KnowraPaleocene–Eocene Thermal MaximumLinked fromLinked fromThe 22 pages that link to Paleocene–Eocene Thermal Maximum, each with the reason it gives.All 22Broader topic 12Related 6Compared with 4PaleoclimatologyBroader topic: Its deposits document a past episode of rapid carbon-driven warming.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.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.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.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.