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Paleoecological characterization of the Middle Siberian Trappean plateau during the middle period of its formation (terminal Permian)

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Abstract

The formation of the Middle Siberian Traps has been considered one of the main causes for the change in the biota at the Permian-Triassic boundary. At the first stage of the formation of the volcanic plateau (Lebedevskian time), volcanism was dominated by tuffs; at the second stage (Khungtukunian time), by tuffs and lavas; and at the last stage (Putoranian time), by flood basalts. The paper presents a paleoecological characterization of the plateau at the middle (Khungtukunian) stage, immediately before the Permian-Triassic boundary (ammonoid standard). At the beginning of this stage the plateau reached an altitude of about 500 m above sea level, at the end of the stage it was higher than 800 m above sea level (Sadovnikov and Turlova, 2004). The Khungtukunian deposits have yielded more than 230 species, belonging to more than 70 genera of plants, conchostracans, ostracods, bivalves, and fishes.

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Correspondence to G. N. Sadovnikov.

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Original Russian Text © G.N. Sadovnikov, 2015, published in Paleontologicheskii Zhurnal, 2015, No. 4, pp. 103–110.

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Sadovnikov, G.N. Paleoecological characterization of the Middle Siberian Trappean plateau during the middle period of its formation (terminal Permian). Paleontol. J. 49, 438–447 (2015). https://doi.org/10.1134/S0031030115040152

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