| details |
Early Danian |
|
Tunisia |
Brinkhuis,H. et al. Dinoflagellate cysts, sea level changes and planktonic foraminifers across the Cretaceous-Tertiary boundary at El Haria, northwest Tunisia. |
1988 |
| details |
Late Danian |
|
Tunisia |
Brinkhuis,H. et al. Danian - Selandian dinoflagellate cysts from lower latitudes with special reference to the El Kef section, Northwest Tunisia. |
1994 |
| details |
Middle Oligocene |
Late Oligocene |
W.Germany(N.Rhine) |
Benedek,P.N. Phytoplanktons from the Middle and Upper Oligocene of Tonisberg, (Lower Rhine area). |
1972 |
| details |
Middle Oligocene |
|
W.Germany(N.Rhine) |
Benedek,P.N. Phytoplanktons from the Middle and Upper Oligocene of Tonisberg, (Lower Rhine area). |
1972 |
| details |
Rupelian |
|
W.Germany(N.Rhine) |
Benedek,P.N. et al. Nannoplankton-phytoplankton correlation from the Middle and Upper Oligocene of northwest Germany. |
1974 |
| details |
Maestrichtian |
Early Paleocene |
Canada(Eastern Offshore) |
Barss,M.S. et al. A palynological zonation and correlation of Sixty-Seven wells, |
1979 |
| details |
Maestrichtian |
Early Paleocene |
Canada(Eastern Offshore) |
Barss,M.S. et al. A palynological zonation and correlation of Sixty-Seven wells, |
1979 |
| details |
Paleocene |
|
Antarctica |
Askin,R.A. Campanian to Paleocene palynological succession of Seymour and adjacent Islands, Northeastern Antarctic Peninsula. |
1988 |
| details |
Early Eocene |
|
Antarctica |
Askin,R.A. Palynology of Olistostrome at Cape Wiman, Seymour Island. |
1993 |
| details |
Middle Miocene |
Late Miocene |
Argentina(Buenos Aires) |
Archangelsky,S. Palynostratigraphy of the Continental Shelf. (In: Geologia Y Recursos naturales De La Plataforma Continental Argentina) |
1996 |
| details |
Paleocene |
|
Denmark |
Andersen,S.B. et al. Petrography to age the Brown Turritella-Sandstone, Tertiary drift from Astersoomradet. |
1983 |
| details |
Paleocene |
|
Denmark |
Andersen,S.B. et al. Petrography to age the Brown Turritella-Sandstone, Tertiary drift from Astersoomradet. |
1983 |