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- W4310993451 abstract "Abstract Global climate and environmental changes were the main causes of the end-Triassic mass extinction. However, direct sedimentological evidence of environmental catastrophes is rare in Triassic – Jurassic interval, especially in the eastern Tethys region. The newly discovered in-situ trunk fossils in paleosol surface and a set of unique branch-supported sandstones below may record the environmental disaster at the Triassic-Jurassic interval in the northern Sichuan Basin. Sedimentological data showed the strong storm prevalent induced the lodging direction of in-situ trunks is opposite to the direction of paleocurrent. Enhancement of large-scale runoff along with the dramatic increase of woody detrital input may indicate the deforesting at the Triassic -Jurassic boundary in eastern Tethys, Sichuan Basin." @default.
- W4310993451 created "2022-12-22" @default.
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- W4310993451 date "2022-11-29" @default.
- W4310993451 modified "2023-09-27" @default.
- W4310993451 title "Storms and deforestation prior to Triassic – Jurassic Boundary? Evidence from woody fossils at upmost Xujiahe Formation, Southwestern China" @default.
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- W4310993451 doi "https://doi.org/10.21203/rs.3.rs-2138752/v1" @default.
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