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              <p>The Pyrenees are part of the northeastern margin of the Ibero-Armorican Variscan Arc. They possess one of the most completeuppermost Ediacaran–Cambrian successions in West Gondwanawhich has been classically divided into two principal lithostratigraphicunits : the Canaveilles and Jujols Groups. In the southernflank of the Canigou massif (Puigmal Variscan tectonostratigraphicunit), a unique Fabert volcanic level is usually described atthe top of the Cabrils Formation (uppermost Canaveilles Group)which was recently dated around ca. 570 Ma. The overlying TreguràFormation (Jujols Group) is divided into a lower volcanoclasticbreccia member with limestone olistoliths and strong thicknessvariations, and an upper limestone member. The Tregurà Formationhas been considered to encompass the Ediacaran-Cambriantransition, however, until now, no geochronological data have supportedthis hypothesis. The present study has been aimed to providean up-to-date and detailed facies analyzes of the Ediacaran-Cambrian formations from the Pyrenees, and to test previouslypublished dating of above-mentioned volcanic and breccia levelsthrough new LA-ICPMS U–Pb dating of zircons. Therefore, theso-called Fabert volcanic level have been sampled in the FabertVillage and the nearby Pic de la Clape, yielding respective agesat ca.559.5 +1.7/-1.3 Ma and ca.542.9 +5/-1.3 Ma. The Treguràbreccia, sampled at the Pic du Finestrelles and the Pic dela Clape, have respectively yielded maximum depositional agesof ca.556±7Ma and ca.532.9±6.1 Ma.. These new dating arguefor a long-lasting volcanic episode with multiple pulses during theEdiacaran-Cambrian transition. As a consequence, an updatedstratigraphic framework is proposed.</p>
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