Dorog type (Middle Eocene) spore-pollen assemblage in the Socka Beds of Slovenia I.
During our multidisciplinary studies of the problem of the Óligocene and Lower Miocene stratigraphy in Slovenia, we have established the following: 1. The Socka Beds are heterochronous. 2. The type locality is of Middle Eocene age. 3. The tropical coal forming vegetation was reconstructed on the bas...
Elmentve itt :
| Szerzők: | |
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| Dokumentumtípus: | Cikk |
| Megjelent: |
1994
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| Sorozat: | Plant cell biology and development
5 |
| Kulcsszavak: | Palinológia, Paleobotanika - eocén - Szlovákia |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/47798 |
| Tartalmi kivonat: | During our multidisciplinary studies of the problem of the Óligocene and Lower Miocene stratigraphy in Slovenia, we have established the following: 1. The Socka Beds are heterochronous. 2. The type locality is of Middle Eocene age. 3. The tropical coal forming vegetation was reconstructed on the basis of palynological data. 4. The dominance of the pollen grains associated with spores of tropical ferns (Anemia, Lygodium, Gleicheniaceae, etc.) is identical with the Dorog Basin type. This result changes the previous paleophytogeographical concepts on this subject. |
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| Terjedelem/Fizikai jellemzők: | 20-28 |
| ISSN: | 0866-5443 |