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- W2008321337 abstract "Resume L'etude des ostracodes du Neogene de Huelva (Sud-Ouest du Bassin du Gualdalquivir) permet de mettre en evidence l'evolution des environnements dans le golfe forme apres la fermeture du detroit nord-betique. Durant le Tortonien superieur, des Krithe, Parakrithe et Cytherella peuplent un etage epibathyal, agite. Durant le Messinien, la profondeur augmente vers l'Ouest, avec un etage circalittoral externe (100–150 m) autour de La Palma del Condado, et un milieu plus profond (200–250 m), pres de Gibraleon. Au Pliocene, les ostracodes dominants sont frequents a l'etage infralittoral interne, sauf dans la zone de Huelva (circalittoral interne-infralittoral externe)." @default.
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- W2008321337 date "1996-06-01" @default.
- W2008321337 modified "2023-09-27" @default.
- W2008321337 title "Les ostracodes du golfe mio-pliocene du Sud-Ouest de l'espagne" @default.
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- W2008321337 doi "https://doi.org/10.1016/s0035-1598(96)90038-0" @default.
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