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Crustal signature of δ 13C and nitrogen content in microdiamonds from Erzgebirge, Germany: Ion microprobe studies

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Abstract

The study of δ 13CPDB (Pee Dee Belemnite) and nitrogen contents in 1 to 5-μm-diameter microdiamonds included in garnets from the quartz-feldspathic gneisses (Erzgebirge, Germany) was performed in situ with the Nano-scale Secondary Ion Mass Spectrometer. The results revealed that there were two stages of diamond crystallization from a C-O-H supecritical fluid rich in biogenic carbon and diverse minor elements of crustal origin. The δ 13CPDB of the Erzgebirge diamond of the first stage falls in the range −17‰ to 19‰, with an average value of −17.8‰; the average content of nitrogen is 820 ppm. Diamonds of the second stage are characterized by δ 13CPDB=−21.5‰ to −25.5‰, with an average value of −23.24‰; the average nitrogen content is non-homogeneously scattered from 740 ppm to 3 370 ppm among 6 diamonds situated in garnets within the same polished rock slide. Both diamond of the first stage and diamond of the second stage carbon reservoirs belong to biogenic matter, therefore confirming deep subduction of the continental crust sediments and their subsequent exhumation during the Variscan orogeny.

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References Cited

  • Cartigny, P., Boyd, S. R., Harris, J. W., et al., 1997. Nitrogen Istopes in Peridotitic Diamonds from Fuxian, China: The Mantle Signature. Terra Nova, 9(4): 175–179

    Article  Google Scholar 

  • Cartigny, P., de-Corte, K., Shatsky, V. S., et al., 2001. The Origin and Formation of Metamorphic Microdiamonds from the Kokchetav Massif, Kazakhstan: A Nitrogen and Carbon Isotopic Study. Chem. Geol., 176(1–4): 265–281

    Article  Google Scholar 

  • Cartigny, P., Harris, J. W., Taylor, A., et al., 2003. On the Possibility of a Kinetic Fractionation of Nitrogen Stable Isotopes during Natural Diamond Growth. Geochim. Cosmochim. Acta, 67(8): 1571–1576

    Article  Google Scholar 

  • Chopin, C., Sobolev, N. V., 1995. Principal Mineralogic Indicators of UHP in Crustal Rocks. In: Coleman, R. G., Wang, X., eds., Ultrahigh Pressure Metamorphism. Cambridge University Press, London. 96–131

    Chapter  Google Scholar 

  • de-Corte, K., Cartigny, P., Shatsky, V. S., et al., 1998. Evidence of Fluid Inclusions in Metamorphic Microdiamonds from the Kokchetav Massif, Northern Kazakhstan. Geochim. Cosmochim. Acta, 62(23–24): 3765–3773

    Article  Google Scholar 

  • Dobrzhinetskaya, L. F., Eide, E. A., Larsen, R. B., et al., 1995. Microdiamond in High Grade Metamorphic Rocks of the Western Gneiss Region, Norway. Geology, 23: 597–600

    Article  Google Scholar 

  • Dobrzhinetskaya, L. F., Green, H. W., Mitchell, T. E., et al., 2001. Metamorphic Diamonds: Mechanism of Growth and Inclusion of Oxides. Geology, 29: 263–266

    Article  Google Scholar 

  • Dobrzhinetskaya, L. F., Green, H. W., Weschler, M., et al., 2003a. Focused Ion Beam Technique and Transmission Electron Microscope Studies of Microdiamonds from the Saxonian Erzgebirge, Germany. Earth Planet. Sci. Lett., 210(3–4): 399–410

    Article  Google Scholar 

  • Dobrzhinetskaya, L. F., Green, H. W., Bozhilov, K. N., et al., 2003b. Crystallization Environment of Kazakhstan Microdiamonds: Evidence from Nanometric Inclusions and Mineral Associations. J. Metamorph. Geol., 21(5): 425–437

    Article  Google Scholar 

  • Dobrzhinetskaya, L. F., Liu, Z. X., Cartigny, P., et al., 2006. Synchrotron Infrared and Raman Spectroscopy of Microdiamonds from Erzgebirge, Germany. Earth Planet. Sci. Lett., 248(1–2): 340–349

    Google Scholar 

  • Dobrzhinetskaya, L., Wirth, R., 2010. Ultradeep Mantle Rocks and Diamonds in the Light of Advanced Scientific Technologies. In: Cloethingh, S., Negendank, J., eds., New Frontiers of Integrated Earth. Springer, Netherlands. 373–395

    Google Scholar 

  • Dobrzhinetskaya, L. F., Wirth, R., Green, H. W., 2007. A Look inside of Diamond-Forming Media in Deep Subduction Zones. Proceed. Nat. Acad. Sci. USA, 104(22): 9128–9132

