地球科学进展 ›› 2009, Vol. 24 ›› Issue (12): 1325 -1329. doi: 10.11867/j.issn.1001-8166.2009.12.1325

所属专题: IODP研究

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2013年后的大洋钻探——从INVEST会议看学科前沿
IODP-China通讯员   
  • 收稿日期:2009-11-04 修回日期:2009-11-27 出版日期:2009-12-10

IODP Beyond 2013—Research Frontiers at the INVEST Conference

IODP-China Correspondent   

  • Received:2009-11-04 Revised:2009-11-27 Online:2009-12-10 Published:2009-12-10

在德国布莱梅举行的“INVEST”大会上,讨论了2013年后10年内综合大洋钻探的学术研究方向。报道了会议概况,从深部与表层相互作用、暖室气候、深部生物圈与碳、观测系统、地球和人等5个主题,介绍了大洋钻探未来的学科前沿,并分析了大洋钻探今后发展的特点。

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.

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[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.

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