时间:2018年02月24日 14:44来源: 点击数:







2000.9-2004.6  北京大学 | 固体地球物理学 | 大学本科毕业 | 学士学位

2004.9-2005.8  中科院研究生院 | 固体地球物理学 | 硕士研究生

2005.9-2009.5  英国南安普顿大学 | 固体地球物理学 | 研究生(博士)毕业 | 博士学位




2009.05--2011.08 英国国家海洋中心 博士后

2010.01--2010.04 日本高知大学先进海洋钻孔研究中心 特邀研究人员

2011.09--2013.09 荷兰乌特勒支大学地球科学学院 研究人员

2013.10--2015.09 澳大利亚国立大学地球科学3522com B级研究员

2015.09--至今 北京大学地球与空间科学学院 研究员




[1]Chang, L., D. Heslop, A.P. Roberts, D. Rey, and K. J. Mohamed, Discrimination of biogenic and detrital magnetite through a double Verwey transition temperature, J. Geophys. Res. Solid Earth, 121, 3-14, doi: 10.1002/2015JB012485, 2016.

[2]Zhao, G.Y., Y. Han, X.M. Liu, L. Chang et al, Can the magnetic susceptibility record of Chinese Red Clay sequence be used for paleomonsoon reconstructions? Geophysical Journal International, 204, 1421-1429, doi: 10.1093/gji/ggv510, 2016.

[3]avian, J. F., Jovane, L., Giorgioni, M., Iacoviello, F., Rodelli, D., Roberts, A. P., L. Chang, F. Florindo, and M. Sprovieri, Environmental magnetic implications of magnetofossil occurrence during the Middle Eocene Climatic Optimum (MECO) in pelagic sediments from the equatorial Indian Ocean, Palaeogeography, Palaeoclimatology, Palaeoecology, 441, 212-222, 2016.

[4]Liu, S., C. Deng, J. Xiao, J. Li, G.A. Paterson, L. Chang, L. Yi, H. Qin, Y. Pan, and R. Zhu, Insolation driven biomagnetic response to the holocene warm period in semi-arid East Asia, Scientific Report, 5, 8001, doi:10.1038/srep08001, 2015.

[5]Sier, M.J., J. Peeters, M.J. Dekkers, J.M. Parés, L. Chang, F.S. Busschers, K.M. Cohen, J. Wallinga, F.P.M. Bunnik, and W. Roebroeks, The Blake Event recorded near the Eemian type locality – A diachronic onset of the Eemian in Europe, Quaternary Geochronology, 28, 12-28, 2015.

[6]Sant, K., A. de Leeuw, L. Chang, G. Czapowski, A. G?siewicz and W. Krijgsman, Paleomagnetic analyses on Badenian–Sarmatian drill cores from the North Carpathian foredeep (Middle Miocene, Poland), Biuletyn Panstwowego Instytutu Geologiznego, 461, 179-192, 2015.

[7]Chang, L., A.P. Roberts, M. Winklhofer, D. Heslop, M.J. Dekkers, W. Krijgsman, and P. Smith, Magnetic detection and characterization of biogenic magnetic minerals: A comparison of ferromagnetic resonance and first-order reversal curve diagrams, Journal of Geophysical Research – Solid Earth, 119, 6136-6158, 2014.

[8]Chang, L., I. Vasiliev, C.G.C. van Baak, W. Krijgsman, M.J. Dekkers, A.P. Roberts, A. van Hoesel and M. Winklhofer, Identification and environmental interpretation of diagenetic and biogenic greigite in sediments: A lesson from the Messinian Black Sea, Geochemistry, Geophysics, Geosystems, 15, 3612-3627, 2014.

[9]Winklhofer, M., L. Chang and S. Eder, On the magnetocrystalline anisotropy of greigite (Fe3S4), Geochemistry, Geophysics, Geosystems, 15, 1558-1579, 2014.

[10]Heslop, D., A.P. Roberts and L. Chang, Recognition of biogenic components from first-order reversal curve signatures, Geochemistry, Geophysics, Geosystems, 15, 2170-2179, 2014.

