Geophysical Monograph Series, Page 1-26., 2021 Exploring the links between Large Igneous Provinces and dramatic environmental impact
An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Richard E. Ernst +8 more
wiley +11 more sources
The fate of the homoctenids (Tentaculitoidea) during the Frasnian–Famennian mass extinction (Late Devonian) [PDF]
Geobiology, 2006 ABSTRACTThe homoctenids (Tentaculitoidea) are small, conical‐shelled marine animals that are among the most abundant and widespread of all Late Devonian fossils. They were a principal casualty of the Frasnian–Famennian (F‐F, Late Devonian) mass extinction, and thus provide an insight into the extinction dynamics. Despite their abundance during the Late
Alberti GKB +48 more
openaire +5 more sources
Author Correction: Basin-scale reconstruction of euxinia and Late Devonian mass extinctions [PDF]
Nature, 2023 Swapan Sahoo +8 more
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Patterns of evolution and extinction in proetid trilobites during the late Devonian mass extinction event, Canning Basin, Western Australia [PDF]
Palaeontology, 2013 Abstract: In the early Late Devonian, terminal Frasnian proetid trilobites have previously only been known from Europe and North Africa. For the first time, a rich fauna of late Frasnian proetids is described from the Virgin Hills Formation, Canning Basin, Western Australia.
Raimund Feist, Kenneth J. McNamara
openalex +3 more sources
Edinburgh Student Journal of ScienceThe Late-Devonian Mass Extinction (LDME) extinguished up to 40% of all marine species, with evidence suggesting marine anoxia was the primary cause.
Craig Mellon +2 more
doaj +3 more sources
地质科技通报, 2022 The Frasnian-Famennian extinction in the late Devonian was one of the largest mass extinction during Earth's history, which was believed to be caused by the plant landing-indued intensification of terrestrial chemical weathering and the consequent ...
Faliang Deng +4 more
doaj +1 more source
Frontiers in Earth Science, 2021 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
Frontiers in Earth Science, 2021 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
Functional consequences of Palaeozoic reef collapse
Scientific Reports, 2022 Biogenic reefs have been hotspots of biodiversity and evolutionary novelty throughout the Phanerozoic. The largest reef systems in Earth’s history occurred in the Devonian period, but collapsed during the Late Devonian Mass Extinction.
Tom C. L. Bridge +4 more
doaj +1 more source
Invasive species and biodiversity crises: testing the link in the late devonian. [PDF]
PLoS ONE, 2010 During the Late Devonian Biodiversity Crisis, the primary driver of biodiversity decline was the dramatic reduction in speciation rates, not elevated extinction rates; however, the causes of speciation decline have been previously unstudied.
Alycia L Stigall
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