Arias, C. (2008). Diversity dynamics of Early Jurassic ostracods of the Cordillera Ibérica (Spain) and the revaluation of the Pliensbachian-Toarcian mass extinction.  Canadian Journal of Earth Science Reviews Sciences, 44 (10) 1397-1411.

 

Arias, C. (2008). Early Jurassic palaeoceanographical reconstruction of the Panthalassa and the Tethys oceans. Gondwana Research, 14 (3) 306-315.     

 

Arias, C. (2009): Extinction pattern of marine Ostracoda across the Pliensbachian-Early Toarcian boundary in the Cordillera Ibérica, NE Spain: causes and consequences. Geobios, 42, 1-15

 

Arias, C. (2009). Pliensbachian ostracods from the Prejano section, Sierra de la Demanda, Cordillera Ibérica .  Neue Jahrbuch für Geologie und Paläontologie, 252(2):181-206        

 

Arias, C., Garcia-Frank, A., Canales, M.L., Ureta, S. (2009). Ostracods from the Global Stratotype Section for the base of the Aalenian Stage, Jurassic, at Fuentelsaz Section (Cordillera Iberica, Spain). Rivista Italiana di Paleontologia e Stratigrafia 115(2):209-232.

 

Arias, C. (2009). Multivariate hierarchical analyses of European Early Jurassic Marine Ostracoda assemblages: paleoecological, and palaeobiogeographical implications. Lethaia , 42, 495-510.                

 

Arias, C. (2009). Seasonal cycle variations on the supercontinent of Pangaea: implications for the Early Jurassic Palaeoceanography of the European Epicontinental Sea. Ocean Circulation and El Niño: New Research, 1-30. NOVA Science Publisher, New York. ISBN 978-1- 6092-084-8                 

 

Comas -Rengifo, M.J. Arias, C., Gómez, J.J., Goy, A., Herrero, C. Osete, M.L., Palencia.  A. (2010).  Complementary Section for the Toarcian (Lower Jurassic) Global Stratotype: the Almonacid de la Cuba Section (Spain). Stratigraphy and Geological Correlation, 18 (2): 133-152.

 

Gómez, J.J., Arias, C. (2010). Rapid warming and mass extinction at the Lower Toarcian (Jurassic) of central Spain. Marine Micropaleontology, 74:119-135

          

Arias, C. (2013). The early Toarcian (early Jurassic) ostracod extinction events in the Iberian Range: the effect of temperature changes and prolonged exposure to low dissolved oxygen concentrations. Palaeogeography, Palaeoclimatology, Palaeoecology 387, 40–55.