2022
DOI: 10.1073/pnas.2119194119
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Massive perturbations to atmospheric sulfur in the aftermath of the Chicxulub impact

Abstract: Significance Sulfur isotopes confirm a key role for atmospheric sulfur gases in climatic cooling, mass extinction, and the demise of dinosaurs and other global biota after the Chicxulub bolide impact at the Cretaceous–Paleogene boundary. The sulfur isotope anomalies are confined to beds containing ejecta and, in the immediately overlying sediments, are temporally unrelated to known episodes of volcanism that also bracket this event, further addressing the controversial role of the Deccan Traps in the… Show more

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Cited by 11 publications
(3 citation statements)
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“…Following this assumption, S-MIF observed in ice cores and post-GOE sediments is interpreted as a compelling evidence of stratospheric volcanic eruptions that allow profound productions of isotopic anomalous sulfates above the ozone layer in the stratosphere, which subsequently deposit on the Earth’s surface . The presence of S-MIF after the GOE has been used as a proxy to evaluate the influence of past stratospheric eruptions on paleoclimate and mass extinction. The observation of S-MIF in Martian meteorites is also utilized to reconstruct photochemistry of the Martian atmosphere …”
Section: Introductionmentioning
confidence: 99%
“…Following this assumption, S-MIF observed in ice cores and post-GOE sediments is interpreted as a compelling evidence of stratospheric volcanic eruptions that allow profound productions of isotopic anomalous sulfates above the ozone layer in the stratosphere, which subsequently deposit on the Earth’s surface . The presence of S-MIF after the GOE has been used as a proxy to evaluate the influence of past stratospheric eruptions on paleoclimate and mass extinction. The observation of S-MIF in Martian meteorites is also utilized to reconstruct photochemistry of the Martian atmosphere …”
Section: Introductionmentioning
confidence: 99%
“…Additionally, a wave of WGD events have been identified in different angiosperm lineages around the Cretaceous‐Paleogene (K‐Pg) boundary (Fawcett et al ., 2009; Vanneste et al ., 2014; Van de Peer et al ., 2017; Wu et al ., 2020). The K‐Pg boundary is marked by mass extinctions triggered by an asteroid impact that caused prolonged global cooling and darkness on Earth (Pope et al ., 1997; Vellekoop et al ., 2014; Junium et al ., 2022).…”
Section: Introductionmentioning
confidence: 99%
“…Contemporary hypotheses on the cause of the Cretaceous/Paleogene boundary (KPB) mass extinction event emphasize an abrupt loss of primary productivity at the KPB associated with a severe, long-lasting impact winter caused by sulfate and other stratospheric aerosols produced by the Chicxulub asteroid impact in the Yucatán Peninsula (Junium et al, 2022;Morgan et al, 2022). Although previous paleobotanical investigations emphasized a rather mild KPB impact winter associated with selection for deciduousness or other fast-return leaf economic strategies (Wolfe and Upchurch, 1987;Blonder et al, 2014), this hypothesis lacks critical empirical support in recent investigations (Berry, 2020;Butrim et al, 2022).…”
mentioning
confidence: 99%