Results 21 to 30 of about 2,503 (171)
The Late Devonian Frasnian–Famennian (F–F) mass extinction has been long-time debated by non-volcanic causes, extra-terrestrial impacts, and large igneous province (LIP) eruptions.
Jiawei Zhang +8 more
doaj +1 more source
Frasnian-Famennian stable isotopes ratios of CG-1_core
Frasnian-Famennian stable isotopes ratios of Sinsin section ...
Day, James E +15 more
core +1 more source
Biodiversity, distribution and patterns of extinction of the last odontopleurid tilobites during the Devonian (Givetian, Frasnian) [PDF]
Biostratigraphical ranges and palaeogeographical distribution of mid-Givetian to end-Frasnian odontopleurids are investigated. The discovery of Leonaspis rhenohercynica sp. nov. in mid-Givetian strata extends this genus unexpectedly up to the late Middle
McNamara, K. J. +3 more
core +2 more sources
Frasnian-Famennian magnetic susceptibility of Fuhe_section
Frasnian-Famennian magnetic susceptibility of ...
Day, James E +15 more
core +1 more source
Frasnian-Famennian high resolution organic carbon isotope data from South China, Fuhe section
Frasnian-Famennian low resolution organic carbon isotope data from South China, Fuhe ...
Day, James E +15 more
core +1 more source
Revision of the Late Devonian ptyctodonts (Vertebrata, Placodermi) from southern Poland [PDF]
New studies on Frasnian ptyctodonts, including the revision of historic material in addition to the description of new material, have resulted in the detailed description of two species of Ptyctodus (Ptyctodus obliquus, Ptyctodus kielcensis), eight ...
Katarzyna Grygorczyk +2 more
doaj +1 more source
Frasnian-Famennian magnetic susceptibility of Sinsin section, Belgium
Frasnian-Famennian magnetic susceptibility of Sinsin section ...
Day, James E +15 more
core +1 more source
Facies patterns and depositional processes in two Frasnian mixed siliciclastic-carbonate systems in the Cantabrian Mountains, northwest Spain [PDF]
Relative sea level fluctuations during the Frasnian generated two shallow-marine, mixed siliciclastic-carbonate successions in the Devonian Asturo-Leonese Basin.
van Loevezijn, Gerard B.S. +1 more
core +2 more sources
Three stages, namely Middle Devonian (I), Early Late Devonian (II) and Late Late Devonian (III), are distin-guished in the evolution of antiarchs (Placodermi, Antiarchi) in the Middle-Late Devonian of Northern Eurasia.
S. V. Moloshnikov
doaj +1 more source
At present, within the Baltic-Ladoga structural-facies zone characterized by the distribution of coastal-marine and coastal-continental deposits of the Lower and Middle Frasnian outcrops of bedrock are practically lost.
Tsinkoburova M. G. +2 more
doaj +1 more source

