Environmental controls on Early Cambrian macroevolution: Insights from the Tarim Basin, Northwest China

Terminal Mesoproterozoic (1.1−1.0 Ga) shallow ocean oxygenation and the rise of crown-group eukaryotes

Cadmium isotope constraints on primary productivity and environmental perturbations across the Late Ordovician mass extinction

Redox changes in the Iapetus Ocean during the Late Ordovician extinction crises

Marine redox and nutrient dynamics linked to the Cambrian radiation of animals

Marine redox dynamics and biotic response to the mid-Silurian Ireviken Extinction Event in a mid-shelf setting

Climatic controls on water-mass chemistry in a Paleocene lacustrine setting, Subei Basin, eastern China

Evidence for abundant organic matter in a Neoarchean banded iron formation

Calibration of redox thresholds in black shale: Insight from a stratified Mississippian basin with warm saline bottom waters

Environmental and trilobite diversity changes during the middle-late Cambrian SPICE event

Implications of an integrated late Ediacaran to early Cambrian stratigraphy of the Siberian Platform, Russia

Origin of the Neoarchean VMS-BIF Metallogenic Association in the Qingyuan Greenstone Belt, North China Craton: Constraints from Geology, Geochemistry, and Iron and Multiple Sulfur ( δ 33 S, δ 34 S, and δ 36 S) Isotopes

Secular variation in seawater redox state during the Marinoan Snowball Earth event and implications for eukaryotic evolution

No effect of thermal maturity on the Mo, U, Cd, and Zn isotope compositions of Lower Jurassic organic-rich sediments

A template for an improved rock-based subdivision of the pre-Cryogenian timescale

The Ediacaran ‘Miaohe Member’ of South China: new insights from palaeoredox proxies and stable isotope data

Ocean euxinia and climate change “double whammy” drove the Late Ordovician mass extinction

A continental-weathering control on orbitally driven redox-nutrient cycling during Cretaceous Oceanic Anoxic Event 2

Phosphorus sources for phosphatic Cambrian carbonates

Stability of the nitrogen cycle during development of sulfidic water in the redox-stratified late Paleoproterozoic Ocean