ocean did occur, it happened much later than the rise in atmospheric CO₂, suggesting that other mechanisms must be responsible for the release of CO₂ from the oceans at the end of the last ice age.

"We set out to test the idea that a decrease in ocean density resulted in a rise in CO₂ by reconstructing how it changed across time periods when the Earth was warming," said the paper's lead author Jenny Roberts, a PhD student in Cambridge's Department of Earth Sciences who is also a member of the British Antarctic Survey. "However what we found was not what we were expecting to see."

In order to determine how the oceans have changed over time and to identify what might have caused the massive release of CO₂, the researchers studied the chemical composition of microscopic shelled animals that have been buried deep in ocean sediment since the end of the ice age. Like layers of snow, the shells of these tiny animals, known as foraminifera, contain clues about what the ocean was like while they were alive, allowing the researchers to reconstruct how the ocean changed as the ice age was ending.

They found that during the cold glacial periods, the deepest water was significantly denser than it is today. However, what was unexpected was the timing of the reduction in the deep ocean density, which happened some 5,000 years after the initial increase in CO₂, meaning that the density decrease couldn't be responsible for releasing CO₂ to the atmosphere.

"Before this study there were these two observations, the first was that glacial deep water was really salty and dense, and the second that it also contained a lot of CO₂, and the community put two and two together and said these two observations must be linked," said Roberts. "But it was only through doing our study, and looking at the change in both density and CO₂ across the deglaciation, that we found they actually weren't linked. This surprised us all."

Through examination of the shells, the researchers found that changes in CO₂ and density are not nearly as tightly linked as previously thought, suggesting something else must be causing CO₂ to be released from the ocean.

Like a bottle of wine with a cork, sea ice can prevent CO₂-rich water from releasing its CO₂ to the atmosphere. The Southern Ocean is a key area of exchange of CO₂ between the ocean and atmosphere. The expansion of sea ice during the last ice age acted as a 'lid' on the Southern Ocean, preventing CO₂ from escaping. The researchers suggest that the retreat of this sea ice lid at the end of the last ice age uncorked this vintage CO₂, resulting in an increase in carbon dioxide in the atmosphere.

"Although conditions at the end of the last ice age were very different to today, this study highlights the importance that dynamic features such as sea ice have on regulating the climate system, and emphasises the need for improved understanding and prediction as we head into our ever warming world," said Roberts.

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The above post is reprinted from materials provided by University of Cambridge. The original story is licensed under a Creative Commons Licence. Note: Materials may be edited for content and length.