SciencePaleogene (~56 million years ago)globalhigh confidence

A transient thermal maximum occurred near the Paleocene-Eocene boundary about 56 million years ago and was associated with a rapid increase in atmospheric carbon dioxide concentrations, possibly caused by massive outgassing and oxidation of methane hydrates from the ocean floor.

Notes on verification

Well-supported by peer-reviewed literature and scientific consensus on the PETM event; the methane hydrate outgassing mechanism is a leading but still debated hypothesis, which the claim appropriately frames as 'possible'. [tier=silver indep_score=0.925 clusters=2 claim_tier=notable]

Sources

A transient thermal maximum occurred near the Paleocene-E… · DeepInquiry