Faraoni Thermal Excursion

The Faraoni Thermal Excursion (FTX) was a hyperthermal event that occurred during the Hauterivian stage of the Cretaceous period,[1] being induced by flood basalt volcanism.[2] It is associated with an oceanic anoxic event (OAE).[3]

  1. ^ Cite error: The named reference ChristopherRobertScotese was invoked but never defined (see the help page).
  2. ^ Cite error: The named reference MercuryAnomalies was invoked but never defined (see the help page).
  3. ^ Cite error: The named reference TheLateHauterivianFaraoniOceanicAnoxicEvent was invoked but never defined (see the help page).