| details |
Late Albian |
|
USSR(Primorsk Kray) |
Shugaevskaya,O.V. et al. Upper Mesozoic spore and pollen assemblages of southern Far East and their significance for stratigraphy. |
1974 |
| details |
Early Cretaceous |
|
Oklahoma |
Wingate,F.H. Palynology of the Denton Shale (Lower Cretaceous), of southeastern Oklahoma. |
1974 |
| details |
Early Campanian |
|
Japan(Hokkaido I.) |
Miki,A. Late Cretaceous pollen and spore floras of northern Japan composition and interpretation. |
1977 |
| details |
Santonian |
|
Utah |
Nichols,D.J. Palynostratigraphy in relation to sequence stratigraphy, Straight Cliffs Formation (Upper Cretaceous) Kaiparowits Plateau, Utah |
1995 |
| details |
Late Albian |
|
Wyoming |
Ravn,R.L. Miospores from the Muddy Sandstone, (Upper Albian), Wind River Basin, Wyoming, USA. |
1995 |
| details |
Cretaceous |
|
USSR(Kazakh SSR) |
Medvedeva,A.M. et al. Direct evidence for vertical oil migration in the eastern Precaspian. |
1993 |
| details |
Cretaceous |
|
Nd |
Herngreen,G.F.W. et al. Cretaceous palynofloral Provinces: A review. (Principles and Applications. Applications. J.Jansonius and D.C.McGregor, editors.) |
1996 |
| details |
Late Albian |
|
USSR(Urals) |
Bolkhovitina,N.A. The fossil spores of the ferns of the Family Gleicheniaceae (Taxonomy and distribution). (In: The Importance of Palynological Analysis for the Stratigraphic and Paleofloristic Investigations. M.I. Nejshtadt, editor. Papers for the Second International Palynology Conference., Utrecht,1966) |
1966 |
| details |
Early Cretaceous |
|
Poland |
Waksmundzka,M. Triassic and Lower Cretaceous miospores of the mid-Polish Trough (Central Poland) as a record of stratigraphy, paleoecology, and history of thermal changes. |
2001 |
| details |
Albian |
|
Alaska |
Lyle,M.W. et al. Hydrocarbon reservoir and source-rock characteristics from selected areas of southwestern Alaska. |
1982 |
| details |
Albian |
|
Alaska |
Lyle;W.M. et al. Hydrocarbon reservoir and source-rock characteristics from selected areas of Southwestern Alaska. |
1982 |