The interactions between clay minerals and organic matter, specifically adsorption, are
widely recognized as a crucial mechanism for promoting the preservation of organic matter …

Oceanic anoxic events (OAEs) record profound changes in the climatic and
paleoceanographic state of the planet and represent major disturbances in the global …

The black shale submember of core shales of Pennsylvanian Kansas-type cyclothems is
highly enriched in redox-sensitive trace elements (TEs) relative to the overlying gray shale …

Marine Shales: Depositional Mechanisms and Environments of Ancient Deposits ADS
Classic is now deprecated. It will be completely retired in October 2019. This page will …

Early Cretaceous life and the environment were strongly influenced by the accelerated
break up of Pangaea, which was associated with the formation of a multitude of rift basins …

Organic carbon-rich sediments are enriched in several redox-sensitive and stable sulfide-
forming trace metals (TM) and form an important sink in global TM cycles. In today's ocean …

Mid‐Cretaceous (Barremian‐Turonian) plankton preserved in deep‐sea marl, organic‐rich
shale, and pelagic carbonate hold an important record of how the marine biosphere …

Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

Carbon stable-isotope variation through the Cenomanian–Santonian stages is
characterized using data for 1769 bulk pelagic carbonate samples collected from seven …

Twenty-five years ago, Mesozoic oceanic anoxic events (OAEs) were documented and
formalised as intervals of widespread to global deposition of organic matter. The Toarcian …