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Tahiti Sea Level Expedition Examines History of Global Sea Level Change, El Niño Events

Scientists from Leicester involved in international climate change study

Scientists from the UK's University of Leicester were among colleagues from nine nations to set sail for the Integrated Ocean Drilling Program (IODP) Tahiti Sea Level Expedition, a research expedition initiated to investigate global sea level rise since the last glacial maximum, approximately 23,000 years ago.

For six weeks, aboard the DP HUNTER, the expedition science party worked on the most extensive geological research investigation ever undertaken in a coral reef area. Off the coast of Tahiti, IODP scientists took samples of fossil corals from the ocean seafloor to analyse the environmental records that are inside them.

Scientists expect the coral reefs to yield records on changes in sea surface temperature during the circumscribed period and information on climatic anomalies, including El Niño/Southern Oscillation events.

Through this research expedition, IODP scientists aim to learn more about the timing and course of past global sea level changes to better understand present and future sea level rise due to global greenhouse conditions. Since the climax of the last ice age, global sea level has risen by about 120 meters, primarily because of the melting of large inland ice sheets and thermal expansion of the global body of ocean water attributable to rising temperatures.

According to IODP scientists, Tahiti is well situated for these investigations because the island is located in a tectonically stable region. Consequently, changes in sea level here can be related solely to global effects. Because the corals off Tahiti have strict ecological requirements and are extremely sensitive to environmental changes, both natural and human-induced, they are accurate, sensitive recorders of past sea level and climatic change.

The science party analysed fossils, i.e. dead corals, because they form archives that help decipher the long-term behaviour of the tropical ocean-atmosphere system and how it has responded to manmade and natural impacts. Live corals were not cored, nor analysed.

Because corals live in a sufficiently narrow depth range, they can be used as absolute sea level indicators. Corals can be considered chronometers as they can absolutely date by radiometric methods, methods so accurate that even in the oldest coral rocks to be studied, scientists will be able to accurately determine the age of corals to within 50 years.

Tim Brewer, of the University of Leicester Department of Geology, commented:

"The University of Leicester, as part of the European Petrophysics Consortium (Universities of Leicester, Monpellier and Aachen), was responsible for the planning, acquisition and quality control/assurance for a unique suite of wireline logs which are providing important scientific information to this expedition."

Expedition co-chief scientist Yasufumi Iryu of Japan’s Tohoku University said:

“We are very excited about being able to understand these past environmental changes in such detail for the first time.”

French co-chief scientist Gilbert Camoin of the CEREGE Institute added:

“Understanding the rate at which sea level and environments have changed is vital to understanding the effects that human activity now have on Earth’s environment.”

Notes to Editors:

ESO, the ECORD (European Consortium for Ocean Research Drilling) Science Operator, is managing the Tahiti Sea Level Expedition on behalf of IODP. Co-ordinated by the British Geological Survey, ESO includes the University of Bremen and the European Petrophysics Consortium (Universities of Leicester, Montpellier, Aachen and Amsterdam). In addition to ECORD funding, ESO is supported by IODP, in part, with commingled funds from the U.S. National Science Foundation and Japan’s Ministry of Education, Culture, Science, and Technology. See www.ecord.org for more information.

The Integrated Ocean Drilling Program (IODP) is an international marine research program dedicated to advancing scientific understanding of the Earth by monitoring and sampling subseafloor environments. Through multiple platforms, IODP scientists explore the program’s principal themes: the deep biosphere, climate change, and Earth processes. Mission-specific drilling platforms are operated by the ECORD Science Operator (ESO), one of three IODP Implementing Organizations. Two others - in Japan and in the United States - conduct riser-equipped and riserless drilling operations, respectively. IODP’s initial 10-year, $1.5 billion program is supported by two lead agencies, the U.S. National Science Foundation and Japan’s Ministry of Education, Culture, Sports, Science, and Technology. ECORD and the People’s Republic of China Ministry of Science and Technology give additional support. More program information about IODP is available at www.iodp.org.

For more information, on the University of Leicester’s involvement in this project please contact Dr Tim Brewer, Department of Geology, tel 0116 252 3611, email tsb5@le.ac.uk

For other information contact:

France

Christiane Grappin

• christiane.grappin@cnrs-dir.fr
• Tel.: +33 (0) 1 44 96 43 37

UK

Andy Kingdon

• aki@bgs.ac.uk
• Tel.: +44 (0)115 936 3415 (office)
• +44 (0)7779 616 602 (mobile)

Germany and Central Europe

Albert Gerdes

• agerdes@marum.de
• Tel.: +49 421 218-655 40 (office)
• +49 172 43 77 986 (mobile)

North America

Nancy Light

• nlight@iodp.org
• Tel.: +1 (202) 465-7511
• +1 (202) 361-3325 (mobile)