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Your search keyword '"Chu, Daoliang"' showing total 10 results
Start Over Author "Chu, Daoliang" Publisher geological society of america
10 results on '"Chu, Daoliang"'

4. Metal-induced stress in survivor plants following the end-Permian collapse of land ecosystems

Author

Marine palynology and palaeoceanography, Marine Palynology, Chu, Daoliang, Corso, Jacopo Dal, Shu, Wenchao, Song, Haijun, Wignall, Paul B., Grasby, Stephen E., van de Schootbrugge, Bas, Zong, Keqing, Wu, Yuyang, Tong, Jinnan, Marine palynology and palaeoceanography, Marine Palynology, Chu, Daoliang, Corso, Jacopo Dal, Shu, Wenchao, Song, Haijun, Wignall, Paul B., Grasby, Stephen E., van de Schootbrugge, Bas, Zong, Keqing, Wu, Yuyang, and Tong, Jinnan

Published
2021

10. Five million years of high atmospheric CO2 in the aftermath of the Permian-Triassic mass extinction.

Author

Joachimski, Michael M., Müller, Johann, Gallagher, Timothy M., Mathes, Gregor, Chu, Daoliang L., Mouraviev, Fedor, Silantiev, Vladimir, Sun, Yadong D., and Tong, Jinnan N.

Subjects
*MASS extinctions, *GASWORKS, *TRIASSIC Period, *CARBON cycle, *ATMOSPHERE, *PALEOPEDOLOGY
Abstract

The end-Permian mass extinction, the largest biological crisis in Earth history, is currently understood in the context of Siberian Traps volcanism introducing large quantities of green- house gases to the atmosphere, culminating in the Early Triassic hothouse. In our study, the late Permian and Early Triassic atmospheric CO2 history was reconstructed by applying the paleosol pCO2 barometer. Atmospheric pCO2 shows an approximate 4x increase from mean concentrations of 412-919 ppmv in the late Permian (Changhsingian) to maximum levels between 2181 and 2610 ppmv in the Early Triassic (late Griesbachian). Mean CO2 estimates for the later Early Triassic are between 1261-1936 ppmv (Dienerian) and 1063-1757 ppmv (Spathian). Significantly lower concentrations ranging from 343 to 634 ppmv are reconstructed for the latest Early to Middle Triassic (Anisian). The 5 m.y. episode of elevated pCO2 suggests that negative feedback mechanisms such as silicate weathering were not effective enough to reduce atmospheric pCO2 to precrisis levels and that marine authigenic clay formation (i.e., reverse weathering) may have been an important component of the global carbon cycle keeping atmospheric pCO2 at elevated levels. [ABSTRACT FROM AUTHOR]

Published
2022
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