details |
Kimmeridgian |
Valanginian |
Australia(Queensland) |
Burger,D. Stratigraphy, palynology and palaeoenvironments of the Hooray Sandstone, Eastern Eromanga Basin, Queensland and New South Wales. |
1989 |
details |
Kimmeridgian |
Valanginian |
Australia(NSW) |
Burger,D. Stratigraphy, palynology and palaeoenvironments of the Hooray Sandstone, Eastern Eromanga Basin, Queensland and New South Wales. |
1989 |
details |
Berriasian |
Valanginian |
China(Kirin) |
Chen,P.-D. Distribution and migration of the Jehol fauna with reference to the non-marine Jurassic-Cretaceous boundary in China. (In: Jurassic - Cretaceous Boundary. V.V.Menner, editor) |
1990 |
details |
Berriasian |
Valanginian |
Chile |
Drinnan,A.N. et al. Cretaceous paleobotany and its bearing on the biogeography of Austral angiosperms. (In: Its Role in the Reconstruction of Gondwanaland. T.N. Taylor and E.L. Taylor, editors) |
1990 |
details |
Berriasian |
Valanginian |
England(Dorset) |
Allen,P. et al. Correlation of northwest European Purbeck-Wealden, (nonmarine Lower Cretaceous), as seen from the English type areas |
1991 |
details |
Berriasian |
Valanginian |
China(Heilungkiang) |
Zhao,C. et al. Jurassic and Cretaceous boundary palynology in northeast China. |
2000 |
details |
Oxfordian |
Volgian |
USSR(Yakut ASSR) |
Petrova,L.D. Palynological characteristics of Upper Jurassic deposits of the Vilyusk Syncline. (In: Stratigraphy and Correlation of Sediments Using Palynology Methods. Materials IV All-Union Palynological Conference. G.N.Papulov, editor) |
1983 |
details |
Early Toarcian |
Volgian |
USSR(Siberia) |
Ilyina,V.I. Subdivision and correlation of Jurassic deposits in Central and eastern Siberia, on the basis of palynological data |
1981 |
details |
Midway |
Wilcox |
Texas |
Elsik,W.C. Palynology of the Wilcox Group. |
1968 |
details |
Thanetian |
Ypresian |
Georgia |
Frederiksen,N.O. Lower Tertiary sporomorph biostratigraphy |
1980 |
details |
Thanetian |
Ypresian |
Alabama |
Frederiksen,N.O. Lower Tertiary sporomorph biostratigraphy |
1980 |