IODP Beyond 2013—Research Frontiers at the INVEST Conference
The recent INVEST Conference in Bremen, Germany, discussed the scientific research goals of IODP in the decade beyond 2013. This paper provides a brief report of the conference, and introduces five scientific frontiers to be addressed by the future IODP, namely: Interactions between the Earth′s deep and surface, hot-house climate, deep biosphere and carbon cycling, observatory system, Earth and human. The specific features of IODP in its new stage are also discussed.
Key words： IODP; INVEST; Research frontiers
IODP-China Correspondent . IODP Beyond 2013—Research Frontiers at the INVEST Conference[J]. Advances in Earth Science, 2009 , 24(12) : 1325 -1329 . DOI: 10.11867/j.issn.1001-8166.2009.12.1325
[1]IODP & Ocean Leadership. Charting the Future Course of Scientific Ocean Drilling
[R].Workshop Report February 2-March,2009:13.
[2]ECORD. Beyond 2013: The Future of European Scientific Drilling Research
[R]. Workshop Report April, 2009:24-25.
[3]J-DESC. Reports from Japanese Domestic Workshop for INVEST
[R].July,2009.
[4]InterRidge. Melting, Magma, Fluids and Life: Challenges for the next Generation of Scientific Ocean Drilling into the Oceanic Lithosphere
[R]. Workshop Report July,Southampton,NOC2009:27-29.
[5]COMPLEX. Conference on Multiple Platform Exploration on the Ocean
[R]. Vancouver BC, May,1999.
[6]Schiermeier Q. Experts draw up ocean-drilling wish list
[J].Nature,2009, 461: 578-579.
[7]Wang Pinxian. Interactions between earth′s deep and surface
[J].Advaces in Earth Science,2009,24(12): 1 331-1 338.
[汪品先.地球深部与表层的相互作用
[J].地球科学进展,2009,24(12): 1 331-1 338.]
[8]Turgeon S C, Creaser R A. Cretaceous oceanic anoxic event-triggered by a massive magnetic episode
[J].Nature,2008, 454: 323-326.
[9]Tejada M L G, Suzuki K, Kuroda J, et al. Ontong Java Plateau eruption as a trigger for the early Aptian oceanic anoxic event
[J].Geology,2009,37(9):855-858.
[10]Kuroda J, Ogawa N O, Tanimizu M,et al. Contemporaneous massive subaerial volcanism and Late Cretaceous oceanic anoxic event 2
[J].Earth and Planetary Science Letters,2007, 256: 211-222.
[11]Zachos J C, Röhl U, Schellenberg S A,et al.Rapid acidification of the ocean during the Paleocene-Eocene Thermal Maximum
[J].Science,2005, 308: 1 611-1 615.
[12]Zeebe R E, Zachos J C, Dickens G R. Carbon dioxide forcing alone insufficient to explain Paleocene-Eocene Thermal Maximum warming
[J].Nature Geoscience,2009,2:576-580.
[13]Whitman W B, Coleman D C, Wiebe W J. Prokaryotes: The unseen majority
[J].Proceedings of the Natlional Academy Sciences USA,1998,95:6 578-6 583.
[14]Ledford H. Death and life beneath the sea floor
[J].Nature,2008,454:1 038.
[15]Becker K, Davis E E. A review of CORK designs and operations during the Ocean Drilling Program
[C]∥Fisher A T, Urabe T, Klaus A,et al. Proceedings IODP, 2005,301,doi:10.2204/iodp.proc.301.104.2005.
[16]Kinoshita M, Moore G, von Huene R. The seismic zone experiment
[J].Oceanography,2006,19(4):28-38.
[17]Morgan J K, Silver E, Camerlenghi A,et al. Addressing geohazards through ocean drilling
[J].Scientific Drilling March,2009, 7: 15-20.
[18]Goodbred S L, Jr Kuhel S A. Enormous Ganges-Brahmaputra sediment discharge during strengthened early Holocene monsoon
[J].Geology,28(12):1 083-1 086.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
