Image2_The Influence of the Permian-Triassic Magmatism in the Tunguska Basin, Siberia on the Regional Floristic Biota of the Permian-Triassic Transition in the Region.pdf

• Main Authors: V. I. Davydov, E. V. Karasev
• Format: Still Image
• Language: unknown
• Published: 2021
• Subjects: Solid Earth Sciences; Climate Science; Atmospheric Sciences not elsewhere classified; Exploration Geochemistry; Inorganic Geochemistry; Isotope Geochemistry; Organic Geochemistry; Geochemistry not elsewhere classified; Igneous and Metamorphic Petrology; Ore Deposit Petrology; Palaeontology (incl. Palynology); Structural Geology; Tectonics; Volcanology; Geology not elsewhere classified; Seismology and Seismic Exploration; Glaciology; Hydrogeology; Natural Hazards; Quaternary Environments; Earth Sciences not elsewhere classified; Evolutionary Impacts of Climate Change; Permian-Triassic transition; Norilsk Russia; radioisotopic ages; geomagnetic secular variartion; multi-stadial intrusions; floral diversity and dynamics; Norilsk; Tunguska; Talnakh; norilsk; Siberia
• Online Access: https://doi.org/10.3389/feart.2021.635179.s002; https://figshare.com/articles/figure/Image2_The_Influence_of_the_Permian-Triassic_Magmatism_in_the_Tunguska_Basin_Siberia_on_the_Regional_Floristic_Biota_of_the_Permian-Triassic_Transition_in_the_Region_pdf/14540112

The end-Permian extinction event (EPEE) considered to have been caused by the eruption of the Siberian Large Igneous Province (SLIP), the age of which is critical for extinction-SLIP model evaluation. The Tunguska Basin flora during this time, in accordance with the EPEE model, supposed to have been...