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Tanycythere New Genus and its Significance for Jurassic Ostracod Diversity

Published online by Cambridge University Press:  15 October 2015

Maria Cristina Cabral ,
Alan Lord ,
Ian Boomer ,
Isabel Loureiro  and
Heinz Malz
Maria Cristina Cabral
Affiliation:
Universidade de Lisboa, Faculdade de Ciências, Departamento and Centro de Geologia, Campo Grande, C6, 4° piso, 1749-016 Lisboa, Portugal, ;
Alan Lord
Affiliation:
Senckenberg Forschungsinstitut, Senckenberganlage 25, D-60325 Frankfurt-am-Main, Germany,
Ian Boomer
Affiliation:
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, B15 2TT, UK,
Isabel Loureiro
Affiliation:
Universidade de Lisboa, Faculdade de Ciências, Departamento and Centro de Geologia, Campo Grande, C6, 4° piso, 1749-016 Lisboa, Portugal, ;
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Abstract

The new genus Tanycythere (Crustacea, Ostracoda) is described from the Jurassic (Hettangian–Bathonian) of western and central Europe based on T. caudata new species, T. praecaudata praecaudata new subspecies, T. praecaudata parallela new subspecies, T. duartei new species, T. posteroelongata new species, and T. wattonensis new species. Another new species, T. procera, is described from the Lower Cretaceous (?Barremian). Recognition of a new genus comprising six new species and subspecies indicates that overall Jurassic and Early Cretaceous ostracod biodiversity is underestimated.

Type
Research Article
Information
Journal of Paleontology , Volume 88 , Issue 3 , May 2014 , pp. 519 - 530
Copyright
Copyright © The Paleontological Society 

