A change from warm/humid to cold/dry climate conditions recorded in lower Barremian clay-dominated continental successions from the SE Iberian Chain (NE Spain)
Elisa Laita, Blanca Bauluz, Marcos Aurell, Beatriz Bádenas, José Ignacio Canudo, Alfonso Yuste
Topics & Concepts
MarlGeologyClay mineralsKaoliniteIlliteSedimentary rockGeochemistryMineralogyFaciesMicritePaleontologyStructural basinGeochemistry and Elemental AnalysisClay minerals and soil interactionsPaleontology and Stratigraphy of Fossils