International researchers, led by the Australian National University (ANU), have developed a new way to determine sea-level changes and deep-sea temperature variability over the past 5.3 million years.
The findings will help scientists better understand the climate surrounding ice ages over the past two million years, and could help determine the relationship between carbon dioxide levels, global temperatures and sea levels.
The team from ANU, the University of Southampton (UoS) and the National Oceanography Centre (NOC) in the United Kingdom, examined oxygen isotope levels in fossils of microscopic plankton recovered from the Mediterranean Sea, dating back as far as 5.3 million years.
"This is the first step for reconstructions from the Mediterranean records," says lead researcher Eelco Rohling from the ANU Research School of Earth Sciences.
Professor Rohling said the team focused on the flow of water through Strait of Gibraltar, which was particularly sensitive to sea-level changes.
"As continental ice sheets grew during the ice ages, flow through the Strait of Gibraltar was reduced, causing measurable changes in oxygen isotope ratios in Mediterranean waters, which became preserved in the shells of the ancient plankton," he said.
Co-author Gavin Foster from UoS said the research for the first time found long-term trends in cooling and continental ice-volume build-up cycles over the past 5.3 Million years were not the same.
"In fact, for temperature the major step toward the ice ages of the past two million years was a cooling event at 2.7 million years ago," he said.
"But for ice-volume, the crucial step was the development of the first intense ice age at around 2.15 million years ago. Before our results, these were thought to have occurred together at about 2.5 million years ago." Professor Rohling said the findings will help scientists better understand the nature of ice ages and development of coastal sediment.
|Contact: ANU Media Office|
Australian National University