Extreme crustal oxygen isotope signatures preserved in coesite in diamond
The anomalously high and low oxygen isotope values observed in eclogite xenoliths from the upper mantle beneath cratons have been interpreted as indicating that the parent rock of the eclogites experienced alteration on the ancient sea floor. Recognition of this genetic lineage has provided the foun...
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| Veröffentlicht in: | Nature (London) 2003-05, Vol.423 (6935), p.68-70 |
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| creator | SCHULZE, Daniel J HARTE, Ben VALLEY, John W BRENAN, James M DE R. CHANNER, Dominic M |
| description | The anomalously high and low oxygen isotope values observed in eclogite xenoliths from the upper mantle beneath cratons have been interpreted as indicating that the parent rock of the eclogites experienced alteration on the ancient sea floor. Recognition of this genetic lineage has provided the foundation for a model of the evolution of the continents whereby imbricated slabs of oceanic lithosphere underpin and promote stabilization of early cratons. Early crustal growth is thought to have been enhanced by the addition of slab-derived magmas, leaving an eclogite residuum in the upper mantle beneath the cratons. But the oxygen isotope anomalies observed in eclogite xenoliths are small relative to those in altered ocean-floor basalt and intermediate-stage subduction-zone eclogites, and this has hindered acceptance of the hypothesis that the eclogite xenoliths represent subducted and metamorphosed ocean-floor basalts. We present here the oxygen isotope composition of eclogitic mineral inclusions, analysed in situ in diamonds using an ion microprobe/secondary ion mass spectrometer. The oxygen isotope values of coesite (a polymorph of SiO2) inclusions are substantially higher than previously reported for xenoliths from the subcratonic mantle, but are typical of subduction-zone meta-basalts, and accordingly provide strong support for the link between altered ocean-floor basalts and mantle eclogite xenoliths. |
| doi_str_mv | 10.1038/nature01615 |
| format | Article |
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CHANNER, Dominic M</creator><creatorcontrib>SCHULZE, Daniel J ; HARTE, Ben ; VALLEY, John W ; BRENAN, James M ; DE R. CHANNER, Dominic M</creatorcontrib><description>The anomalously high and low oxygen isotope values observed in eclogite xenoliths from the upper mantle beneath cratons have been interpreted as indicating that the parent rock of the eclogites experienced alteration on the ancient sea floor. Recognition of this genetic lineage has provided the foundation for a model of the evolution of the continents whereby imbricated slabs of oceanic lithosphere underpin and promote stabilization of early cratons. Early crustal growth is thought to have been enhanced by the addition of slab-derived magmas, leaving an eclogite residuum in the upper mantle beneath the cratons. But the oxygen isotope anomalies observed in eclogite xenoliths are small relative to those in altered ocean-floor basalt and intermediate-stage subduction-zone eclogites, and this has hindered acceptance of the hypothesis that the eclogite xenoliths represent subducted and metamorphosed ocean-floor basalts. We present here the oxygen isotope composition of eclogitic mineral inclusions, analysed in situ in diamonds using an ion microprobe/secondary ion mass spectrometer. The oxygen isotope values of coesite (a polymorph of SiO2) inclusions are substantially higher than previously reported for xenoliths from the subcratonic mantle, but are typical of subduction-zone meta-basalts, and accordingly provide strong support for the link between altered ocean-floor basalts and mantle eclogite xenoliths.</description><identifier>ISSN: 0028-0836</identifier><identifier>EISSN: 1476-4687</identifier><identifier>DOI: 10.1038/nature01615</identifier><identifier>PMID: 12721625</identifier><identifier>CODEN: NATUAS</identifier><language>eng</language><publisher>London: Nature Publishing</publisher><subject>Basalt ; Cratons ; Crystalline rocks ; Diamonds ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Igneous and metamorphic rocks petrology, volcanic processes, magmas ; Isotope geochemistry ; Isotope geochemistry. Geochronology ; Isotopes ; Lithosphere ; Ocean floor ; Oxygen ; Oxygen isotopes ; Slabs ; Upper mantle</subject><ispartof>Nature (London), 2003-05, Vol.423 (6935), p.68-70</ispartof><rights>2003 INIST-CNRS</rights><rights>COPYRIGHT 2003 Nature Publishing Group</rights><rights>Copyright Macmillan Journals Ltd. 