    Article  Google Scholar 

  • Gross, J., Burchard, M., Schertl, H. P., et al., 2008. Common High-Pressure Metamorphic History of Eclogite Lenses and Surrounding Metasediments: A Case Study of Calc-Silicate Reaction Zones (Erzgebirge, Germany). Eur. J. Miner., 20: 757–775

    Article  Google Scholar 

  • Hoefs, J., 2004. Stable Isotopes Geochemistry. 5th Edition. Springler-Verlag, Berlin-Heidelberg, New York. 244

    Google Scholar 

  • Hwang, S. L., Chu, H. T., Yui, T. F., et al., 2006. Nanometer-Size P/K-Rich Silica Glass (Former Melt) Inclusions in Microdiamond from the Gneisses of Kokchetav and Erzgebirge Massifs: Diversified Characteristics of Formation Media of Metamorphic Microdiamonds in UHP Rocks due to Host-Rock Buffering. Earth Planet. Sci. Lett., 243(1–2): 94–106

    Article  Google Scholar 

  • Hwang, S. L., Shen, P. Y., Chu, H. T., et al., 2000. Nanometer-Size-PbO2-Type TiO2 in Garnet: A Thermobarometer for Ultrahigh-Pressure Metamorphism. Science, 288(5464): 321–324

    Article  Google Scholar 

  • Kröener, A., Willner, A. P., 1998. Time of Formation and Peak of Variscan HP-HT Metamorphism of Quartz-Feldspar Rocks in the Central Erzgebirge, Saxony, Germany. Contr. Mineral. Petrol., 132(1): 1–20

    Article  Google Scholar 

  • Massonne, H. J., 1999. A New Occurrence of Microdiamonds in Quartzofeldspathic Rocks of the Saxonian Erzgebirge, Germany, and Their Metamorphic Evolution. In: Gurney, J. J., Gurney, J. L., Pascoe, M. D., et al., eds., Proceedings of the 7th International Kimberlite Conference—1999, vol. 2. Red Roof Design cc, Cape Town, South Africa. 533–539

  • Massonne, H. J., 2003. A Comparison of the Evolution of Diamondiferous Quartz-Rich Rocks from the Saxonian Erzgebirge and the Kokchetav Massif: Are So-Called Diamondiferous Gneisses Magmatic Rocks? Earth Planet. Sci. Lett., 216(3): 347–364

    Article  Google Scholar 

  • Massonne, H. J., Kennedy, A., Nasdala, L., et al., 2007. Dating of Zircon and Monazite from Diamondiferous Quartzofeldspathic Rocks of the Saxonian Erzgebirge—Hints at Burial and Exhumation Velocities. Mineral. Mag., 71: 407–425

    Article  Google Scholar 

  • Massonne, H. J., Tu, W. M., 2007. δ 13C-Signature of Early Graphite and Subsequently Formed Microdiamond from the Saxonian Erzgebirge, Germany. Terra Nova, 19(6): 476–480

    Article  Google Scholar 

  • Mingram, B., Kröener, A., Hegner, E., et al., 2004. Zircon Ages, Geochemistry, and Nd Isotopic Systematics of Pre-Variscan Orthogneisses from the Erzgebirge, Saxony (Germany), and Geodynamic Interpretation. Intern. J. Earth Sci., 93(5): 706–727

    Article  Google Scholar 

  • Mojzsis, S. J., Harrison, T. M., 2000. Vestiges of a Beginning: Clues to the Emergent Biosphere Recorded in the Oldest Known Sedimentary Rocks. GSA Today, 10(4): 1–6

    Google Scholar 

  • Mposkos, E. D., Kostopoulos, D. K., 2001. Diamond, Former Coesite and Supersilicic Garnet in Metasedimentary Rocks from the Greek Rhodope: A New Ultrahigh-Pressure Metamorphic Province Established. Earth Planet. Sci. Lett., 192(4): 497–506

    Article  Google Scholar 

  • Nasdala, L., Massonne, H. J., 2000. Microdiamonds from the Saxonian Erzgebirge, Germany: In Situ Micro-Raman Characterisation. Eur. J. Mineral., 12: 495–498

    Google Scholar 

  • Ogasawara, Y., 2005. Microdiamonds in Ultrahigh-Pressure Metamorphic Rocks. Elements, 1: 91–96

    Article  Google Scholar 

  • Perraki, M., Proyer, A., Mposkos, E., et al., 2006. Raman Micro-Spectroscopy on Diamond, Graphite and Other Carbon Polymorphs from the Ultrahigh-Pressure Metamorphic Kimi Complex of the Rhodope Metamorphic Province, NE Greece. Earth Planet. Sci. Lett., 241(3–4): 672–685

