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 ORCID: https://orcid.org/0000-0001-7211-8049 and Franz, S. O. ;
Contact
Ralf.Tiedemann [ at ] awi.de

Abstract


Item Type
Article
Authors
Tiedemann, Ralf ORCID: https://orcid.org/0000-0001-7211-8049 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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