Linked from

The 22 pages that link to Paleocene–Eocene Thermal Maximum, each with the reason it gives.

• Ocean acidificationRelated: Its marine carbonate dissolution provides a geological comparison for rapid carbon-driven ocean change.

• PaleoclimatologyBroader topic: Its deposits document a past episode of rapid carbon-driven warming.

• Geologic time scaleRelated: Its sharply recorded signal helps correlate layers within the Cenozoic.

• EoceneBroader topic: This sharp warming event occurred at the Eocene’s beginning and helps explain its climatic baseline.

• PaleogeneBroader topic: It sharply punctuated the Paleogene’s early climate history.

• PaleoclimateBroader topic: Its geological record reveals how Earth systems responded to a large ancient carbon perturbation.

• CenozoicBroader topic: It captures the Cenozoic’s early climate extremes and carbon-cycle disruption.

• PaleogeographyRelated: Its climate and fossil records help test reconstructions of high-latitude land and ocean settings.

• Deccan TrapsCompared with: It provides a later comparison for climate disruption linked to carbon emissions.

• PaleoceneBroader topic: This major warming episode occurred at the epoch’s close.

• PaleoceanographyBroader topic: Marine sediments record its carbon release, warming, ocean acidification, and deep-sea ecosystem disruption.

• Carbonate–silicate cycleBroader topic: The event shows how silicate weathering can gradually draw down carbon after a rapid carbon release.

• Quaternary glaciationCompared with: It offers a deep-time comparison for studying climate responses to rapid carbon release without Quaternary ice sheets.

• Carbon isotope excursionBroader topic: Its prominent negative carbon isotope excursion is a defining geological signal.

• Abrupt climate changeBroader topic: It provides a deep-time case of rapid warming driven by carbon input.

• Grande CoupureCompared with: It offers a contrasting climate-driven faunal disturbance, marked by warming rather than cooling.

• CoryphodonRelated: Coryphodon lived across the boundary near this major climate disturbance.

• MultituberculataRelated: Its environmental changes provide context for mammalian turnovers during multituberculate persistence.

• Methane clathrateBroader topic: Hydrate release has been proposed as one possible contributor to its carbon-cycle disturbance.

• Historical geologyBroader topic: Its sedimentary and isotope records preserve a case of abrupt ancient climate change.

• MegalictisCompared with: It offers a much earlier climate episode, distinct from the Miocene setting of Megalictis.

• TaeniodontaRelated: Its timing overlaps faunal turnover relevant to the later history of taeniodonts.