Limestone-marl alternations are usually interpreted to reflect cyclic paleoenvironmental fluctuations linked to Milankovitch-scale climate variations. However. the impact of diagenesis on lithological differentiation can be overprinted on the primary signal. In order to evaluate environmental variations during the deposition of the Gargasian hemipelagic limestone-marl alternations fro... https://www.paulynramirez.com/product-category/socks/