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Licensed Unlicensed Requires Authentication Published by De Gruyter January 23, 2020

Extraterrestrial, shock-formed, cage-like nanostructured carbonaceous materials

  • Péter Németh EMAIL logo and Laurence A.J. Garvie
From the journal American Mineralogist

Abstract

Shock caused by impacts can convert carbonaceous material to diamond. During this transition, new materials can form that depend on the structure of the starting carbonaceous materials and the shock conditions. Here we report the discovery of cage-like nanostructured carbonaceous materials, including carbon nano-onions and bucky-diamonds, formed through extraterrestrial impacts in the Gujba (CBa) meteorite. The nano-onions are fullerene-type materials and range from 5 to 20 nm; the majority shows a graphitic core-shell structure, and some are characterized by fully curved, onion-like graphitic shells. The core is either filled with carbonaceous material or empty. We show the first, natural, 4 nm sized bucky-diamond, which is a type of carbon nano-onion consisting of multilayer graphitic shells surrounding a diamond core. We propose that the nano-onions formed during shock metamorphism, either the shock or the release wave, of the pre-existing primitive carbonaceous material that included nanodiamonds, poorly ordered graphitic material, and amorphous carbonaceous nanospheres. Bucky-diamonds could have formed either through the high-pressure transformation of nano-onions, or as an intermediate material in the high-temperature transformation of nanodiamond to nano-onion. Impact processing of planetary materials was and is a common process in our solar system, and by extension, throughout extrasolar planetary bodies. Together with our previous discovery of interstratified graphite-diamond in Gujba, our new findings extend the range of nano-structured carbonaceous materials formed in nature. Shock-formed nano-onions and bucky-diamonds are fullerene-type structures, and as such they could contribute to the astronomical 217.5 nm absorption feature.



Acknowledgments and Funding

We are grateful to the staff and for use of the facilities in the John M. Cowley Center for High Resolution Electron Microscopy at Arizona State University. P.N. acknowledges financial support from the Hungarian National Research, Development and Innovation Office project NKFIH_KH126502 and the János Bolyai Research Scholarship; L.A.J.G. was supported by a NASA Emerging Worlds grant NNX17AE56G. We thank the three reviewers for their comments.

References cited

Asphaug, E., Jutzi, M., and Movshovitz, N. (2011) Chondrule formation during planetesimal accretion. Earth and Planetary Science Letters, 308, 369–379.10.1016/j.epsl.2011.06.007Search in Google Scholar

Barnard, A.S., Russo, S.P., and Snook, I.K. (2003) Coexistence of bucky diamond with nanodiamond and fullerene carbon phases. Physical Review B, 68, 073406.10.1103/PhysRevB.68.073406Search in Google Scholar

Bernatowicz, T.J., Cowsik, R., Gibbons, P.C., Lodders, K., Fegley, B., Amari, S., and Lewis, R.S. (1996) Constraints on stellar grain formation from presolar graphite in the Murchison Meteorite. The Astrophysical Journal, 472, 760–782.10.1086/178105Search in Google Scholar

Blank, V.D., Denisov, V.N., Kirichenko, A.N., Kulnitskiy, B.A., Martushov, S.Y., Mavrin, B.N., and Perezhogin, I.A. (2007) High pressure transformation of single-crystal graphite to form molecular carbon–onions. Nanotechnology, 18, 345601.10.1088/0957-4484/18/34/345601Search in Google Scholar

Blank, V.D., Churkin, V.D., Kulnitsky, B.A., Perezhogin, I.A., Kirichenko, A.N., Erohin, S.V., Sorokin, P.B., and Popov, M.Y. (2018) Pressure-induced transformation of graphite and diamond to onions. Crystals, 8(2), 68.10.3390/cryst8020068Search in Google Scholar

Bouvier, A., and Wadhwa, M. (2010) The age of the Solar System redefined by the oldest Pb-Pb age of a meteoritic inclusion. Nature Geosciences, 3, 637–641.10.1038/ngeo941Search in Google Scholar

Bradley, J., Dai, Z.R., Erni, R., Browning, N., Graham, G., Weber, P., Smith, J., Hutcheon, I., Ishii, H., Bajt, S., Floss, C., Stadermann, F., and Standford, S. (2005) An astronomical 2175 Å feature in interplanetary dust particles. Science, 307, 244–247.10.1126/science.1106717Search in Google Scholar PubMed

Chao, E.T.C., Fahey, J.J., Littler, J., and Milton, D.J. (1962) Stishovite, SiO2 a very high pressure new mineral from Meteor Crater, Arizona. Journal of Geophysical Research, 67, 419–421.10.1029/JZ067i001p00419Search in Google Scholar

