Multiple studies support the mechanism that deep ocean warming during the Paleocene-Eocene Thermal Maximum (PETM) triggered the dissociation of methane clathrates, releasing massive amounts of carbon into the ocean and atmosphere.
The provided literature consistently supports the claim that methane clathrate (hydrate) release during the PETM was triggered by warming. Papers [0], [1], [3], and [7] specifically link the thermal feedback, initial ocean warming, or isotopic signatures directly to methane hydrate dissociation as a primary carbon source or amplification mechanism during the PETM. None of the provided papers refute this mechanism. Therefore, the verdict is SUPPORTED.