with 9 figures and 7 tables Abstraet. A charophyte succession has been established in nineteen sections and eight isolated outcrops from the Ebro Basin, ranging from the Priabonian ro the Aquitanian. Most assemblages were recovered fmm continuous sections and their abundance and diversity allow to define a new zonal scheme for the Upper Eocene-Lower Miocene of Europe. The new zonation includes nine subdivisions, based on the distribution of thirty-two species and directly correlated with the mammal standard levels. Changes in diversity, occurring mainly in the Middle and Upper Oligocene, have been related to climatíc variations. A new species, Chara sp. A. is also described and figured. Résumé. Une biozonatÍon basée sur les charophytes esr ...
In this paper the micromammals from three localities in the Oligocene/Miocene boundary interval and ...
Se describen las asociaciones fósiles del Eoceno medio y superior (Bartoniense y Priaboniense) de la...
A diverse Eocene charophyte flora from a section at G ant (V ertes Hills), Transdanubian Central Ran...
A charophyte succession has been established in nineteen sections and eight isolated outcrops from t...
A charophyte biozonation of the Paleogene (Thanetian-Chattian) sequences of the Eastern Ebro Basin (...
Sanjuan, Josep, Martín-Closas, Carles (2014): Taxonomy and palaeobiogeography of charophytes from th...
FIG. 8. — Charophytes from the Artés and lateral south-western Formations, Ebro Basin: A-C, Lychnoth...
FIG. 9. — Charophytes from Sant Boi, Artés and lateral south-western Formations, Ebro Basin: A-C, Ha...
The occurrence of Ramys cf. perezi in the Miocene sequences of the Central Ebro Basin allows to loca...
An analysis is given of the floral distribution in the Upper Eocene and Oligocene of the South of Fr...
The onset of endorheic sedimentation in the Ebro Basin is a prominent feature of the basin's evoluti...
charophytes were recorded in two different stratigraphic units from the non-marine Palaeogene of the...
The Grande Coupure represents a major terrestrial faunal turnover recorded in Eurasia associated wit...
Fossil charophytes were recorded in two different stratigraphic units from the non- marine Palaeogen...
A charophyte biozonation of the Paleogene (Thanetian-Chattian) sequences of the Eastern Ebro Basin (...
In this paper the micromammals from three localities in the Oligocene/Miocene boundary interval and ...
Se describen las asociaciones fósiles del Eoceno medio y superior (Bartoniense y Priaboniense) de la...
A diverse Eocene charophyte flora from a section at G ant (V ertes Hills), Transdanubian Central Ran...
A charophyte succession has been established in nineteen sections and eight isolated outcrops from t...
A charophyte biozonation of the Paleogene (Thanetian-Chattian) sequences of the Eastern Ebro Basin (...
Sanjuan, Josep, Martín-Closas, Carles (2014): Taxonomy and palaeobiogeography of charophytes from th...
FIG. 8. — Charophytes from the Artés and lateral south-western Formations, Ebro Basin: A-C, Lychnoth...
FIG. 9. — Charophytes from Sant Boi, Artés and lateral south-western Formations, Ebro Basin: A-C, Ha...
The occurrence of Ramys cf. perezi in the Miocene sequences of the Central Ebro Basin allows to loca...
An analysis is given of the floral distribution in the Upper Eocene and Oligocene of the South of Fr...
The onset of endorheic sedimentation in the Ebro Basin is a prominent feature of the basin's evoluti...
charophytes were recorded in two different stratigraphic units from the non-marine Palaeogene of the...
The Grande Coupure represents a major terrestrial faunal turnover recorded in Eurasia associated wit...
Fossil charophytes were recorded in two different stratigraphic units from the non- marine Palaeogen...
A charophyte biozonation of the Paleogene (Thanetian-Chattian) sequences of the Eastern Ebro Basin (...
In this paper the micromammals from three localities in the Oligocene/Miocene boundary interval and ...
Se describen las asociaciones fósiles del Eoceno medio y superior (Bartoniense y Priaboniense) de la...
A diverse Eocene charophyte flora from a section at G ant (V ertes Hills), Transdanubian Central Ran...