JOURNAL AND BOOK CITATIONS

Birke, T.K., and Fuller, M., submitted. Shipboard paleomagnetic age estimate for an acoustic basement emplacement and later remagnetization in Marion Plateau, ODP Leg 194, NE Australia. Phys. Earth Planet. Inter.

Delius, H., submitted. Relating log signatures to lithologies in Miocene cool subtropical carbonates, Marion platforms (offshore NE Australia). Geochem., Geophys., Geosyst.

Ehrenberg, S.N., 2005. Porosity and permeability in Miocene carbonate platforms of the Marion Plateau, offshore NE Australia: relationships to stratigraphy, facies and dolomitization. In Braithwaite, C.J.R., Rizzi. G., and Darke, G. (Eds.), The Geometry and Petrogenesis of Dolomite Hydrocarbon Reservoirs, Spec. Publ.—Geol. Soc. London, 235:233–253.

Fuller, M., Molina-Garza, R., Touchard, Y., and Kidane, T., submitted. ODP legs in the Southern Ocean and Marion Plateau: paleomagnetic records from carbonates. Phys. Earth Planet. Inter.

Isern, A.R., Anselmetti, F.S., and Blum, P., 2001. Ocean drilling contrains carbonate platform formation and Miocene sea level on the Australian margin. Eos, Trans. Am. Geophys. Union, 83(41):469.

Isern, A.R., Anselmetti, F.S., and Blum, P. 2004. A Neogene carbonate platform, slope and shelf edifice shaped by sea level and ocean currents, Marion Plateau (Northeast Australia). In Eberli, G.P., Masaferro, J.L., and Sarg, J.F. (Eds.), Seismic Imaging of Carbonate Reservoirs and Systems. AAPG Mem., 81:291–307.

Isern, A.R., Anselmetti, F.S., Blum, P., and the Leg 194 Scientific Party, 2001. ODP Leg 194: sea level magnitudes recorded by continental margin sequences on the Marion Plateau, northeast Australia. JOIDES J., 27(2):7–11.

John, C.M., Adatte, T., and Mutti, M., 2006. Regional trends in clay mineral fluxes to the Queensland margin and ties to middle Miocene global cooling. Palaeogeogr., Palaeoclimatol., Palaeoecol.. 233(3–4):2040–224. doi:10.1016/j.palaeo.2005.09.010

John, C.M., Karner, G.D., and Mutti, M., 2004. ¹⁸O and Marion Plateau backstripping: combining two approaches to constrain late middle Miocene eustatic amplitude. Geology, 32:829–832. doi:10.1130/G20580.1

John, C.M., and Mutti, M., 2005. Relative control of paleoceanography, climate, and eustasy over heterozoan carbonates: a perspective from slope sediments of the Marion Plateau (ODP Leg 194). J. Sediment. Res., 75:216–230. doi:10.2110/jsr.2005.017

Kindler, P., Ruchonnet, C., and White, T., 2006. The Southern Marion Platform (Marion Plateau, NE Australia) during the early Pliocene: a lowstanding-producing, temperate-water carbonate factory. In Pedley, H.M., and Carannante, G. (Eds.), Cool-Water Carbonates: Depositional Systems and Palaeoenvironmental Control. Spec. Publ.—Geol. Soc. London, 255:271–284.

Mutti, M., John, C.M., and Knoerich, A.C., 2006. Chemostratigraphy in Miocene heterozoan carbonate settings: applications, limitations and perspectives. In Pedley, H.M., and Carannante, G. (Eds.), Cool-Water Carbonates: Depositional Systems and Palaeoenvironmental Controls. Spec. Publ.—Geol. Soc. London, 255:307–322.

Meyer, N., 2005. Changements climatiques et Océanographique au Pléistocène supérieur: les données du Plateau du Marion, NE Australie [M.S. thesis]. Univ. Geneva, Switzerland.

Obrochta, S.P., Hine, A.C., Flower, B., Hallock, P.H., and Brooks, G.R., 2003. Quantification of the changing sedimentary architecture of a continental margin sediment drift as a result of the mid-Pleistocene climate transition. Eos, Trans. Am. Geophys. Union, 84(6):PP51C-0937. (Abstract)

Obrochta, S.P., 2004. Australian Great Barrier Reef initiation constrained by seaward, shallow-water sediment drift architecture: are Pleistocene reefs contemporaneous (ODP Leg 194, Marion Plateau) [M.S. thesis]. Univ. South Florida, Tampa.

Sheps, K., 2004. Quantitative paleoenvironmental analysis of carbonate platform sediments on the Marion Plateau (NE Australia, ODP Leg 194) [M.S. thesis]. Univ. South Florida, Tampa. http://etd.fcla.edu/SF/SFE0000546/kshepsthesis.pdf