|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. hdl.handle.net/10.1038/ngeo2430
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894, more
|Authors|| || Top |
- Alexander, K.
- Meissner, K.J.
- Bralower, T.J.
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