Abad de los Santos, ManuelClemente Pérez, María JoséGonzález-Regalado Montero, María LuzRuiz Muñoz, FranciscoRodríguez Vidal, JoaquínCáceres Puro, Luis MiguelIzquierdo, TatianaPérez Quintero, Juan CarlosTosquella Angrill, JosepPozo Rodríguez, ManuelGómez Gutiérrez, PaulaToscano Grande, AntonioRomero Aguilar, VerónicaArroyo Serrano, Marta2023-02-222023-02-222022Abad, M., Clemente, M. J., González-Regalado, M. L., Ruiz, F., Rodríguez Vidal, J., Cáceres, L. M., Izquierdo, T., Pérez Quintero, J. C., Tosquella, J., Pozo, M., Gómez, P., Toscano, A., Romero, V., Arroyo, M., & Gómez, G. (2022). Faunal evidence of the 1755 Lisbon Tsunami in Gibraltar (S Iberian Peninsula). In Geobios (Vols. 72–73, pp. 1–11). Elsevier BV. https://doi.org/10.1016/j.geobios.2022.07.0030016-6995https://hdl.handle.net/10272/21670This paper analyzes the first systematic faunal record of the 1755 Lisbon tsunami in the Mediterranean. On the basis of sedimentological and paleontological features, the sedimentary record of a core collected in Gibraltar was divided into six sedimentary facies, with a paleoenvironmental evolution from a shallow marine paleoenviroment to an increasingly restricted lagoon. This record includes a bioclastic layer deposited by the 1755 Lisbon tsunami and characterized by an erosive base, presence of basal rip-up clasts and abundant shell debris composed by marine and brackish molluscs. The paleoenvironmental reconstruction derived from the foraminiferal analysis is congruent with that inferred from the sedimentary and the macrofaunal reconstructions, with the introduction of brackish species into the innermost, intertidal areas of a confined lagoon. This paleontological record is the first faunal evidence of the 1755 Lisbon tsunami in the Mediterranean.spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Sedimentary faciesMacrofaunaForaminifera1755 Lisbon TsunamiGibraltarS Iberian Peninsulajournal article10.1016/j.geobios.2022.07.003open access2416 Paleontología