Publicaties | Instituten | Personen | Datasets | Projecten | Kaarten
[ meld een fout in dit record ]mandje (0): toevoegen | toon Print deze pagina
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, meer
Peer reviewed article  
Beschikbaar in  Auteurs 
Trefwoord
    Marien/Kust
Auteurs  Top 
  • 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.
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.
Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid Top | Auteurs