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/content/papers/10.3997/2214-4609.202333220
2023-09-10
2026-01-20
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References

  1. Alvarez, L.W., et al.Extraterrestrial cause for the Cretaceous-Tertiary extinction.Science208, 1095–1108 (1980).
    [Google Scholar]
  2. Barnet, J.S.K., et al.A high‐fidelity benthic stable isotope record of late Cretaceous-early Eocene climate change and carbon‐cycling.Paleoceanography and Paleoclimatology34, 672–691 (2019).
    [Google Scholar]
  3. Clyde, W.C., et al.Direct high-precision U-Pb geochronology of the end-Cretaceous extinction and calibration of Paleocene astronomical timescales.Earth and Planetary Science Letters452, 272–280 (2016).
    [Google Scholar]
  4. Hughes, P. D., et al.The impact of high tephra loading on late-Holocene carbon accumulation and vegetation succession in peatland communities.Quaternary Science Reviews67, 160–175 (2013).
    [Google Scholar]
  5. Hull, P. M., et al.On impact and volcanism across the Cretaceous-Paleogene boundary.Science367, 266–272 (2020).
    [Google Scholar]
  6. Naafs, B.D.A., et al.Introducing global peat-specific temperature and pH calibrations based on brGDGT bacterial lipids.Geochimica et Cosmochimica Acta208, 285–301 (2017).
    [Google Scholar]
  7. O’Connor, L.K. & Crampton-Flood, E.D., et al.Steady decline in mean annual air temperatures in the first 30 ka after the Cretaceous-Paleogene boundary.Geology (in press).
    [Google Scholar]
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