Article ID Journal Published Year Pages File Type
9463100 Palaeogeography, Palaeoclimatology, Palaeoecology 2005 15 Pages PDF
Abstract
Similar involutinid foraminiferal assemblages occur in the upper Muschelkalk of the Iberian Ranges and Catalan Coastal Ranges, as well as in the upper part of the transgressive systems track of the UAA-2.2 third-order cycle identified in the Muschelkalk of the Pyrenees Basin. Thus, this foraminiferal assemblage can be considered as an extensive bioevent marker related to an important transgressive stage of Ladinian age.
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Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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A foraminiferal assemblage as a bioevent marker of the main Ladinian transgressive stage in the Betic Cordillera, southern Spain
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