Foraminiferal fauna recovered after the Late Permian extinctions in Iberia and the westernmost Tethys area

The mass extinction at the end of the Permian has long been recognized as the greatest in the history of life. Foraminifers were common throughout the Permian–Triassic (P–T) interval and provide one of the best, and certainly the most informative, fossil records of the P–T crisis. This study addresses the recovery of foraminiferal faunas during the Triassic after the Late Permian extinction in the western Tethys, and particularly in Iberia, through the analysis of evolution rates both at the species and genus level. For the Tethys area in general, a rapid recovery of these faunas during the Olenekian is reflected by high rates of appearance of new taxa along with the reappearance of many “Lazarus” taxa. These taxa became stabilized throughout the Anisian and Ladinian, with a reduction in the rates of origination of new taxa and the presence of associations that were highly diversified, comprising large numbers of species. rst foraminifers in the Triassic of Iberia can be observed at two different levels. The first of these is in the Upper Anisian, while the second level corresponds to the Upper Ladinian (Longobardian)–Lower Carnian. The Triassic associations of the basins of Iberia show paleobiogeographic characteristics that are generally “Tethyan”, most of these associations being well known for the “alpine” Triassic. For the Ladinian, some associations from NE Iberia (NE Iberian basin, Catalonian basin, and Pyrenean basin) also show “Germanic” affinities. Finally, also for the Ladinian, there is some evidence of the possible southward movement of faunas from the Sephardic domain to the Betic basin. This point, however, requires further investigation. he exception of faunas associated with the reefs of the Ladinian Catalonian basin, communities are usually of low diversity and typical of unstable, shallow marine facies.