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Sudden spreading of corrosive bottom water during the Palaeocene–Eocene Thermal Maximum
Alexander, K.; Meissner, K.J.; Bralower, T.J. (2015). Sudden spreading of corrosive bottom water during the Palaeocene–Eocene Thermal Maximum. Nature Geoscience 8(6): 458–461. http://dx.doi.org/10.1038/ngeo2430
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, more
Peer reviewed article  

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Keyword
    Marine/Coastal

Authors  Top 
  • Alexander, K.
  • Meissner, K.J.
  • Bralower, T.J.

Abstract
    The Palaeocene–Eocene Thermal Maximum was associated with warming and seafloor carbonate dissolution. Numerical simulations suggest that the spread of deep corrosive water from the North Atlantic can explain the observed dissolution patterns

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