Chen, M., Sharp, T.G., El Goresy, A., Wopenka, B., and Xie, X. (1996) The majorite-pyrope + magnesiowüstite assemblage: Constraints on the history of shock veins in chondrites. Science, 271, 1570–1573.10.1126/science.271.5255.1570Search in Google Scholar

Chhowalla, M., Wang, H., Sano, N., Teo, K.B.K., Lee, S.B., and Amaratunga, G.A.J. (2003) Carbon Onions: Carriers of the 217.5 nm Interstellar Absorption Feature. Physical Review Letters, 90, 155504.10.1103/PhysRevLett.90.155504Search in Google Scholar PubMed

Choucair, M., and Stride, J.A. (2012) The gram-scale synthesis of carbon onions. Carbon, 50, 1109–1115.10.1016/j.carbon.2011.10.023Search in Google Scholar

Connelly, J.N., Bollard, J., and Bizzarro, M. (2017) Pb-Pb chronometry and the early Solar System. Geochimica et Cosmochimica Acta, 201, 345–363.10.1016/j.gca.2016.10.044Search in Google Scholar

Daulton, T.L., Eisenhour, D.D., Bernatowicz, T.J., Lewis, R.S., and Buseck, P.R. (1996) Genesis of presolar diamonds: comparative high-resolution transmission electron microscopy study of meteoritic and terrestrial nano-diamonds. Geochimica et Cosmochimica Acta, 60, 4853–4872.10.1016/S0016-7037(96)00223-2Search in Google Scholar

DeCarli, P.S., and Jamieson, J.C. (1961) Formation of diamond by explosive shock. Science, 133, 1821–1822.10.1126/science.133.3467.1821Search in Google Scholar PubMed

El Goresy, A., Dera, P., Sharp, T., Prewitt, C.T., Chen, M., Dubrovinsky, L., Wopenka, B., Boctor, N.Z., and Hemley, R.J. (2008) Seifertite, a dense orthorhombic polymorph of silica from the Martian meteorites Shergotty and Zagami. European Journal of Mineralogy, 20, 523–528.10.1127/0935-1221/2008/0020-1812Search in Google Scholar

Erskine, D.J., and Nellis, W.J. (1991) Shock-induced martensitic phase-transformation of oriented graphite to diamond. Nature, 349, 317–319.10.1038/349317a0Search in Google Scholar

Garvie, L.A.J. (2005) Extraterrestrial carbon nanospheres. Carbon, 44, 158–160.10.1016/j.carbon.2005.08.028Search in Google Scholar

Garvie, L.A.J. (2006) Surface electronic states of meteoritic nanodiamonds. Meteoritics and Planetary Science, 41, 667–672.10.1111/j.1945-5100.2006.tb00982.xSearch in Google Scholar

Garvie, L.A.J., and Buseck, P.R. (2004) Nanosized carbon-rich grains in carbonaceous chondrite meteorites. Earth and Planetary Science Letters, 224, 431–439.10.1016/j.epsl.2004.05.024Search in Google Scholar

Garvie, L.A.J., and Buseck, P.R. (2006) Carbonaceous materials in the acid residue from the Orgueil carbonaceous chondrite meteorite. Meteoritics and Planetary Science, 41, 633–642.10.1111/j.1945-5100.2006.tb00486.xSearch in Google Scholar

Garvie, L.A.J., Németh, P., and Buseck, P.R. (2011) Diamond, bucky-diamond, graphite-diamond, Al-silicate and stishovite in the Gujba CB chondrite. Meteoritics and Planetary Science, 46, A75.Search in Google Scholar

Garvie, L.A.J., Németh, P., and Buseck, P.R. (2014) Transformation of graphite to diamond via a topotactic mechanism. American Mineralogist, 99, 531–538.10.2138/am.2014.4658Search in Google Scholar

Garvie, L.A.J., Knauth, L.P., and Morris, M.A. (2017) Sedimentary laminations in the Isheyevo (CH/CBb) carbonaceous chondrite formed by gentle impact-plume sweep-up. Icarus, 292, 36–47.10.1016/j.icarus.2017.03.021Search in Google Scholar

Huss, G.R., and Lewis, R.S. (1995) Presolar diamond, SiC, and graphite in primitive chondrites: abundances as a function of meteorite class and petrologic type. Geochimica et Cosmochimica Acta, 59, 115–160.10.1016/0016-7037(94)00376-WSearch in Google Scholar

Kis, V.K., Shumilova, T., and Masaitis, V. (2016) HRTEM study of Popigai impact diamond: heterogeneous diamond nanostructures in native amorphous carbon matrix. Physics and Chemistry of Minerals, 43, 661–670.10.1007/s00269-016-0825-6Search in Google Scholar

Krot, A.N., Amelin, Y., Cassen, P., and Meibom, A. (2005) Young chondrules in CB chondrites from a giant impact in the early Solar System. Nature, 436, 989–992.10.1038/nature03830Search in Google Scholar

