Abstract The global Hangenberg Crisis near the Devonian–Carboniferous boundary (DCB)
represents a mass extinction that is of the same scale as the so-called 'Big Five'first-order …

Abstract The Late Paleozoic Ice Age (LPIA) is a critical interval for marine ecosystems when
marine fauna was viewed to have experienced a second-order mass extinction and a …

Chrono-, litho-and biostratigraphy across the Devonian–Carboniferous transition are
reviewed to provide a precise time framework for the global Hangenberg Crisis and for the …

Microbial carbonates commonly flourished following mass extinction events. The end-
Devonian (Hangenberg) mass extinction event is a first-order mass extinction on the scale of …

The timing of the final collision of Laurentia and Gondwana as well as the disappearance of
the gateway between the Rheic and Tethyan oceans are quite controversial and poorly …

Abstract The Devonian–Carboniferous boundary is associated with a major extinction event
of the Phanerozoic. It was also a time marked by a rapid but short-lasting change in …

The late Viséan to early Bashkirian shallow-water carbonate Valdediezma Platform in the
Picos de Europa Province of the Cantabrian Zone, has been subdivided into eight …

Ten foraminiferal zones are proposed in the Youjiang Basin (South China): Pojarkovella,
Pojarkovella nibelis-Endothyranopsis compressa, Cribrospira panderi-Eostaffella ikensis …

Abstract The Lower Carboniferous Mobarak Formation records the development of a storm-
sensitive pervasive carbonate factory on the southern Paleo-Tethyan passive margin …

Abstract The Kirchbach Limestone occurs in the middle part of the early Viséan to Bashkirian
Hochwipfel Formation, which was deposited in a flysch basin that formed during an …