| original |
Maestrichtian |
Paleocene |
New Mexico |
Anderson,R.Y. Cretaceous - Tertiary palynology, eastern side of the San Juan Basin, New Mexico. |
1960 |
| details |
Paleocene |
|
Canada(Alberta) |
Snead,R.G. Microfloral diagnosis of the Cretaceous-Tertiary boundary, Central Alberta. |
1969 |
| details |
Paleocene |
|
Wyoming |
Guennel,G.K. et al. Palynology of the Hoback Basin |
1973 |
| details |
Early Paleocene |
|
Canada(Saskatchewan) |
Sweet,A.R. Palynology of the Ravenscrag and Frenchman Formation. (In: Coal Resources of Southern Saskatchewan: A model for evaluation methodology. S.H.Whitaker, J.A.Irvine and P.L.Broughton, editors) |
1978 |
| details |
Early Eocene |
Middle Eocene |
Colorado |
Newman,K.R. Palynomorphs of the Green River Formation, (Eocene) Colorado and Utah. Some observations and interpretations. |
1984 |
| details |
Early Eocene |
Middle Eocene |
Utah |
Newman,K.R. Palynomorphs of the Green River Formation, (Eocene) Colorado and Utah. Some observations and interpretations. |
1984 |
| details |
Middle Paleocene |
|
Canada(Alberta) |
Jerzykiewicz,T. et al. Caliche and associated improverished palynology assemblages: An innovative line of paleoclimatic research onto the Uppermost Cretaceous and Paleocene of Southern Alberta |
1986 |
| details |
Paleocene |
|
New Mexico |
Newman,K.R. Biostratigraphic correlation of Cretaceous-Tertiary Boundary Rio Colorado to San Juan Basin, New Mexico. (In: The Cretaceous-Tertiary Boundary in the San Juan and Raton Basins, New Mexico and Colorado. J.E. Fassett and J.K.Rigby, editors) |
1987 |
| details |
Late Paleocene |
|
Canada(Alberta) |
Demchuk,T.D. Palynostratigraphic zonation of Paleocene strata in the Central and South-Central Alberta Plains. |
1990 |
| details |
Early Paleocene |
|
North America |
Nichols,D.J. et al. Palynological evidence of effects of the terminal Cretaceous event on terrestrial floras in Western North America. (In: Extinction events in earth history. IGCP, Proceeding of Project 216. E.G.Kauffman and O.H.Walliser, editors) |
1990 |