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.

Tiedemann, Ralf; Franz, S. O.

hdl:10013/epic.28402

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.

Tiedemann, Ralf

and Franz, S. O. ;

Contact

Ralf.Tiedemann [ at ] awi.de

Abstract

Item Type

Article

Authors

Tiedemann, Ralf

and Franz, S. O. ;

Divisions

AWI Organizations > Geosciences > Marine Geology and Paleontology

Programs

Basic Research > Helmholtz Independent Research

Publication Status

Published

Eprint ID

17842

Cite as

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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