Ján Schlögl

Orbital forcing in Lower Jurassic rhythmically bedded basinal carbonates: implications for depositional environment, benthic life, and stratigraphy

Abstract The Sinemurian to Pliensbachian limestone–marlstone succession exposed in the Tatra Mountains (Western Carpathians) forms part of a widespread, rhythmically bedded hemipelagic carbonate facies that developed along the north-western Tethyan margin. Such deposits are typic...