A Middle Permian mass extinction, first discovered in 1994, has become known as the “end-
Guadalupian event” in the literature. However, recent studies of foraminifera-and brachiopod …

The temporal link between mass extinctions and large igneous provinces is well known.
Here, we examine this link by focusing on the potential climatic effects of large igneous …

Previous studies of the end-Permian mass extinction have established that it was
geologically rapid, but condensed sections have made it difficult to establish the exact timing …

The boundaries of the Devonian, Carboniferous, and Permian stages of the Global
Stratigraphic Reference Scale (abbreviated to Global Stratigraphic Scale—GSS) are …

The Middle Permian Emeishan large igneous province of SW China has provided the
quintessential example of the phenomenon of kilometre-scale pre-eruption domal uplift …

Clarkina postbitteri hongshuiensis to C. dukouensis and nearly coincides with the Middle-
Upper Absaroka Megasequence boundary and as such is documented within a …

Middle to Upper Permian shallow marine carbonates in the Kamura area, Kyushu (SW
Japan), were derived from a paleo-atoll complex developed on an ancient seamount in mid …

The main components of Asselian through Artinskian conodont faunas found around the
world are basically the same, and the provincialism is indicated only by less common …

The Capitanian (late Guadalupian) high positive plateau interval of carbonate carbon
isotope ratio (δ13Ccarb) was recognized lately in a mid-Panthalassan paleo-atoll limestone …

New fieldwork was carried out in the central and eastern Alborz, addressing the sedimentary
succession from the Pennsylvanian to the Early Triassic. A regional synthesis is proposed …