The Permian-Triassic transition in the Karoo Basin of South Africa was characterized by a
rapid and apparently basin-wide change from meandering to braided river systems, as …

The Karoo basin of South Africa exposes a succession of Upper Permian to Lower Triassic
terrestrial strata containing abundant terrestrial vertebrate fossils. Paleomagnetic …

The extinction of vertebrates around the time of the Permian-Triassic boundary has long
been regarded as a gradual event occurring over millions of years. Our new field …

The end-Permian extinction records the greatest ecological catastrophe in Earth history. The
vertebrate fossil record in the Karoo Basin, South Africa, has been used for more than a …

Distinct assemblages of paleosols above and below the Permian–Triassic boundary in the
Karoo Basin of South Africa are evidence for reorganization of ecosystems following this …

The southern half of the main Karoo Basin in South Africa contains an almost continuous
stratigraphic record of terrestrial sedimentation through the Permo-Triassic boundary (PTB) …

Recent advances in radiometric dating and isotopic stratigraphy have resulted in a different
placement of the Permian-Triassic boundary within the sedimentary sequence of the Sydney …

Mineralogical and geochemical studies of the non-marine Permian–Triassic (P–Tr)
boundary across two stratigraphically well-constrained sections (Commando Drift Dam and …

The southern part of the Karoo Basin of South Africa contains a near complete stratigraphic
record of the Permo-Triassic boundary (PTB). Isotope-and magneto-stratigraphy confirm that …

The end-Permian mass extinction (EPME) is widely recognised as the largest mass
extinction in Phanerozoic history. In marine strata the main extinction event is well …