A detailed, 10 my redox history of Changhsingian to Anisian (latest Permian to Middle
Triassic) oceans in ramp settings is reconstructed based on framboidal pyrite analysis from …

A wide range of various proxies (eg, mineralogy, organic carbon, inorganic geochemistry, C
and Mo isotopes, and framboidal pyrite) were applied for interpretation of changing oceanic …

Large, globally documented negative δ 13 C excursions that occur across the Permian-
Triassic transition are thought to represent the isotopic fingerprint of considerable releases …

We describe variations in trace element compositions that occurred on the deep seafloor of
palaeo-superocean Panthalassa during the end-Permian mass extinction based on samples …

Detailed geochemical analyses (δ13Ccarb, δ13Corg, δ34Ssulfide, and abundance of
sulfide, carbonate and organic carbon) were performed on samples from the Wangjiawan …

The recovery of marine ecosystems in the aftermath of the Permian-Triassic mass extinction
was accompanied by significant carbon-cycle perturbations, as reflected in large-amplitude …

The largest mass extinction of biota in the Earth's history occurred during the Permian–
Triassic transition and included two extinctions, one each at the latest Permian (first phase) …

The global carbon cycle experienced a major perturbation during the Permian–Triassic
transition, reflected inter alia in a large increase in the vertical (shallow-to-deep) gradient of …

Large carbon cycle perturbations associated with the Middle Permian (Capitanian) mass
extinction have been widely reported, but their causes and timing are still in dispute. Low …

Abstract The Central European Basin is very suitable for high-resolution multistratigraphy of
Late Permian to Early Triassic continental deposits. Here the well exposed continuous …