Search Results

Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron

by Roberts, A. P., Florindo, F., Villa, G., Chang, L., Jovane, L., Bohaty, S. M., Larrasoaña, J. C., Heslop, D., Fitz Gerald, J. D.
Published in Earth and Planetary Science Letters (2011)

Magnetotactic bacterial response to Antarctic dust supply during the Palaeocene-Eocene thermal maximum

by Larrasoaña, J.C., Roberts, A.P., Chang, L., Schellenberg, S.A., Fitz Gerald, J.D., Norris, R.D., Zachos, J.C.
Published 2012

Low-temperature magnetic properties of pelagic carbonates: Oxidation of biogenic magnetite and identification of magnetosome chains

by Chang, L., Winklhofer, M., Roberts, A. P., Heslop, D., Florindo, F., Dekkers, M. J., Krijgsman, W., Kodama, K., Yamamoto, Y.
Published in Journal of Geophysical Research: Solid Earth (2013)

Low-temperature magnetic properties of pelagic carbonates: Oxidation of biogenic magnetite and identification of magnetosome chains

by Chang, L., Winklhofer, M., Roberts, A.P., Heslop, D., Florindo, F., Dekkers, M.J., Krijgsman, W., Kodama, K., Yamamoto, Y.
Published 2013