Modern low-oxygen marine systems exhibit patterns of molybdenum–uranium covariation
that can be linked to specific attributes and processes of the depositional system, including …

Patterns of uranium–molybdenum covariation in marine sediments have the potential to
provide insights regarding depositional conditions and processes in paleoceanographic …

Redox-sensitive trace metals and their isotopes have emerged as important tools that are
used to reconstruct the redox-evolution of the ocean-atmosphere system. However …

Sedimentary molybdenum (Mo) and uranium (U) abundances, as well as their isotope
systematics, are used to reconstruct the evolution of the oxygenation state of the surface …

The concentration and isotope composition of molybdenum (Mo) in sediments and
sedimentary rocks are widely used proxies for anoxic conditions in the water column of …

Deepwater anoxia developed widely within a series of silled intracratonic basins in North
America during the Middle Devonian to Early Carboniferous, but the hydrographic factors …

The purpose of this research is to characterize the mobilization and immobilization
processes that control the authigenic accumulation of uranium (U), rhenium (Re), and …

Patterns of sedimentary trace-metal variation can provide information not only about benthic
redox conditions, but also about other water-mass properties in ancient marine depositional …

Elevated molybdenum (Mo) contents in organic-rich sediments are indicative of deposition
from an anoxic and sulfide-rich (euxinic) water-column. This can be used for tracing past …

The geochemical behavior of molybdenum (Mo) in the oceans is closely linked to the
presence of sulfide species in anoxic environments, where Fe availability may play a key …