Karst bauxite formation during Miocene Climatic Optimum
WEBAug 9, 2021 · The Miocene Climatic Optimum (MCO) represents a global warm period (approximately 17– Ma) interrupting a longterm period of Cenozoic cooling. To elucidate if bauxitization took place in southeastern European midlatitude areas during the MCO, we studied a section of undated massive karst bauxite (Crveni Klanac, CK) in .