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References

Arias, C. 2006. Northern and Southern Hemispheres ostracod palaeobiogeography during the Early Jurassic: Possible migration routes. Palaeogeography, Palaeoclimatology, Palaeoecology, 233:63–95.CrossRefGoogle Scholar
Baird, W. 1850. The Natural History of the British Entomostraca. Ray Society, London, p. viii+1–364.Google Scholar
Bown, P. R., Lees, J. A., and Young, J. R. 2004. Calcareous nannoplankton evolution and diversity through time, p. 481–508. In Thierstein, H. R. and Young, J. R. (eds.), Coccolithophores—From Molecular Processes to Global Impact. Springer.Google Scholar
Boomer, I. D. 1991. Lower Jurassic ostracod biozonation of the Mochras Borehole. Journal of Micropalaeontology, 9:205–218.Google Scholar
Brand, E. 1990. Biostratigraphische Untergliederung des Ober-Bathonium im Raum Hildesheim, Nordwest-deutschland mittels Ostracoden und Korrelation ihrer Vertikalreichweiten mit Ammoniten-Zonen. Geologisches Jahrbuch, A, 121:119–273.Google Scholar
Comas-Rengifo, M. J., Duarte, L. V., Goy, A., Paredes, R., and Silva, R. L. 2013. El Sinemuriense superior (Cronozonas Oxynotum y Raricostatum) en la región de S. Pedro de Moel (Cuenca Lusitánica, Portugal), p. 15–19. In Duarte, L. V., Silva, R. L., and Azerêdo, A. C. (eds.), Fácies carbonatadas ricas em matéria orgânica do Jurássico da Bacia Lusitânica. Novos contributos paleontológicos, sedimentológicos e geoquímicos. Comunicações Geológicas, 100, volume especial I.Google Scholar
Copestake, P. and Johnson, B. 2014. Lower Jurassic Foraminifera from the Llanbedr (Mochras Farm) Borehole, North Wales, U.K. Monograph of the Palaeontographical Society 641, Vol. 167.Google Scholar
Drexler, E. 1958. Foraminiferen und Ostracoden aus dem Lias α von Siebeldingen/Pfalz. Geologisches Jahrbuch, 75:475–554.Google Scholar
Duarte, L. V., Krautter, M., and Soares, A. F. 2001. Bioconstructions à spongiaires siliceux dans le Lias terminal du Bassin lusitanien (Portugal): Stratigraphie, sédimentologie et signification paléogéographique. Bulletin Société Géologique de France, 172:637–646.CrossRefGoogle Scholar
Duarte, L. V., Silva, R. L., Oliveira, L. C. V., Comas-Rengifo, M. J., and Silva, F. 2010. Organic-rich facies in the Sinemurian and Pliensbachian of the Lusitanian Basin, Portugal: Total organic carbon and relation to transgressive-regressive facies cycles. Geologica Acta, 8:325–340.Google Scholar
Duarte, L. V. and Soares, A. F. 2002. Litostratigrafia das séries margo-calcárias do Jurássico inferior da Bacia Lusitânica (Portugal). Comunicações do Instituto Geológico e Mineiro, 89:135–154.Google Scholar
Duarte, L. V., Silva, R. L., Mendonça Filho, J. G, Poças Ribeiro, N., and Chagas, R. B. A. 2012. High-resolution stratigraphy, palynofacies and source rock potential of the Água de Madeiros Formation (upper Sinemurian) of the Lusitanian Basin, Portugal. Journal of Petroleum Geology, 35:105–126.Google Scholar
Dunhill, A. M., Benton, M. J., Twitchett, R. J., and Newell, A. J. 2012. Completeness of the fossil record and the validity of sampling proxies at outcrop level. Palaeontology, 55:1155–1175.Google Scholar
Gründel, J. 1967. Zur Grossgliederung der Ordnung Podocopida G. W. Müller, 1894 (Ostracoda). Neues Jahrbuch für Geologie und Paläontologie, Monatshefte, 1967:321–332.Google Scholar
Gründel, J. and Kozur, H. 1971. Zur taxonomie der Bythocytheridae und Tricornidae (Podocopida, Ostracoda). Monatsberichte der Deutschen Akademie der Wissenschaften zu Berlin, 13 (10–12):907–937.Google Scholar
Kozur, H. 1972. Die Bedeutung triassischer Ostracoden für stratigraphische und paläoökologische Untersuchungen. Mitteilungen der Gesellschaft für Geologie und Bergbaustudien, 21:623–660.Google Scholar
Kozur, H. 1985. Neue ostracoden-arten aus dem Oberen Mittelkarbon (Höheres Moskovian), Mittel- und Oberperm des Bükk-Gebirges (N-Ungarn). Geologisch-Paläontologische Mitteilungen Insbruck, special volume, 2:1–145.Google Scholar
Latreille, P. A. 1806.Genera crustaceorum et insectorum, secundum ordinem naturalem et familias disposita. Amand Koenig, Paris, xviii+302 p.Google Scholar
Lord, A. R. 1974. Ostracods from the Domerian and Toarcian of England. Palaeontology, 17:599–622.Google Scholar
Michelsen, O. 1975. Lower Jurassic biostratigraphy and ostracods of the Danish Embayment. Danmarks Geologiske Undersøgelse, II, 104:1–287.CrossRefGoogle Scholar
Oertli, H. J. 1959. Les ostracodes du Bathonien du Boulonnais 1. les micro-ostracodes. Revue de Micropaléontologie, 3:115–126.Google Scholar
Paredes, R., Comas-Rengifo, M. J., Duarte, L. V., and Goy, A. 2013. Braquiópodes do Sinemuriano superior da região de S. Pedro de Moel e de Peniche (Bacia Lusitânica, Portugal), p. 29–35. In Duarte, L. V., Silva, R. L., and Azerêdo, A. C. (eds.), Fácies carbonatadas ricas em matéria orgânica do Jurássico da Bacia Lusitânica. Novos contributos paleontológicos, sedimentológicos e geoquímicos. Comunicações Geológicas, 100, volume especial I.Google Scholar
Roth, R. 1928. Monoceratina, a new genus of Ostracoda from the Pennsylvanian of Oklahoma. Journal of Paleontology, 2:15–19.Google Scholar
Sars, G. O. 1866 . Oversigt af Norges marine Ostracoder. Forhandlinger i Videnskabs-Selskabet i Christiania, 1865:1–130.Google Scholar
Sars, G. O. 1922–1928. An account of the Crustacea of Noway, 9. Ostracoda. Bergen Museum, xii+1–277 p.Google Scholar
Schmidt-Kaler, H. 1985. Der Lias in neuen Kernbohrungen unter der südöstlichen Frankenalb. Geologisches Jahrbuch, A84:5–11.Google Scholar
Schornikov, E. I. 1990. Evolution and classification of Bythocytheridae. Courier Forschungs-Institut Senckenberg, 123:291–302.Google Scholar
Silva, R. L., Duarte, L. V., Comas-Rengifo, M. J., Mendonça Filho, J. G., and Azerêdo, A. C. 2011. Update of the carbon and oxygen isotopic records of the early-late Pliensbachian: Insights from the organic-rich hemipelagic series of the Lusitanian Basin (Portugal). Chemical Geology, 283:177–184.CrossRefGoogle Scholar
Whittaker, J. E. and Hart, M. B. (eds.). 2009. Ostracods in British Stratigraphy. The Micropalaeontological Society, Special Publications. The Geological Society, London, viii+485 p.Google Scholar