| details |
Late Oligocene |
Early Miocene |
USSR(European) |
Korallova,V.V. Palynological boundary of Oligocene and Miocene deposits of the Southern European part of the USSR. |
1980 |
| original |
Early Sarmatian |
|
Austria |
Klaus,W. A Middle Miocene, (Lower Sarmatian) microflora from the southeastern Border of the Alps. |
1984 |
| details |
Karaganian |
|
USSR(Ukrainian SSR) |
Korallova,V.V. Palynological complex of the Karaganian deposition of the Prichernomorian Depression (Middle Miocene, Ukrainian Ssr) |
1985 |
| details |
Nd |
|
China(E.China) |
Wang,K. et al. Palynological assemblages of crude oil from the oil fields in East China and the research of the oil source. |
1986 |
| details |
Miocene |
|
Massachusetts |
Frederiksen,N.O. Late Cretaceous and Tertiary floras, vegetation and paleoclimates of New England. |
1989 |
| details |
Oligocene |
|
Vermont |
Frederiksen,N.O. Late Cretaceous and Tertiary floras, vegetation and paleoclimates of New England. |
1989 |
| details |
Early Miocene |
Middle Miocene |
California |
Barnett,J. Palynology and paleoecology of the Tertiary Weaverville Formation, Northwestern California, USA. |
1989 |
| details |
Early Oligocene |
Middle Oligocene |
USSR(Siberia) |
Kolykhalov,Y.M. et al. Paleogene and Noegene deposits in the Southwest Chulym-Yenisei Basin. (In: The Cenozoic of Siberia and Northeastern USSR. V.S.Zykina.editor) |
1989 |
| details |
Early Miocene |
|
Austria |
Meller,B. et al. Lower Miocene leaf, palynomorph, and diaspore assemblages from the base of the lignite-bearing sequence in the opencast mine Oberdorf, north Voitsberg (Styria, Austria) as an indication of "Younger Mastixioid" vegetation. |
1999 |
| details |
Paleogene |
|
China(Honan) |
Tao,M. et al. The Paleogene sporopollen assemblages series in China and the discussion about two important stratigraphic boundaries. |
2000 |
| details |
Paleogene |
|
China(Hupei) |
Tao,M. et al. The Paleogene sporopollen assemblages series in China and the discussion about two important stratigraphic boundaries. |
2000 |