Deep water circulation, chemistry and terrigenous sediment supply in the Equatorial Atlantic during the Pliocene, 2.6 - 3.3 Ma and 4.5 - 5 Ma. In Curry, W.B., Shackleton, N.J., and Richter, C.


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Ralf.Tiedemann [ at ] awi.de

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Tiedemann, R. and Franz, S. O. (1997): Deep water circulation, chemistry and terrigenous sediment supply in the Equatorial Atlantic during the Pliocene, 2.6 - 3.3 Ma and 4.5 - 5 Ma. In Curry, W.B., Shackleton, N.J., and Richter, C. , Proceedings Ocean Drilling Program Scientific Results, 154 , pp. 299-318 .


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