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 …

A newly compiled global reef database indicates that the 5–6 Myr long Frasnian (Late
Devonian) metazoan reef episode had relatively low diversity compared to Middle Devonian …

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

We present detailed biostratigraphy based on conodonts and palaeoenvironmental trends
deduced from microfacies and conodont abundance through the Famennian (Late …

To provide a new insight into the diagenetic versus detrital origin of the magnetic
susceptibility variations in ancient carbonate sequences, a study was conducted within four …

The lower Frasnian (transitans Zone with Ancyrodella priamosica= MN 4 Zone) rhythmic
basin succession of marly limestones and shales (upper Szydlówek Beds) at Kostomloty …

Song, j., Crasquin, s. & Gong, Y., September 2016. Ostracods of the Late Devonian
Frasnian/Famennian transition from western Junggar, **njiang, NW China. Alcheringa 41 …

The lower part of the Frasnian succession in the Radlin Syncline (Kielce–Łagów
Synclinorium, southern region of the Holy Cross Mountains), in the two studied successions …

This study focuses on the Late Devonian ostracods and their responses to the F—F
(Frasnian-Famennian) event based on abundant materials collected from the Yangdi and …

Four major microfacies have been recognized in the Psie Górki section and the bioclastic
content indicates an open marine environment in the photic zone close to an algal shole …