[11]Li, G., B. Zhang, F. Yu, A.A. Novakova, M.S. Krivenkov, T.Y. Kiseleva, L. Chang, J. Rao, A.O. Polyakov, G.R. Blake, R.A. de Groot and T.T.M. Palstra, High purity Fe3S4 greigite microcrystals for magnetic and electro-chemical performance, Chemistry of Materials, 26, 5821-5829, 2014.

[12]Chang, L., M. Winklhofer, A.P. Roberts, D. Heslop, F. Florindo, M. J. Dekkers, W. Krijgsman, K. Kodama & Y. Yamamoto, Low-temperature magnetic properties of pelagic carbonates: oxidation of biogenic magnetite and identification of magnetosome chains, Journal of Geophysical Research – Solid Earth, 118, 6049-6065, 2013.

[13]Bolton, C.T., L. Chang, S.C. Clemens, K. Kodama, M. Ikehara, M. Medina-Elizalde, G.A. Paterson, A.P. Roberts, E.J. Rohling, Y. Yamamoto and X. Zhao, A 500,000 year record of Indian summer monsoon dynamics recorded by equatorial Indian Ocean upper water-column structure, Quaternary Science Reviews, 77, 167-180, 2013.

[14]Roberts, A.P., F. Florindo, L. Chang, D. Heslop, L. Jovane and J.C. Larrasoa?a, Magnetic properties of pelagic marine carbonates, Earth-Science Reviews, 127, 111-139, 2013.

[15]Heslop, D., A.P. Roberts, L. Chang, M. Davies, A. Abrajevitch and P. De Deckker, Quantifying magnetite magnetofossil contributions to sedimentary magnetizations, Earth and Planetary Science Letters, 382, 58-65, 2013.

[16]Muxworthy, A.R., W. Williams, A.P. Roberts, M. Winklhofer, L. Chang and M. Pósfai, Critical single domain grain sizes in chains of interacting greigite particles: implications for magnetosome crystals, Geochemistry, Geophysics, Geosystems, 14: 5430-5441, 2013.

[17]Zhao G., X. Liu, Q. Chen, B. Lü, L. Chang, H. Niu, P. Li, H. Guo, and Z. Liu, A long-term increasing aridification and cooling trend at the Chinese Loess Plateau during the Pliocene, Quaternary International, 306, 121-128, 2013.

[18]Reichenbacher, B., W. Krijgsman, Y. Lataster, M. Pippèrr, C.G.C. van Baak, L. Chang, D. K?lin, J. Jost, G. Doppler, D. Jung, J. Prieto, H. Abdul Aziz, M. B?hme, J. Garnish, U. Kirscher, V. Bachtadse, A new magnetostratigraphic framework for the Lower Miocene (Burdigalian/Ottnangian, Karpatian) in the North Alpine Foreland Basin, Swiss J. Geoscience, 106, 309-334, 2013.

[19]Chang, L., A.P. Roberts, W. Williams, J.D. Fitz Gerald, J.C. Larrasoa?a, L. Jovane, and A.R. Muxworthy, Giant magnetofossils and hyperthermal events, Earth and Planetary Science Letters, 351-352, 258-269, 2012.

[20]Chang, L., M. Winklhofer, A.P. Roberts, M.J. Dekkers, C-S. Horng, L. Hu, and Q. Chen, Ferromagnetic resonance characterization of greigite (Fe3S4), monoclinic pyrrhotite (Fe7S8) and non-interacting titanomagnetite (Fe3-xTixO4), Geochemistry Geophysics Geosystems, 13, Q05Z41, 2012.

[21]Chang L., R.A.D. Pattrick, G. van der Laan, V.S. Coker, and A.P. Roberts, Enigmatic X-ray magnetic circular dichroism in greigite, The Canadian Mineralogist, 50, 429-436, 2012.

[22]Roberts, A.P., L. Chang, D. Heslop, F. Florindo, and J.C. Larrasoa?a, Searching for single domain magnetite in the ‘pseudo-single-domain’ sedimentary haystack: Implications of biogenic magnetite preservation for sediment magnetism and relative paleointensity determinations, Journal of Geophysical Research, 117, B08104, 2012.