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CHANNER, Dominic M</creatorcontrib><title>Extreme crustal oxygen isotope signatures preserved in coesite in diamond</title><title>Nature (London)</title><addtitle>Nature</addtitle><description>The anomalously high and low oxygen isotope values observed in eclogite xenoliths from the upper mantle beneath cratons have been interpreted as indicating that the parent rock of the eclogites experienced alteration on the ancient sea floor. Recognition of this genetic lineage has provided the foundation for a model of the evolution of the continents whereby imbricated slabs of oceanic lithosphere underpin and promote stabilization of early cratons. Early crustal growth is thought to have been enhanced by the addition of slab-derived magmas, leaving an eclogite residuum in the upper mantle beneath the cratons. 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The oxygen isotope values of coesite (a polymorph of SiO2) inclusions are substantially higher than previously reported for xenoliths from the subcratonic mantle, but are typical of subduction-zone meta-basalts, and accordingly provide strong support for the link between altered ocean-floor basalts and mantle eclogite xenoliths.</description><subject>Basalt</subject><subject>Cratons</subject><subject>Crystalline rocks</subject><subject>Diamonds</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Igneous and metamorphic rocks petrology, volcanic processes, magmas</subject><subject>Isotope geochemistry</subject><subject>Isotope geochemistry. 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CHANNER, Dominic M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Extreme crustal oxygen isotope signatures preserved in coesite in diamond</atitle><jtitle>Nature (London)</jtitle><addtitle>Nature</addtitle><date>2003-05-01</date><risdate>2003</risdate><volume>423</volume><issue>6935</issue><spage>68</spage><epage>70</epage><pages>68-70</pages><issn>0028-0836</issn><eissn>1476-4687</eissn><coden>NATUAS</coden><abstract>The anomalously high and low oxygen isotope values observed in eclogite xenoliths from the upper mantle beneath cratons have been interpreted as indicating that the parent rock of the eclogites experienced alteration on the ancient sea floor. Recognition of this genetic lineage has provided the foundation for a model of the evolution of the continents whereby imbricated slabs of oceanic lithosphere underpin and promote stabilization of early cratons. Early crustal growth is thought to have been enhanced by the addition of slab-derived magmas, leaving an eclogite residuum in the upper mantle beneath the cratons. But the oxygen isotope anomalies observed in eclogite xenoliths are small relative to those in altered ocean-floor basalt and intermediate-stage subduction-zone eclogites, and this has hindered acceptance of the hypothesis that the eclogite xenoliths represent subducted and metamorphosed ocean-floor basalts. We present here the oxygen isotope composition of eclogitic mineral inclusions, analysed in situ in diamonds using an ion microprobe/secondary ion mass spectrometer. The oxygen isotope values of coesite (a polymorph of SiO2) inclusions are substantially higher than previously reported for xenoliths from the subcratonic mantle, but are typical of subduction-zone meta-basalts, and accordingly provide strong support for the link between altered ocean-floor basalts and mantle eclogite xenoliths.</abstract><cop>London</cop><pub>Nature Publishing</pub><pmid>12721625</pmid><doi>10.1038/nature01615</doi><tpages>3</tpages></addata></record> |
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| ispartof | Nature (London), 2003-05, Vol.423 (6935), p.68-70 |
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| subjects | Basalt Cratons Crystalline rocks Diamonds Earth sciences Earth, ocean, space Exact sciences and technology Igneous and metamorphic rocks petrology, volcanic processes, magmas Isotope geochemistry Isotope geochemistry. Geochronology Isotopes Lithosphere Ocean floor Oxygen Oxygen isotopes Slabs Upper mantle |
| title | Extreme crustal oxygen isotope signatures preserved in coesite in diamond |
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