Plant microfossils from the Upper Cretaceous and Lower Tertiary layers of Northern Spain I.
The spore-pollen assemblages of two localities of the Upper Cretaceous layers from Northern Spain are presented in this contribution. In the sample of the Zambrana section (30 km South of Miranda de Ebro) the gymnospermous Classoidites glandis occurs in a dominant quantity with a large number of ear...
Elmentve itt :
| Szerző: | |
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| Dokumentumtípus: | Cikk |
| Megjelent: |
1994
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| Sorozat: | Plant cell biology and development
5 |
| Kulcsszavak: | Palinológia, Paleobotanika - felső-krétakor - Spanyolország |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/47799 |
| LEADER | 01917nab a2200217 i 4500 | ||
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| 008 | 170713s1994 hu o 000 eng d | ||
| 022 | |a 0866-5443 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Kedves Miklós | |
| 245 | 1 | 0 | |a Plant microfossils from the Upper Cretaceous and Lower Tertiary layers of Northern Spain I. |h [elektronikus dokumentum] / |c Kedves Miklós |
| 260 | |c 1994 | ||
| 300 | |a 29-41 | ||
| 490 | 0 | |a Plant cell biology and development |v 5 | |
| 520 | 3 | |a The spore-pollen assemblages of two localities of the Upper Cretaceous layers from Northern Spain are presented in this contribution. In the sample of the Zambrana section (30 km South of Miranda de Ebro) the gymnospermous Classoidites glandis occurs in a dominant quantity with a large number of early Brevaxonate pollen grains: Adantopollis and Complexiopollis fspp. This is similar to the spore-pollen assemblage isolated from Oviedo (SOLÉ DE PORTA, 1978) and to those of Fermetelos, Oia, etc. from Portugal (KEDVES and PÁRDUTZ, 1983). As for their geological age, the Lower Turonian seems to be probable. The spore-pollen assemblage of the Sobron section (80 km North-West of Burgos) is quite different. Dominant forms are the disaccate gymnosperm pollen grains. The quantity of the evolved early Brevaxonate pollen grains (Eunormapolles: Papillopollis, Interporopollenites, Verruoculopollis, Endopollis, Krutzschipollis, etc.) and that of thePostnormapolles is relatively large. A similar palynomorph assemblage was described from Guadalix (MÉDUS and ALVAREZ RAMIS, 1989), its geological age is probably Santonian. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Biológiai tudományok | |
| 695 | |a Palinológia, Paleobotanika - felső-krétakor - Spanyolország | ||
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/47799/1/plant_cell_005_029-041.pdf |z Dokumentum-elérés |