U-Pb constraints on pulsed eruption of the Deccan Traps across the end-Cretaceous mass extinction

@article{Schoene2019UPbCO,
  title={U-Pb constraints on pulsed eruption of the Deccan Traps across the end-Cretaceous mass extinction},
  author={Blair Schoene and Michael P. Eddy and Kyle M. Samperton and C. Brenhin Keller and Gerta Keller and Thierry Adatte and Syed F.R. Khadri},
  journal={Science},
  year={2019},
  volume={363},
  pages={862 - 866}
}
Two timelines for extinction The Cretaceous-Paleogene extinction that wiped out the nonavian dinosaurs 66 million years ago was correlated with two extreme events: The Chicxulub impact occurred at roughly the same time that massive amounts of lava were erupting from the Deccan Traps (see the Perspective by Burgess). Sprain et al. used argon-argon dating of the volcanic ash from the Deccan Traps to argue that a steady eruption of the flood basalts mostly occurred after the Chicxulub impact… 
An evaluation of Deccan Traps eruption rates using geochronologic data
Abstract. Recent attempts to establish the eruptive history of the Deccan Traps large igneous province have used both U−Pb (Schoene et al., 2019) and 40Ar/39Ar (Sprain et al., 2019) geochronology.
An evaluation of Deccan Traps eruption rates using geochronologic data
Abstract. Recent attempts to establish the eruptive history of the Deccan Traps large igneous province have used both U-Pb (Schoene et al., 2019) and 40Ar/39Ar (Sprain et al., 2019) geochronology.
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Rapidly expanding geochronological, paleomagnetic and volcanological data of the Deccan Volcanic Province (DVP) has given new insights to the expansive knowledge on it that had been built up through
No Cretaceous‐Paleogene Boundary in Exposed Rajahmundry Traps: A Refined Chronology of the Longest Deccan Lava Flows From 40Ar/39Ar Dates, Magnetostratigraphy, and Biostratigraphy
Deccan Traps flood basalt volcanism affected ecosystems spanning the end‐Cretaceous mass extinction, with the most significant environmental effects hypothesized to be a consequence of the largest
On impact and volcanism across the Cretaceous-Paleogene boundary
TLDR
Carbon cycle modeling and paleotemperature records are used to constrain the timing of volcanogenic outgassing and found support for major out gassing beginning and ending distinctly before the impact, with only the impact coinciding with mass extinction and biologically amplified carbon cycle change.
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TLDR
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