Krot, A.N., Yurimoto, H., McKeegan, K., Leshin, L., Chaussidon, M., Libourel, G., Yoshitake, M., Huss, G., Guan, Y., and Zanda, B. (2006) Oxygen isotopic compositions of chondrules: Implications for evolution of oxygen isotopic reservoirs in the inner solar nebula. Chemie der Erde—Geochemistry, 66(4), 249–276.10.1016/j.chemer.2006.07.002Search in Google Scholar

Kuznetsov, V.L., Chuvilin, A.L., Butenko, Y.V., Mal’kov, I.Y., and Titov, V.M. (1994a) Onion-like carbon from ultra-disperse diamond. Chemical Physics Letters, 222, 343–348.10.1016/0009-2614(94)87072-1Search in Google Scholar

Kuznetsov, V.L., Chuvilin, A.L., Moroz, E.M., Kolomiichuk, V.N., Shaikhudtdinov, S.K., Butenko, Y.V., and Mal’kov, I.Y. (1994b) Effect of explosion conditions on the structure of detonation soots: Ultradisperse diamond and onion carbon. Carbon, 32, 873–882.10.1016/0008-6223(94)90044-2Search in Google Scholar

Le Guillou, C., Rouzaud, J.N., Remusat, L., Jambon, A., and Bourot-Denise, M. (2010) Structures, origin and evolution of various carbon phases in the ureilite Northwest Africa 4742 compared with laboratory-shocked graphite. Geochimica et Cosmochimica Acta, 74, 4167–4185.10.1016/j.gca.2010.03.038Search in Google Scholar

Marty, B., Kelley, S., and Turner, G. (2010) Chronology and shock history of the Bencubbin meteorite: a nitrogen, noble gas, and Ar-Ar investigation of silicates, metal and fluid inclusions. Geochimica et Cosmochimica Acta, 74, 6636–6665.10.1016/j.gca.2010.05.035Search in Google Scholar

Morris, M.A., Garvie, L.A.J., and Knauth, L.P. (2015) New insight into the Solar System’s transition disk phase provided by the metal-rich carbonaceous chondrite Isheyevo. The Astrophysical Journal Letters, 801, L22.10.1088/2041-8205/801/2/L22Search in Google Scholar

Murri, M., Smith, R.L., McColl, K., Hart, M., Alvaro, M., Jones, A.P., Németh, P., Salzmann, C.H., Corá, F., Domeneghetti, M.C., and others. (2019) Quantifying hexagonal stacking in diamond. Scientific Reports, 9, 10334.10.1038/s41598-019-46556-3Search in Google Scholar

Nakamura-Messenger, K., Messenger, S., Keller, L.P., Clemett, S.J., and Zolensky, M.E. (2006) Organic globules in the Tagish Lake meteorite: remnants of the protosolar disk. Science, 314, 1439–1442.10.1126/science.1132175Search in Google Scholar

Naraoka, H., Mita, H., Komiya, M., Yoneda, S., Kojima, H., and Shimoyama, A. (2004) A chemical sequence of macromolecular organic matter in the CM chondrites. Meteoritics and Planetary Science, 39, 401–406.10.1111/j.1945-5100.2004.tb00101.xSearch in Google Scholar

Németh, P., Garvie, L.A.J., Aoki, T., Dubrovinskaia, N., Dubrovinsky, L., and Buseck, P.R. (2014) Lonsdaleite is faulted and twinned cubic diamond and does not exist as a discrete material. Nature Communications, 5, 6447.10.1038/ncomms6447Search in Google Scholar

Németh, P., Garvie, L.A.J., and Buseck, P.R. (2015) Twinning of cubic diamond explains reported nanodiamond polymorphs. Scientific Reports, 5, 18381.10.1038/srep18381Search in Google Scholar

Ohfuji, H., Irifune, T., Litasov, K.D., Yamashita, T., Isobe, F., Afanasiev, V.P., and Pokhilenk, N.P. (2015) Natural occurrence of pure nano-polycrystalline diamond from impact crater. Scientific Reports, 5, 14702.10.1038/srep14702Search in Google Scholar

Qin, L-C., and Iijima, S. (1996) Onion-like graphitic particles produced from diamond. Chemical Physics Letters, 262(3-4), 252–258.10.1016/0009-2614(96)01037-8Search in Google Scholar

Pearson, V.K., Sephton, M.A., Franchi, I.A., Gibson, J.M., and Gilmour, I. (2006) Carbon and nitrogen in carbonaceous chondrites: Elemental abundances and stable isotopic compositions. Meteoritics and Planetary Science, 41, 1899–1918.10.1111/j.1945-5100.2006.tb00459.xSearch in Google Scholar

