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
The end-Triassic extinction (ETE) is associated with rapid atmospheric CO2-driven warming amplified ...
18 pagesInternational audienceThe Early Triassic is generally portrayed as a time of various, high e...
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...
A detailed, 10 m.y. redox history of Changhsingian to Anisian (latest Permian to Middle Triassic) oc...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
Geochemical, biomarker, and isotopic evidence suggests that the end-Permian was characterized by ext...
The end-Permian mass extinction, ~252 million years ago, is notable for a complex recovery period of...
Severe changes in ocean redox, nutrient cycling, and marine productivity accompanied most Phanerozoi...
Water column oxygen deficiency has been considered as a potent driver of the extinction of marine be...
The role of ocean anoxia as a cause of the end-Triassic marine mass extinction is widely debated. He...
One method to gain perspective on the consequences of modern climate change and future projections i...
Both the duration and severity of deep-water anoxic conditions across the Permian-Triassic mass exti...
The end-Permian mass extinction (EPME) has been linked with the widespread development of oxygen-poo...
The end-Triassic extinction (ETE) is associated with rapid atmospheric CO2-driven warming amplified ...
18 pagesInternational audienceThe Early Triassic is generally portrayed as a time of various, high e...
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...
A detailed, 10 m.y. redox history of Changhsingian to Anisian (latest Permian to Middle Triassic) oc...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
Geochemical, biomarker, and isotopic evidence suggests that the end-Permian was characterized by ext...
The end-Permian mass extinction, ~252 million years ago, is notable for a complex recovery period of...
Severe changes in ocean redox, nutrient cycling, and marine productivity accompanied most Phanerozoi...
Water column oxygen deficiency has been considered as a potent driver of the extinction of marine be...
The role of ocean anoxia as a cause of the end-Triassic marine mass extinction is widely debated. He...
One method to gain perspective on the consequences of modern climate change and future projections i...
Both the duration and severity of deep-water anoxic conditions across the Permian-Triassic mass exti...
The end-Permian mass extinction (EPME) has been linked with the widespread development of oxygen-poo...
The end-Triassic extinction (ETE) is associated with rapid atmospheric CO2-driven warming amplified ...
18 pagesInternational audienceThe Early Triassic is generally portrayed as a time of various, high e...
Biomarker, palaeontological and isotopic evidence suggests that the Late Permian carbonate seas, i.e...