Diachronous end-Permian terrestrial crises in North and South China

Mercury evidence of Emeishan volcanism driving the mid-Capitanian (Middle Permian) extinction

Volcanic and orbitally forced carbon release during the Middle Eocene Climatic Optimum

Oceanic anoxic event 3 in Arctic Canada—Arc volcanism and ocean fertilization drove anoxia

Marine snowstorm during the Permian–Triassic mass extinction

How Large Igneous Provinces Have Killed Most Life on Earth—Numerous Times

Basaltic sills emplaced in organic-rich sedimentary rocks: Consequences for organic matter maturation and Cretaceous paleo-climate

Collapse of terrestrial ecosystems linked to heavy metal poisoning during the Toarcian oceanic anoxic event

Mercury evidence of Deccan volcanism driving the Latest Maastrichtian warming event

Mercury enrichments during the Carnian Pluvial Event (Late Triassic) in South China

Metal-induced stress in survivor plants following the end-Permian collapse of land ecosystems

Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation: REPLY

Toxic mercury pulses into late Permian terrestrial and marine environments

Late Ordovician mass extinction caused by volcanism, warming, and anoxia, not cooling and glaciation

Ecological disturbance in tropical peatlands prior to marine Permian-Triassic mass extinction

Finding the VOICE: organic carbon isotope chemostratigraphy of Late Jurassic – Early Cretaceous Arctic Canada

Global warming leads to Early Triassic nutrient stress across northern Pangea

Controls on the formation of microbially induced sedimentary structures and biotic recovery in the Lower Triassic of Arctic Canada

The Capitanian (Guadalupian, Middle Permian) mass extinction in NW Pangea (Borup Fiord, Arctic Canada): A global crisis driven by volcanism and anoxia

Biotic responses to volatile volcanism and environmental stresses over the Guadalupian-Lopingian (Permian) transition