    Article  Google Scholar 

  • Rosing, M. T., 1999. 13C-Depleted Carbon Microparticles in >3 700-Ma Sea-Floor Sedimentary Rocks from West Greenland. Science, 283(5402): 674–676

    Article  Google Scholar 

  • Rozen, O. M., Zorin, Y. M., Zayachkovsky, A. A., 1972. A Find of the Diamonds Linked with Eclogites of the Precambrian Kokchetav Massif. Doklady Acad. Nauk SSSR, 203: 674–676 (in Russian)

    Google Scholar 

  • Sano, Y., Shirai, K., Takahata, N., 2005. Nano-SIMS Analysis of Mg, Sr, Ba and U in Natural Calcium Carbonate. Anal Sci., 21(9): 1091–1097

    Article  Google Scholar 

  • Sano, Y., Takahata, N., Tsutsumi, Y., et al., 2006. Ion Microprobe U-Pb Dating of Monazite with About Five Micrometer Spatial Resolution. Geochem. J., 40(6): 597–608

    Article  Google Scholar 

  • Schmidt, S., Nagel, T. J., Froitzheim, N., 2010. A New Occurrence of Microdiamond-Bearing Metamorphic Rocks, SW Rhodopes, Greece. Eur. J. Miner., 22: 189–198

    Article  Google Scholar 

  • Sobolev, N. V., Shatsky, V. S., 1990. Diamond Inclusions in Garnets from Metamorphic Rocks: A New Environment for Diamond Formation. Nature, 343(6260): 742–746

    Article  Google Scholar 

  • Stöckhert, B., Duyster, J., Trepmann, C., et al., 2001. Microdiamond Daughter Crystals Precipitated from Supercritical COH+Silicate Fluids Included in Garnet, Erzgebirge, Germany. Geology, 29: 391–394

    Article  Google Scholar 

  • Stöckhert, B., Trepmann, C., Massonne, H. J., 2009. Decrepitated UHP Fluid Inclusions: About Diverse Phase Assemblages and Extreme Decompression Rates (Erzgebirge, Germany). J. of Metamorph. Geol., 27: 673–684.

    Article  Google Scholar 

  • van-Roermund, H. L. M., Carswell, D. A., Drury, M. R., et al., 2002. Microdiamonds in a Megacrystic Garnet Websterite Pod from Bardane on the Island of Fjortoft, Western Norway: Evidence for Diamond Formation in Mantle Rocks during Deep Continental Subduction. Geology, 30: 959–962

    Article  Google Scholar 

  • Vrijmoed, J. C., Smith, D. C., van-Roermund, H. L. M., 2008. Raman Confirmation of Microdiamond in the Svartberget Fe-Ti Type Garnet Peridotite, Western Gneiss Region, Western Norway. Terra Nova, 20(4): 295–301

    Article  Google Scholar 

  • Willner, A. P., Sebazungu, E., Gerya, T. V., et al., 2002. Numerical Modelling of PT-Paths Related to Rapid Exhumation of High-Pressure Rocks from the Crustal Root in the Variscan Erzgebirge Dome (Saxony/Germany). J. Geodynam., 33(3): 281–314

    Article  Google Scholar 

  • Xu, S. T., Okay, A. I., Ji, S. Y., et al., 1992. Diamond from the Dabie-Shan Metamorphic Rocks and Its Implication for Tectonic Setting. Science, 256(5053): 80–82

    Article  Google Scholar 

  • Yang, J. S., Xu, Z. Q., Dobrzhinetskaya, L. F., et al., 2003. Discovery of Metamorphic Diamonds in Central China: An Indication of a >4 000 km-Long-Zone of Deep Subduction Resulting from Multiple Continental Collisions. Terra Nova, 15(6): 370–379

    Article  Google Scholar 

  • Yokochi, R., Ohnenstetter, D., Sano, Y., 2008. Intragrain Variation in δ 13C and Nitrogen Concentration Associated with Textural Heterogeneities of Carbonado. Can. Mineral., 46: 1283–1296

    Article  Google Scholar 

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Correspondence to Larissa F. Dobrzhinetskaya.

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This study was supported by Japanese Society for Promotion of Science.

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Dobrzhinetskaya, L.F., Green, H.W., Takahata, N. et al. Crustal signature of δ 13C and nitrogen content in microdiamonds from Erzgebirge, Germany: Ion microprobe studies. J. Earth Sci. 21, 623–634 (2010). https://doi.org/10.1007/s12583-010-0129-6

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  • DOI: https://doi.org/10.1007/s12583-010-0129-6

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