Large igneous provinces and scientific ocean drilling: status quo and a look ahead

A rich mosaic of disparate crustal types characterizes the Earth beneath the sea. Although “normal” oceanic crust approximately 7-km thick is by far the most prevalent, abnormally thick oceanic-type crust of large igneous provinces (LIPs) also forms a signifi cant component of the marine realm (e.g., Coffi n and Eldholm, 1994; Mahoney and Coffin, 1997; Saunders, 2005). Scientific ocean drilling has significantly advanced understanding of LIPs. Herein we focus on significant outcomes of ten LIP-dedicated expeditions between 1985 and 2000 and also highlight prospects for future drilling efforts. The ten expeditions include three to the volcanic margins of the North Atlantic Tertiary Igneous Province, four to the Kerguelen Plateau/Broken Ridge LIP in the Indian Ocean, two to the Ontong Java Plateau in the western equatorial Pacifi c Ocean, and one to the Chagos-Maldive-Laccadive Ridge and Mascarene Plateau in the Indian Ocean (Table 1). Complementary geophysical and/or onshore geological investigations have added signifi cant value to all of these expeditions.

[1]  A. Saunders Large Igneous Provinces: Origin and Environmental Consequences , 2005 .

[2]  P. Wignall,et al.  The Link between Large Igneous Province Eruptions and Mass Extinctions , 2005 .

[3]  B. Houghton,et al.  Mafic volcaniclastic deposits in flood basalt provinces: A review , 2005 .

[4]  P. V. Keken,et al.  Multiple volcanic episodes of flood basalts caused by thermochemical mantle plumes , 2005, Nature.

[5]  H. Samuel,et al.  Beyond the thermal plume paradigm , 2005 .

[6]  A. Saunders,et al.  Volcanism, impact and mass extinctions: incredible or credible coincidences? , 2005 .

[7]  A. Malthe-Sørenssen,et al.  Release of methane from a volcanic basin as a mechanism for initial Eocene global warming , 2004, Nature.

[8]  M. Coffin,et al.  Impact Origin for the Greater Ontong Java Plateau? Geophysical and Geodynamic Evidence. , 2004 .

[9]  E. Okal,et al.  Multiple-ScS probing of the Ontong-Java Plateau , 2003 .

[10]  Jean Besse,et al.  Three distinct types of hotspots in the Earth's mantle , 2002 .

[11]  D. Jerram,et al.  Silicic volcanism: an undervalued component of large igneous provinces and volcanic rifted margins , 2002 .

[12]  K. Priestley,et al.  Structure of the crust and uppermost mantle of Iceland from a combined seismic and gravity study , 2000 .

[13]  A. Kerr,et al.  LIP Reading: Recognizing Oceanic Plateaux in the Geological Record , 2000 .

[14]  E. Okal,et al.  Rayleigh–wave tomography of the Ontong–Java Plateau , 2000 .

[15]  B. Kennett,et al.  A low seismic wavespeed anomaly beneath northwestern India: a seismic signature of the Deccan plume? , 1999 .

[16]  A. D. Saunders,et al.  Structure and deformation of north and central Malaita, Solomon Islands: tectonic implications for the Ontong Java Plateau-Solomon arc collision, and for the fate of oceanic plateaus , 1997 .

[17]  E. Stolper,et al.  An Experimental Study of Water and Carbon Dioxide Solubilities in Mid-Ocean Ridge Basaltic Liquids. Part II: Applications to Degassing , 1995 .

[18]  Marcelo Assumpção,et al.  Seismic evidence for a fossil mantle plume beneath South America and implications for plate driving forces , 1995, Nature.

[19]  J. Head,et al.  Large igneous provinces: A planetary perspective , 1997 .

[20]  O. Eldholm,et al.  Large igneous provinces: crustal structure, dimensions, and external consequences , 1994 .

[21]  T. Thordarson,et al.  The Laki (Skaftár Fires) and Grímsvötn eruptions in 1783–1785 , 1993 .

[22]  P. Renne,et al.  Rapid Eruption of the Siberian Traps Flood Basalts at the Permo-Triassic Boundary , 1991, Science.

[23]  M. Richards,et al.  Flood Basalts and Hot-Spot Tracks: Plume Heads and Tails , 1989, Science.

[24]  R. White,et al.  Magmatism at rift zones: The generation of volcanic continental margins and flood basalts , 1989 .

[25]  S. Self,et al.  Basaltic fissure eruptions, plume heights, and atmospheric aerosols , 1986 .

[26]  S. Self,et al.  Estimates of sulfur and chlorine yield to the atmosphere from volcanic eruptions and potential climatic effects , 1984 .

[27]  J. G. Moore,et al.  Vesicles, water, and sulfur in Reykjanes Ridge basalts , 1973 .

[28]  W. J. Morgan,et al.  Convection Plumes in the Lower Mantle , 1971, Nature.

[29]  J. Mahoney,et al.  Origin And Evolution of the Ontong Java Plateau , 2004 .

[30]  Klas Lackschewitz,et al.  Proceedings of the Ocean Drilling Program , 2002 .

[31]  M. F. Coffin,et al.  Earth, Oceans, and Life. Scientific Investigations of the Earth System using Multiple Drilling Platforms and New Technologies. Integrated Ocean Drilling Program Initial Science Plan, 2003-2013. , 2001 .

[32]  O. Eldholm,et al.  Large Igneous Provinces and Plate Tectonics , 2000 .

[33]  M. Gurnis,et al.  The history and dynamics of global plate motions , 2000 .

[34]  J. Mahoney,et al.  Large igneous provinces: continental, oceanic, and planetary flood volcanism , 1997 .

[35]  N. Sleep HOTSPOT VOLCANISM AND MANTLE PLUMES , 1992 .

[36]  Donald A. Swanson,et al.  Revisions to the estimates of the areal extent and volume of the Columbia River Basalt Group , 1989 .

[37]  J. Sepkoski Patterns of Phanerozoic Extinction: a Perspective from Global Data Bases , 1989 .