An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal Maximum
Penman, D.E.; Turner, S.K.; Sexton, P.F.; Norris, R.D.; Dickson, A.J.; Boulila, S.; Ridgwell, A.J.; Zeebe, R.E.; Zachos, J.C.; Cameron, A.; Westerhold, T.; Röhl, U. (2016). An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal Maximum. Nature Geoscience 9(8): 575-580. http://dx.doi.org/10.1038/ngeo2757
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, more
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| Authors | | Top |
- Penman, D.E.
- Turner, S.K.
- Sexton, P.F.
- Norris, R.D.
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- Dickson, A.J.
- Boulila, S.
- Ridgwell, A.J.
- Zeebe, R.E.
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- Zachos, J.C.
- Cameron, A.
- Westerhold, T.
- Röhl, U.
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| Abstract |
The Palaeocene–Eocene Thermal Maximum was associated with a massive release of carbon. Marine sediments suggest a temporary deepening of the calcite compensation depth, indicating extensive silicate weatheringin the aftermath of the event. |
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