Results 31 to 40 of about 1,937 (211)
The Late Devonian envelops one of Earth's big five mass extinction events at the Frasnian-Famennian boundary (374 Ma). Environmental change across the extinction severely affected Devonian reef-builders, besides many other forms of marine life.
Day, James E +15 more
core +1 more source
Frasnian-Famennian magnetic susceptibility of Fuhe_section
Frasnian-Famennian magnetic susceptibility of ...
Day, James E +15 more
core +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
Iron microbial communities in Belgian Frasnians carbonate mounds
The Belgian Frasnian carbonate mounds occur in three stratigraphic levels in an overall backstepping succession. Petit-Mont and Arche Members form the famous red and grey “marble” exploited for ornamental stone since Roman times. The evolution and distribution of the facies in the mounds is thought to be associated with ecologic evolution and relative ...
Boulvain, Frédéric +4 more
openaire +2 more sources
Key Points 7 μm spot‐diameter LA‐MC‐ICP‐MS analyses yield accurate zircon U‐Pb ages. 1013 Ω amplifier resistors improve low‐signal Pb measurements. Saturn correction protocols minimise down‐hole fractionation effects. We present a systematic evaluation of high spatial‐resolution zircon U‐Pb dating using a Thermo Scientific Neoma multi‐collector ICP‐MS ...
Cristiano Lana, John D. Clemens
wiley +1 more source
Microbial mounds prior to the Frasnian-Famennian mass extinctions, Hantang, Guilin, South China
Late Frasnian mounds of the Yunghsien Formation, Guilin, South China, developed as part of the Guilin platform, mostly in reef-flat and platform margin settings. Microbial mounds in platform margin settings at Hantang, about 10 km west of Guilin, contain
Webb, GE +6 more
core +1 more source
Research subject. This article focuses on the geological structure of the northern part of the Pai-Khoi carbonate parautochthone.Materials and methods. The study was based on the data obtained on the key sections of the North-Western Pai-Khoi.
D. A. Gruzdev +3 more
doaj +1 more source
LATE DEVONIAN-CARBONIFEROUS CONODONTS FROM EASTERN IRAN
Conodont data from acid-leaching 110 samples from two Late Devonian-Carboniferous areas in the Shotori Range (Tabas region) of eastern Iran are presented.
MEHDI YAZDI
doaj +1 more source
Late Devonian time was a period of rapid upheaval in the Earth system, including climate change, sea level changes, widespread ocean anoxia, and the Frasnian-Famennian mass extinction; the cause(s) of these changes remain(s) uncertain.
Theodore Green +10 more
doaj +1 more source
Frasnian-Famennian magnetic susceptibility of H-32 core drill, Iowa
Frasnian-Famennian magnetic susceptibility of H-32 core drill ...
Day, James E +15 more
core +1 more source

