Nitellopsis (Tectochara) merianii (Al. Braun ex Unger, 1852) Grambast & Soulié-Märsche, 1972 (Fig. 8 L-N) Chara meriani Unger, 1852: 82, pl. 25, figs 10-12. Tectochara meriani – Grambast & Grambast-Fessard 1954: 668. Nitellopsis (Tectochara) meriani – Grambast & Soulié- Märsche 1972: 11. DISTRIBUTION. — Nitellopsis (Tectochara) merianii appears to be exclusive to Europe during the Upper Eocene (Upper Priabonian) and Lower Oligocene (Rupelian) (Table 5). It has been reported in Rupelian lacustrine deposits from many French localities, i.e. Paris Basin (Grambast & Paul 1965; Riveline 1986), Aquitaine (Feist & Ringeade 1977), the western sector of Languedoc (Grambast 1962; Feist- Castel 1971) and Provence (Touraine 1971) basins. It was also reported in Lower Oligocene beds in the Rhine Graben in Germany (Mädler 1955; Schwarz 1997) and in Lower Oligocene deposits from the Molassic Swiss Basin (Kissling 1974; Reichenbacher et al. 1996). In Spain, this species has been documented in Upper Eocene-Lower Oligocene deposits from the Ebro Basin (Choi 1989; Feist et al. 1994) and from Oligocene rocks in the central Iberian Peninsula (Loranca Basin) by Juliá de Agar (1991). Recently, Sanjuan & Martín-Closas (2012) reported the oldest record of the species in the Upper Priabonian of the eastern Ebro Basin, namely at Torre Casanova (Moià), El Talladell and Vinaixa (Tables 2, 4). During the Uppermost Oligocene-Lower Miocene, this species expanded from western Europe across the Paratethys realm to NE China and SE Asia, ranging from latitude 18°N to 50°N and covering the entire Eurasian landmass (Soulié-Märsche et al. 1997 and references therein; Soulié-Märsche et al. 2002; Sanjuan & Martín-Closas in press). In Eastern Europe, this species was also recorded in Lower Oligocene deposits from Slovenia (Ettinghausen 1872) and Romania (Iva et al. 1970; Baciu & Feist 1999). Mädler & Staesche (1979) reported this species in many localities attributed to Early Oligocene from Turkey (Table 5). DESCRIPTION Large gyrogonites, variable in size, 818-1262 µm high (mean 1084 µm), and 716-1045 µm wide (mean 909 µm), normally ovoid but sometimes ellipsoidal in shape with an isopolarity index of 96-146 (mean 121).Spiral cells 126µm wide, generally convex.Eight to eleven (often nine) convolutions visible in lateral view. Apex nitellopsidoid, slightly convex or subrounded, with well-marked thinning and narrowing of the spiral cells in the periapical zone.Apical nodules present, more or less prominent. Base rounded or slightly conical with large basal pore, 100 µm across, and located within a pentagonal funnel. REMARKS Ŋis species shows a notably reduced size in comparison with coeval Nitellopsis species such as N. (T.) wannacotti, N. (T.) aemula and N. (T.) latispira, which are about 300 µm larger and are in general more rounded in shape., Published as part of Sanjuan, Josep & Martín-Closas, Carles, 2014, Taxonomy and palaeobiogeography of charophytes from the Upper Eocene- Lower Oligocene of the Eastern Ebro Basin (Catalonia, NE Spain), pp. 385-420 in Geodiversitas 36 (3) on page 406, DOI: 10.5252/g2014n3a3, http://zenodo.org/record/4538531, {"references":["UNGER F. 1852. - Iconographia plantarum fossilium. Denkschriften Akademie der Wissenschaften, Mathematisch-Naturwissenchaftliche Klasse, Wien 4: 73 - 118.","GRAMBAST L. & PAUL P. 1965. - Observations nouvelles sur la flore de charophytes du Stampien du bassin de Paris. Bulletin de la Societe Geologique de France 7: 239 - 247.","RIVELINE J. 1986. - Les Charophytes du Paleogene et du Miocene inferieur d'Europe Occidentale. Cahiers de Paleontologie, Centre National de la Recherche Scientifique, 227 p.","FEIST M. & RINGEADE M. 1977. - Etude biostratigraphique et paleobotanique (charophytes) des formations continentales d'Aquitaine, de l'Eocene superieur au Miocene inferieur. Bulletin de la Societe geologique de France 7: 341 - 354.","GRAMBAST L. 1962. - Apercu sur les Charophytes tertiaires du Languedoc et leur signification stratigraphique. Comptes Rendus Sommaires des Seances de la Societe Geologique de France 10: 313 - 314.","FEIST- CASTEL M. 1971. - Sur les Charophytes fossiles du Bassin tertiaire d'Ales (Gard). Geobios 4: 157 - 172.","TOURAINE F. 1971. - L'Oligocene nord-varois. Sa position stratigraphique et sa signification dans la tectogenese subalpine (etat des connaissances actuelles). Annales Guebhard 47: 394 - 421.","MADLER K. 1955. - Zur Taxonomie der Tertiaren Charophyten. Geologisches Jahrbuch 70: 265 - 328.","SCHWARZ J. 1997. - Charophyten aus dem Tertiar des Oberrheingrabens (Mitteleozan-Untermiozan). Palaeontographica Abt. B 243: 1 - 84.","KISSLING D. 1974. - L'Oligocene de l'extremite occidentale du basin molassique Suisse. Stratigraphie et apercu sedimentologique. PhD dissertation Universite de Geneve, 188 p.","REICHENBACHER B., BERGER J. P. & WEIDMANN M. 1996. - Charophytes et otolithes de la Molasse d'eau douce inferieure oligocene de Moutier (Jura Suisse). Abhandlungen Neues Jahrbuch fur Geologie und Palaontologie 202 (1): 63 - 93.","CHOI S. J. 1989. - Les Charophytes du Bassin Potassique Catalan (Nord-Est de l'Espagne) a la limite Eocene-Oligocene. Paleobiologie continentale 26: 1 - 67.","FEIST M., ANADON P., CABRERA L., CHOI S. J., COLOM- BO F. & SAEZ M. 1994. - Upper Eocene-Lowermost Miocene charophyte in the Ebro Basin (Spain). Contribution to the charophyte biozonation in Western Europe. Newsletter Stratigraphy 30: 1 - 32.","JULIA DE AGAR J. J. 1991. - Contribucion al estudio de carofitas fosiles de la Cuenca Terciaria de Loranca (provincia de Cuenca, Espana). Coloquios de Paleontologia, Universidad Complutense de Madrid 43: 57 - 78.","ETTINGHAUSEN C. 1872. - Die fossile Flora von Sagor in Krain. Denkschriften der Kaiserlichen Akademie der Wissenschaften / Mathematisch-Naturwissenschaftliche Classe 32: 159 - 202.","IVA M., MARGARIT M. & MARGARIT G. 1970. - Asupra citorva caracee din stratele de Turbuta de Pe Valea Hirtoapelor (Nord-Vesul Baxinului Transsilvaniei). Studiai si cercetari de Geologie, Geofizica, Geografie, Seria Geologie, Bucuresti 15: 419 - 430.","BACIU C. & FEIST M. 1999. - Les charophytes oligocenes du nord-ouest de la Transylvanie (Roumanie). Acta Palaeontologica Romana 2: 27 - 29.","MADLER K. & STAESCHE U. 1979. - Fossile Charophyten aus dem Kanozoikum (Tertiar und Quartar) der Turkei. Geologisches Jahrbuch B 33: 81 - 157."]}