Raty, J-Y., Galli, G., Bostedt, C., van Buuren, T.W., and Terminello, L.J. (2003) Quantum confinement and fullerenelike surface reconstructions in nanodiamonds. Physical Review Letters, 90, 037401.10.1103/PhysRevLett.90.037401Search in Google Scholar PubMed

Rubin, A.E., Kallemeyn, G.W., Wasson, J.T., Clayton, R.N., Mayeda, T.K., Grady, M., Verchovsky, A.B., Eugster, O., and Lorenzetti, S. (2003) Formation of metal and silicate globules in Gujba: A new Bencubbin-like meteorite fall. Geochimica et Cosmochimica Acta, 67, 3283–3298.10.1016/S0016-7037(03)00098-XSearch in Google Scholar

Sano, N., Wang, H., Chhowalla, M., Alexandrou, I., and Amaratunga, G.A.J. (2001) Synthesis of carbon ‘onions’ in water. Nature, 414, 506.10.1038/35107141Search in Google Scholar

Sharp, T.G., and DeCarli, P.S. (2006) Shock effects in meteorites. In D.S. Lauretta and H.Y. McSween, Eds., Meteorites and the Early Solar System II, p. 653–678. The University of Arizona Press.10.2307/j.ctv1v7zdmm.37Search in Google Scholar

Sharp, T.G., Lingemann, C.M., Dupas, C., and Stöffler, D. (1997) Natural occurrence of MgSiO3-ilmenite and evidence for MgSiO3-perovskite in a shocked L chondrite. Science, 277, 352–355.10.1126/science.277.5324.352Search in Google Scholar

Sharp, T.G., El Goresy, A., Wopenka, B., and Chen, M. (1999) A post-stishovite SiO2 polymorph in the meteorite Shergotty: implications for impact events. Science, 284, 1511–1513.10.1126/science.284.5419.1511Search in Google Scholar

Shumilova, T., Kis, V.K., Masaitis, V., Sergey, I., and Boris, M. (2014) Onion-like carbon in impact diamonds from the Popigai astrobleme. European Journal of Mineralogy, 26, 267–277.10.1127/0935-1221/2014/0026-2363Search in Google Scholar

Smith, P.P., and Buseck, P.R. (1981) Graphitic carbon in the Allende meteorite: a microstructural study. Science, 212, 322–324.10.1126/science.11536554Search in Google Scholar

Stecher, T.P. (1965) Interstellar Extinction in the Ultraviolet. Astrophysical Journal, 142, 1683–1684.10.1086/180400Search in Google Scholar

Steele, A., McCubbin, F.M., Fries, M.D., Golden, D.C. Ming, D.W., and Benning, L.G. (2012) Graphite in the martian meteorite Allan Hills 84001. American Mineralogist, 97, 1256–1259.10.2138/am.2012.4148Search in Google Scholar

Terrones, H., and Terrones, M. (1997) The transformation of polyhedral particles into graphitic onions. Journal of Physics and Chemistry of Solids, 58, 1789–1796.10.1016/S0022-3697(97)00067-XSearch in Google Scholar

Ugarte, D. (1992) Curling and closure of graphitic networks under electron-beam irradiation. Nature, 359, 707–709.10.1038/359707a0Search in Google Scholar

Weisberg, M.K., and Kimura, M. (2004) Petrology and Raman spectroscopy of shock phases in the Gujba CB chondrite and the shock history of the CB parent body. Lunar and Planetary Science Conference, XXXV, Abstract 1599.Search in Google Scholar

Weisberg, M.K., and Kimura, M. (2010) Petrology and Raman spectroscopy of high pressure phases in the Gujba CB chondrite and the shock history of the CB parent body. Meteoritics and Planetary Sciences, 45, 873–884.10.1111/j.1945-5100.2010.01058.xSearch in Google Scholar

Weisberg, M.K., Kimura, M., Suzuki, A., Ohtani, E., and Sugiura, N. (2006) Discovery of coesite and significance of high pressure phases in the Gujba CB chondrite. Lunar and Planetary Science Conference, XXXVII, Abstract 1788.Search in Google Scholar

Wright, E.L. (1988) The ultraviolet extinction from interstellar graphitic onions. Nature, 336, 227–228.10.1038/336227a0Search in Google Scholar

Xiao, J., Ouyang, G., Liu, P., Wang, C.X., and Yang, G.W. (2014) Reversible nanodiamond-carbon onion phase transformations. Nano Letters, 14, 3645–3652.10.1021/nl5014234Search in Google Scholar

Yamada, K., and Tanabe, Y. (2002) Shock-induced phase transition of oriented pyrolytic graphite to diamond at pressures up to 15 GPa. Carbon, 40, 261–269.10.1016/S0008-6223(01)00086-0Search in Google Scholar

Received: 2019-09-27
Accepted: 2019-10-09
Published Online: 2020-01-23
Published in Print: 2020-02-25

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