Molybdenum is an essential trace element for human, animal and plant health and has
played an important part in the evolution of life on earth. Nonetheless, exposure to the …

Thermochemical sulfate reduction (TSR) is a set of redox reactions between organic matter
and sulfates at temperatures> 120° C, and occurs in varied environments including deeply …

Transient appearances of oxygen have been inferred before the Great Oxygenation Event
(GOE)[∼ 2.3 billion years (Ga) ago] based on redox-sensitive elements such as Mo and S …

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 …

The observed difference in molybdenum (Mo) mobility and isotopic fractionation under oxic
versus euxinic (ie, anoxic and sulfidic) aqueous conditions provides a sound operational …

Pyrite is the most common authigenic mineral preserved in many ancient sedimentary rocks.
Pyrite also widely exists in the Longmaxi and Wufeng marine shales in the middle Yangtze …

Sedimentary molybdenum (Mo) accumulation is a robust proxy for sulfidic conditions in both
modern and ancient aquatic systems and has been used to infer changing marine redox …

In many unconventional hydrocarbon systems, organic matter (OM) substantially contributes
to total porosity of the rock that led to a positive correlation between total organic carbon …

Based on the sedimentological and geochemical analysis of total organic carbon (TOC) and
major and trace elements in the marine Upper Ordovician-Lower Silurian Wufeng-Longmaxi …

Organic matter is of emerging interest as a control on molybdenum (Mo) biogeochemistry,
and information on isotope fractionation during adsorption to organic matter can improve …