The Ediacaran biota were soft-bodied organisms, many with enigmatic phylogenetic placement and ecology, living in marine environments between 574 and 539 million years …
The geochemistry of the carbonate sedimentary record is invaluable for understanding the ancient seawater evolution of carbon and redox-sensitive elements. However, the …
R Shen, A Shen, K Yu, CA McCormick, W Jiang… - Sedimentary …, 2023 - Elsevier
Rare earth elements and yttrium (REE+ Y), with stable and predictable chemical characteristics, serve as important proxies for diagenetic fluids, but the effect of …
The improving sensitivity of mass-spectrometers has opened the potential of using stable isotope signatures of the rare Earth elements (REE) as geochemical tracers. However, thus …
The end-Triassic extinction (ETE) ranks as one of the 'Big Five'biotic crises of the Phanerozoic and is thought to be triggered by volcanism of the Central Atlantic Magmatic …
Structurally controlled dolomitization typically involves the interaction of high‐pressure (P), high‐temperature (T) fluids with the surrounding host rock. Such reactions are often …
We measured the Ce concentration, oxidation state, and isotope composition of bauxites developed on the Columbia River Basalts (CRBs) to evaluate the impacts of redox and non …
GY Wei, D Li, Z Lu, G Jiang, HF Ling - Global and Planetary Change, 2024 - Elsevier
The oceanic oxygenation from the Ediacaran to the early Cambrian (ca. 635–520 Ma) has been commonly linked with the radiation or innovation of early metazoans. However, in this …
Iron (Fe) oxyhydroxides are major phases that may control the cerium (Ce) behavior in the Earth's Critical Zone. However, understanding Ce behavior with Fe oxyhydroxides remains …