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Pleistocene variability of the Subtropical Convergence at East Tasman Plateau: Evidence from planktonic foraminiferal Mg/Ca (ODP Site 1172A).

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Nürnberg, D. and Groeneveld, J. (2006): Pleistocene variability of the Subtropical Convergence at East Tasman Plateau: Evidence from planktonic foraminiferal Mg/Ca (ODP Site 1172A). , Geochemistry, Geophysics, Geosystems, 7, Q04P11. . doi: 10.1029/2005GC000984
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