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]
ChristopherRobertScotese
was invoked but never defined (see the help page).MercuryAnomalies
was invoked but never defined (see the help page).TheLateHauterivianFaraoniOceanicAnoxicEvent
was invoked but never defined (see the help page).