Massive wildfires followed oceanic anoxic events during the Late Devonian Frasnian-Famennian mass extinction. [PDF]
Lu M +8 more
europepmc +1 more source
The oldest peracarid crustacean reveals a Late Devonian freshwater colonization by isopod relatives. [PDF]
Robin N +5 more
europepmc +1 more source
Lower and Middle Famennian (Upper Devonian) rugose corals from southern Belgium and northern France
After the late Frasnian extinctions, the rugose corals slowly recovered during the Lower and Middle Famennian (crepida to marginifera conodont zones) in southern Belgium and northern France (Avesnois) (Namur–Dinant Basin). Six genera represented by seven
Poty, E. +3 more
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Early sarcopterygian morphological disparity through the Devonian-Carboniferous crisis. [PDF]
Vanhaesebroucke O +2 more
europepmc +1 more source
Reinvestigation of the Late Devonian Lycopsid Sublepidodendron grabaui from Anhui Province, South China. [PDF]
Xu P, Liu L, Wang D.
europepmc +1 more source
Correction: The Bothriolepis (Placodermi, Antiarcha) material from the Valentia Slate Formation of the Iveragh Peninsula (middle Givetian, Ireland): Morphology, evolutionary and systematic considerations, phylogenetic and palaeogeographic implications. [PDF]
Dupret V +9 more
europepmc +1 more source
The Frasnian-Famennian boundary in the Southern Urals
On the western slope of the Southern Urals, a continuous conodont zone sequence within different facies of the Frasnian-Famennian (F-F) boundary beds is documented.
Abramova, A. N., Artyushkova, O. V.
core
Reconstruction of feeding behaviour and diet in Devonian ctenacanth chondrichthyans using dental microwear texture and finite element analyses. [PDF]
Greif M +5 more
europepmc +1 more source
The early diversification of ray-finned fishes (Actinopterygii): hypotheses, challenges and future prospects. [PDF]
Henderson S +3 more
europepmc +1 more source
Late Famennian stromatoporoids from Debnik Anticline, southern Poland
Famennian Stromatoporoidea from the Quasiendothyra communis Foraminiferal Zone and slightly younger strata from the Dębnik anticline, southern Poland, form a succession of three consecutive assemblages.
Wolniewicz, P
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