0000000000381265

AUTHOR

Tianchen He

showing 2 related works from this author

Was climatic cooling during the earliest Carboniferous driven by expansion of seed plants?

2021

Abstract The expansion of land plants is considered to have played a key role in triggering the Late Paleozoic Ice Age (LPIA), but evidence linking climatic events to terrestrial floral changes is limited. Here, we generated bulk carbonate δ13C, conodont δ18O and 87Sr/86Sr profiles from the lowermost Carboniferous of South China and Vietnam in order to investigate their relationship to contemporaneous land plant evolution. Climatic cooling in the mid-Tournaisian coincided with large perturbations to the global carbon cycle and continental weathering regimes as well as with a major diversification episode among seed plants. These relationships are consistent with terrestrial floral changes t…

010504 meteorology & atmospheric sciencesbiologyPaleozoicEarth scienceClimate changeWeathering15. Life on land010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCarbon cycleGeophysics13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyCarboniferousEarth and Planetary Sciences (miscellaneous)Ice ageConodontGlobal coolingGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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An enormous sulfur isotope excursion indicates marine anoxia during the end-Triassic mass extinction

2020

The role of ocean anoxia as a cause of the end-Triassic marine mass extinction is widely debated. Here, we present carbonate-associated sulfate δ34S data from sections spanning the Late Triassic–Early Jurassic transition, which document synchronous large positive excursions on a global scale occurring in ~50 thousand years. Biogeochemical modeling demonstrates that this S isotope perturbation is best explained by a fivefold increase in global pyrite burial, consistent with large-scale development of marine anoxia on the Panthalassa margin and northwest European shelf. This pyrite burial event coincides with the loss of Triassic taxa seen in the studied sections. Modeling results also indica…

Extinction eventBiogeochemical cycleMultidisciplinaryExtinction010504 meteorology & atmospheric sciencesIsotopefungiengineering.material010502 geochemistry & geophysics01 natural sciencesPerturbation (geology)sulfure isotope end Triassic mass extinctionhumanitieschemistry.chemical_compoundPaleontologyδ34SchemistryengineeringPyriteSulfateGeology0105 earth and related environmental sciences
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