Resumen de La Caliza de Peña Redonda (Westfaliense A-B):: Evolución tecto-sedimentaria (Cuenca Carbonífera Central asturiana).

Carlos Ignacio Salvador González

• The occurrence of destructive carbonatic facies at the top of a tectonically controlled megasequence and his probable widespread distribution may be an indicator of an extensive emersion during Westfalian A-B boundary, and could hide important changes in the local fossil distribution