Carbon and sulfur isotopic data, together with biomarker and iron speciation analyses of the Hovea-3 core that was drilled in the Perth Basin, Western Australia, indicate that euxinic conditions prevailed in the paleowater column during the Permian-Triassic superanoxic event. Biomarkers diagnostic for anoxygenic photosynthesis by Chlorobiaceae are particularly abundant at the boundary and into the Early Triassic. Similar conditions prevailed in the contemporaneous seas off South China. Our evidence for widespread photiczone euxinic conditions suggests that sulfide toxicity was a driver of the extinction and a factor in the protracted recovery
Both the duration and severity of deep-water anoxic conditions across the Permian-Triassic mass exti...
Fabric and pyrite framboid size analysis of Permian to Jurassic samples from the Mino-Tamba terrane ...
Biomarker, palaeontological and isotopic evidence suggests that the Late Permian carbonate seas, i.e...
Carbon and sulfur isotopic data, together with biomarker and iron speciation analyses of the Hovea-3...
Reconstruction of basin-scale paleogeography and paleoenvironments in the northern Perth Basin durin...
Severe changes in ocean redox, nutrient cycling, and marine productivity accompanied most Phanerozoi...
The end-Triassic extinction (ETE) is associated with rapid atmospheric CO2-driven warming amplified ...
Geochemical, biomarker, and isotopic evidence suggests that the end-Permian was characterized by ext...
Most organic geochemical studies of the Permian-Triassic mass extinction (PTME) have utilised marine...
The Late Triassic mass extinction event is the most severe global warming–related crisis to have aff...
High-resolution biomarker and compound-specific isotope distributions, coupled with the degradation ...
The end-Permian mass extinction ~252 Mya was the most severe biotic crisis in Earth history, with \u...
The identification of the Permian–Triassic boundary (PTB) and Permian–Triassic mass extinction event...
A detailed, 10 m.y. redox history of Changhsingian to Anisian (latest Permian to Middle Triassic) oc...
Marine redox conditions through the Permian-Triassic (P-T) boundary interval have been intensively s...
Both the duration and severity of deep-water anoxic conditions across the Permian-Triassic mass exti...
Fabric and pyrite framboid size analysis of Permian to Jurassic samples from the Mino-Tamba terrane ...
Biomarker, palaeontological and isotopic evidence suggests that the Late Permian carbonate seas, i.e...
Carbon and sulfur isotopic data, together with biomarker and iron speciation analyses of the Hovea-3...
Reconstruction of basin-scale paleogeography and paleoenvironments in the northern Perth Basin durin...
Severe changes in ocean redox, nutrient cycling, and marine productivity accompanied most Phanerozoi...
The end-Triassic extinction (ETE) is associated with rapid atmospheric CO2-driven warming amplified ...
Geochemical, biomarker, and isotopic evidence suggests that the end-Permian was characterized by ext...
Most organic geochemical studies of the Permian-Triassic mass extinction (PTME) have utilised marine...
The Late Triassic mass extinction event is the most severe global warming–related crisis to have aff...
High-resolution biomarker and compound-specific isotope distributions, coupled with the degradation ...
The end-Permian mass extinction ~252 Mya was the most severe biotic crisis in Earth history, with \u...
The identification of the Permian–Triassic boundary (PTB) and Permian–Triassic mass extinction event...
A detailed, 10 m.y. redox history of Changhsingian to Anisian (latest Permian to Middle Triassic) oc...
Marine redox conditions through the Permian-Triassic (P-T) boundary interval have been intensively s...
Both the duration and severity of deep-water anoxic conditions across the Permian-Triassic mass exti...
Fabric and pyrite framboid size analysis of Permian to Jurassic samples from the Mino-Tamba terrane ...
Biomarker, palaeontological and isotopic evidence suggests that the Late Permian carbonate seas, i.e...