A two-phase end-Triassic mass extinction
The end-Triassic mass extinction was one of the big five crises of the fossil record. It affected
diverse marine groups, including bivalves, brachiopods, ostracods, calcareous algae …
diverse marine groups, including bivalves, brachiopods, ostracods, calcareous algae …
Global organic carbon burial during the Toarcian oceanic anoxic event: Patterns and controls
The early Toarcian oceanic anoxic event (T-OAE,~ 183 Ma), also known as the Jenkyns
Event, was one of the most important hyperthermal events of the Phanerozoic, caused by the …
Event, was one of the most important hyperthermal events of the Phanerozoic, caused by the …
Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis
The sources of isotopically light carbon released during the end-Triassic mass extinction
remain in debate. Here, we use mercury (Hg) concentrations and isotopes from a pelagic …
remain in debate. Here, we use mercury (Hg) concentrations and isotopes from a pelagic …
The Triassic–Jurassic transition–A review of environmental change at the dawn of modern life
Abstract The Triassic–Jurassic transition, which is here broadly defined as extending from
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …
Rhenium-osmium isotope evidence for the onset of volcanism in the central Panthalassa Ocean during the Norian “chaotic carbon episode”
The late Norian “chaotic carbon episode” in the Late Triassic has been identified in North
America, Italy, and China, reflecting a global carbon isotope perturbation. Although it has …
America, Italy, and China, reflecting a global carbon isotope perturbation. Although it has …
Unveiling a new oceanic anoxic event at the Norian/Rhaetian boundary (Late Triassic)
The latest Triassic was characterised by protracted biotic extinctions concluding in the End-
Triassic Extinction (~ 200 Ma) and a global carbon cycle perturbation. The onset of declining …
Triassic Extinction (~ 200 Ma) and a global carbon cycle perturbation. The onset of declining …
Deep-ocean anoxia across the Pliensbachian-Toarcian boundary and the Toarcian Oceanic Anoxic Event in the Panthalassic Ocean
Abstract The early Toarcian Oceanic Anoxic Event (T-OAE, or Jenkyns Event,~ 183 million
years ago) was a major hyperthermal and global carbon-cycle perturbation, likely …
years ago) was a major hyperthermal and global carbon-cycle perturbation, likely …
Shallow-and deep-ocean Fe cycling and redox evolution across the Pliensbachian–Toarcian boundary and Toarcian Oceanic Anoxic Event in Panthalassa
W Chen, DB Kemp, T He, RJ Newton, Y ** biota of Yunnan Province, China
Abstract The early Middle Triassic (Anisian) Luo** biota is representative of marine
ecosystems following their full recovery after the Permian-Triassic mass extinction; however …
ecosystems following their full recovery after the Permian-Triassic mass extinction; however …