FIG. 8. — Charophytes from the Artés and lateral south-western Formations, Ebro Basin: A-C, Lychnothamnus grambastii (Feist-Castel, 1971), Torre Casanova section; A, apical view, no. 80100 MGSCB, sample TC-9; B, lateral view, no. 80101 MGSCB, sample TC-9; C, basal view, no. 80102 MGSCB, sample TC-9; D-F, Lychnothamnus vectensis (Groves, 1926), Santpedor and Rubió sections; D, apical view, no. 80103 MGSCB, sample RB-3; E, oblicuous view, no. 80104 MGSCB, sample SP-18; F, lateral view, no. 80104 MGSCB, sample SP-18; G, basal view, no. 80105 MGSCB, sample SP-4; H-K, Lychnothamnus major (Grambast & Paul, 1965), Sarral section and El Talladell outcrop; H, apex, no. 80106 MGSCB, sample BO-1; I, lateral view, no. 80107 MGSCB, sample BO-1; J, later...
Dix-huit espèces de charophyte sont documentées dans les faciès transitionnels et terrestres de l’Éo...
FIG. 7. — Joania peyrerensis n. sp., Upper Oligocene: A-C, ventral and dorsal views of complete spec...
charophytes were recorded in two different stratigraphic units from the non-marine Palaeogene of the...
FIG. 9. — Charophytes from Sant Boi, Artés and lateral south-western Formations, Ebro Basin: A-C, Ha...
Sanjuan, Josep, Martín-Closas, Carles (2014): Taxonomy and palaeobiogeography of charophytes from th...
with 9 figures and 7 tables Abstraet. A charophyte succession has been established in nineteen secti...
FIG. 7. — Charophytes from the lacustrine deposits of Zahle, sample Zahle 2: A-H, Nitellopsis (T.) m...
The onset of endorheic sedimentation in the Ebro Basin is a prominent feature of the basin's evoluti...
A charophyte succession has been established in nineteen sections and eight isolated outcrops from t...
FIG. 8. — Biometric values of Nitellopsis (T.) merianii (Al. Braun ex Unger, 1852) Grambast & Soulié...
Iberia was first an island and then a European peninsula during most of the Earth’s history. This al...
A charophyte biozonation of the Paleogene (Thanetian-Chattian) sequences of the Eastern Ebro Basin (...
The lower part of the upper Irbzer Formation in the Middle Atlas Mountains of Morocco has yielded a ...
A diverse charophyte assemblage from the Middle Miocene of the Vallès‒Penedès and Vilanova basins (C...
FIG. 5. — Distribution of Asbeckiasporites Von der Brelie, 1964 (*), Elaterosporites klaszii (Jardin...
Dix-huit espèces de charophyte sont documentées dans les faciès transitionnels et terrestres de l’Éo...
FIG. 7. — Joania peyrerensis n. sp., Upper Oligocene: A-C, ventral and dorsal views of complete spec...
charophytes were recorded in two different stratigraphic units from the non-marine Palaeogene of the...
FIG. 9. — Charophytes from Sant Boi, Artés and lateral south-western Formations, Ebro Basin: A-C, Ha...
Sanjuan, Josep, Martín-Closas, Carles (2014): Taxonomy and palaeobiogeography of charophytes from th...
with 9 figures and 7 tables Abstraet. A charophyte succession has been established in nineteen secti...
FIG. 7. — Charophytes from the lacustrine deposits of Zahle, sample Zahle 2: A-H, Nitellopsis (T.) m...
The onset of endorheic sedimentation in the Ebro Basin is a prominent feature of the basin's evoluti...
A charophyte succession has been established in nineteen sections and eight isolated outcrops from t...
FIG. 8. — Biometric values of Nitellopsis (T.) merianii (Al. Braun ex Unger, 1852) Grambast & Soulié...
Iberia was first an island and then a European peninsula during most of the Earth’s history. This al...
A charophyte biozonation of the Paleogene (Thanetian-Chattian) sequences of the Eastern Ebro Basin (...
The lower part of the upper Irbzer Formation in the Middle Atlas Mountains of Morocco has yielded a ...
A diverse charophyte assemblage from the Middle Miocene of the Vallès‒Penedès and Vilanova basins (C...
FIG. 5. — Distribution of Asbeckiasporites Von der Brelie, 1964 (*), Elaterosporites klaszii (Jardin...
Dix-huit espèces de charophyte sont documentées dans les faciès transitionnels et terrestres de l’Éo...
FIG. 7. — Joania peyrerensis n. sp., Upper Oligocene: A-C, ventral and dorsal views of complete spec...
charophytes were recorded in two different stratigraphic units from the non-marine Palaeogene of the...