[Response: Turns out that hydrate preservation is much more sensitive to changes in temperature than it is changes in pressure, so what we might look for is release of
methane during deglaciation.
Not exact matches
In a study released this fall, Petrenko analyzed
methane from 12,000 years ago
during the last
deglaciation, when Earth was transitioning out of the last ice age.
The sharpest
methane concentration increases occur
during deglaciations, in phase with Greenland (NH) temperature and monsoon intensity increases.
The data rule out
methane hydrates as a major contributor to (i) glacial - interglacial variations
during the last
deglaciation, and (ii) millennial
methane increases that occur in phase with Greenland temperature abrupt events.
Light gray bars denote
deglaciations (terminations), while the two dark gray bars denote the Younger Dryas and the Younger Dryas - like event
during termination III (i.e., decreased atmospheric
methane and East Asian Monsoon (higher δ18O).
If the probability of the coming
methane bomb was reasonable, I would think many of these events would have happened
during deglaciations.
However, high - resolution proxy records sensitive to AMOC strength (Chinese speleothem δ18O and atmospheric
methane) document a Younger Dryas — like event
during termination III (the third to the last
deglaciation)(Figs. 2B and 2C; Carlson, 2008; Cheng et al., 2009).