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 will analyze fossil, i.e. dead corals, because they form archives that help decipher the long-term behavior of the tropical ocean-atmosphere system and how it has responded to manmade and natural impacts. Live corals will not be cored, nor analyzed.
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.
Expedition co-chief scientist Yasufumi Iryu of Japan's Tohoku University says, "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 adds, "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."
At the conclusion of the expedition, the fossil coral core material will be shipped to an IODP core repository located at the University of Bremen, Germany. In mid-February 2006, IODP scientists will gather again in Bremen to further analyze the fossil corals and associated reef rocks in greater detail.
More about the science party's activities will be posted during the course of the expedition at http://www.ecord.org (general information) or http://www.iodp.de (expedition logbook).
ESO, the ECORD (European Consortium for Ocean Research Drilling) Science Operator, is managing the Tahiti Sea Level Expedition on behalf of IODP. Coordinated 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 http://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 http://www.iodp.org.
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