Abstract The Late Devonian (383-359 Ma) was a time of prolonged climate instability with
catastrophic perturbation of global marine ecosystems at the Frasnian-Famennian (FF) and …

Abstract This paper presents Late Devonian (Frasnian–Famennian) global and regional
paleogeographic maps displaying present day coastlines, tectonic elements' boundaries …

Although the prime causation of the Late Devonian Frasnian–Famennian (F–F) mass
extinction remains conjectural, such destructive factors as the spread of anoxia and rapid …

Abstract The Frasnian–Famennian biotic crisis (~ 372 Ma) was one of the “big five” mass
extinction events in the Phanerozoic. This event was associated with dramatic climatic and …

Abstract The Late Devonian Kellwasser Events are two major biodiversity crises recorded at
and just below the Frasnian-Famennian stage boundary for which the ultimate cause or …

We present a new biostratigraphically constrained carbon isotope record from the Lali
section (South China) to document perturbations in the Late Devonian carbon cycle. Positive …

Upper Devonian carbonates deposited through the Frasnian/Famennian (F/F) stage
boundary in the Xom Nha Formation, Central Vietnam, were studied. The section is mainly …

Abstract Changes in the climate-sensitive carbon cycle during the major and second-order
Late Devonian global events were more complex than usually expected, ie, they were not …

Oceanic anoxia is regarded as the major cause of the Late Devonian Frasnian–Famennian
(Fsingle bondF) bio-crisis and Annulata bio-event, and it is associated with continental …

The neodymium isotope composition of micritic limestones from the Devonian–
Carboniferous carbonate platform of the Greater Karatau (southern Kazakhstan) was …