[23]Deng, J., L. Chang, P. Wang, E. Zhang, J. Ma and T. Wang, Preparation and magnetic properties of CoWO4 nanocrystals, Crystal Research and Technology, doi: 10.1002/crat.201200130, 2012.

[24]Larrasoa?a, J.C, A.P. Roberts, L. Chang, J.D. Fitz Gerald, S.A. Schellenberg, R.D. Norris, and J.C. Zachos, Magnetotactic bacterial response to Antarctic dust supply during the Palaeocene-Eocene thermal maximum, Earth and Planetary Science Letters, 333-334, 122-133, 2012.

[25]Ma, J., W. Guo, X. Duan, T. Wang, W. Zheng and L. Chang, Growth of flower-like CdSe dendrites from a Br?nsted acid–base ionic liquid precursor, RSC Advances, 2, 5944-5946, 2012.

[26]Roberts, A.P., L. Chang, C.J. Rowan, C-S Horng and F. Florindo, Magnetic properties of sedimentary greigite (Fe3S4): An update, Review of Geophysics, 49, RG1002, 46 PP., 2011.

[27]Roberts, A.P., F. Florindo, G. Villa, L. Chang, L. Jovane, S.M. Bohaty, J.C. Larrasoa?a, D. Heslop, and J.D. Fitz Gerald, Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron, Earth and Planetary Science Letters, 310, 441-452, 2011.

[28]Muxworthy, A.R. X. Ji, V. Ridley, Y. Pan, L. Chang, L. Wang, and A.P. Roberts, Multi-protocol palaeointensity determination from middle Brunhes Chron volcanics, Datong Volcanic Province, China, Physics of the Earth and Planetary Interiors, 187, 188-198, 2011.

[29]Ma, J., L. Chang, J. Lian, Z. Huang, X. Duan, X. Liu, P. Peng, T. Kim, Z. Liu and W. Zheng, Ionic liquid-modulated synthesis of ferrimagnetic Fe3S4 hierarchical superstructures, Chemical Communications, 46, 5006–5008, 2010.

[30]Chang, L., B.D. Rainford, J.R. Stewart, C. Ritter, A.P. Roberts, Y. Tang, and Q. Chen, Magnetic structure of greigite (Fe3S4) probed by neutron powder diffraction and polarized neutron diffraction, Journal of Geophysical Research, 114, B07101, 2009.

[31]Chang, L., A.P. Roberts, C.J. Rowan, Y. Tang, P. Pruner, Q. Chen and C-S. Horng, Low-temperature magnetic properties of greigite (Fe3S4),Geochemistry Geophysics Geosystems, 10, Q01Y04, 2009.

[32]Chang, L., A.P. Roberts, Y. Tang, B.D. Rainford, A.R. Muxworthy, and Q. Chen, Fundamental magnetic parameters from pure synthetic greigite (Fe3S4), Journal of Geophysical Research, 113, B06104, 2008.

[33]Chang, L., A.P. Roberts, A.R. Muxworthy, et al., Magnetic characteristics of synthetic pseudo-single-domain and multi-domain greigite,Geophysical Research Letters, 34, L24304, 2007.

[34]Roberts, A.P., Q. Liu, C.J. Rowan, L. Chang, C. Carvallo, J. Torrent, and C-S. Horng, Characterization of hematite (α-Fe2O3), goethite (α-FeOOH), greigite (Fe3S4), and pyrrhotite (Fe7S8) using first-order reversal curve diagrams, Journal of Geophysical Research – Solid Earth, 111, B12S35, 2006.

[35]Deng, C. L., Q. Wei, R. Zhu, H. Wang, R. Zhang, H. Ao, L. Chang, and Y. Pan, Magnetostratigraphic age of the Xiantai Paleolithic site in the Nihewan Basin and implications for early human colonization of Northeast Asia, Earth and Planetary Science Letters, 244, 336-348, 2006.



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