Palynomorph distribution in Euramerica and western Gondwana, from the Latest Givetian to
the Latest Famennian, may be explained, to some extent, by climatic changes. Detailed …

The Late Devonian mass extinction event near the Frasnian/Famennian (F/F) boundary has
been analysed using conodont biostratigraphy and biofacies, sedimentology, magnetic …

Abstract The Late Devonian was a period of drastic environmental changes, as exemplified
by a major biotic crisis at the Frasnian–Famennian boundary (FFB) and the onset in …

The study aims to put constraints on global environmental changes, which took place during
the Frasnian–Famennian (F/F) transition by using a geochemical multiproxy approach. For …

Abstract The Frasnian–Famennian (F‐F) transition is well exposed in the basinal setting of
La Serre (Montagne Noire, France), where oxygen‐deficient conditions prevailed in bottom …

Bulk magnetic susceptibility measurements on sedimentological samples from all geological
periods have been used widely in the last two decades for correlations and as a proxy for …

Magnetic susceptibility (MS) measurements on carbonate rocks are considered as a proxy
for impurities delivered to the carbonate environments. In the absence of strong climatic or …

Abtract The Late Devonian Frasnian-Famennian (FF) mass extinction event coincides in
many places with the depositionof C org-rich “Kellwasser” facies. Four FF boundary sections …

Summary The Tailfer section (Belgium, northern border of the Dinant Synclinorium) exposes
Middle Frasnian shallow-water limestones. This paper proposes a sedimentological …

To better understand the origin of the initial magnetic susceptibility (χ in) signal in carbonate
sequences, a rock magnetic investigation that includes analysis of acquisition curves of the …