Revision of Late Tithonian charophytes from Lisbon and Sintra-Cascais (Portugal): taxonomy, biostratigraphy and palaeobiogeographical significance

The re-evaluation of the charophyte content of ‘Purbeckian’ sediments from several sections around Lisbon (Olelas and Brouco) and Sintra-Cascais (Murches, Atrozela and Malveira-Guincho) revealed new palaeofloral associations from the Late Tithonian of the South Lusitanian Basin (Portugal). These sections contain Globator rectispirale, G. aff. nurrensis, Nodosoclavator bradleyi, Clavator reidi, Clypeator cf. discordis, Porochara maxima, and newly described occurrences of P. jaccardi, Mesochara harrisi and nodosoclavatoroide utricles. These revised data reinforce the evidence for assigning most of the studied deposits to a Late Tithonian age, instead of the formerly accepted wider interval Tithonian to Early Berriasian (‘Purbeckian’). Population analysis and statistics were applied in order to better assess population variation of the different species. The results of this study are relevant as they contribute to improve the biostratigraphical definition of the ‘Purbeckian’ formations of Portugal and allow more accurate palaeobiogeographical interpretations within the central Tethyan domain, by comparison of the identified charophyte assemblages with documented Jurassic–Cretaceous transition charophytes from other regions.

[1]  J. Rey Le Crétacé inférieur de la marge atlantique portugaise: biostratigraphie, organisation séquentièlle, évolution paléogéographique , 2008 .

[2]  R. Pereira,et al.  New charophytes from the Upper Jurassic of the Lusitanian Basin (Portugal) , 2003, Journal of Micropalaeontology.

[3]  M. Schudack The charophytes of the Lower Saxony Basin (Upper Jurassic-Berriasian): Local zonation, supraregional correlation and paleoecology , 1996 .

[4]  M. Schudack,et al.  European Mesozoic-Cenozoic charophyte biozonation , 1996 .

[5]  Michael E. Schudack Zur Nomenklatur der Gattungen Porochara Mädler 1955 (syn. Musacchiella Feist & Grambast-Fessard 1984) undFeistiella n. gen. (Charophyta) , 1986 .

[6]  L. Grambast PHYLOGENY OF THE CHAROPHYTA , 1974 .

[7]  P. Donze Les couches de passage du Jurassique au Crétacé dans le Jura français et sur les pourtours de la "fosse vocontienne" (Massifs subalpins septentrionaux, Ardèche, Grands-Causses, Provence, Alpes-Maritimes) , 1956 .

[8]  R. E. Peck Morrison Charophyta from Wyoming , 1937 .

[9]  J. Groves,et al.  Preliminary Report on the Purbeck Characeae , 1916 .

[10]  R. Pereira,et al.  Charophytes from the lower Aptian of Rio de Mouro (Lisbon region, Portugal), with the description of a new genus , 2005 .

[11]  C. Martín‐Closas Els caròfits del Juràssic superior i el Cretaci inferior de la Península Ibèrica: = Upper Jurassic and lower Cretaceous charophytes from the Iberian Peninsula , 2000 .

[12]  M. Schudack Some charophytes from the middle dinosaur member of the Tendaguru formation (Upper Jurassic of Tanzania) , 1999 .

[13]  R. D. Lake,et al.  Charophyte biostratigraphy of the Purbeck and Wealden of southern England , 1995 .

[14]  I. Soulié-Märsche,et al.  Fiabilité des données morphométriquesen micropaleontologie: Exemple des Charophytes , 1991 .

[15]  P. Gemayel,et al.  Étude de la variationpopulationnelle d'une charophyte de l'Éocène Pyrénéen par analyses multidimensionnelles , 1991 .

[16]  Richard N. Hiscott,et al.  The Lusitanian Basin of West-Central Portugal: Mesozoic and Tertiary Tectonic, Stratigraphic, and Subsidence History: Chapter 22: European-African Margins , 1989 .

[17]  P. Mojon,et al.  Microfaciès, sédimentologie et micropaléontologie du Purbeckien de Bienne (Jura suisse occidental) , 1987 .

[18]  R. E. Peck North American Mesozoic Charophyta , 1957 .

[19]  P. Donze Nouvelles especes de charophytes dans les niveaux de la limite jurassico-cretacee du Jura, des Alpes-Maritimes et de la Provence , 1955 .

[20]  P. C. Sylvester-Bradley,et al.  British Purbeck Charophyta , 1939 .

[21]  O. Heer Die Urwelt der Schweiz , 1879 .