While the evidence for catastrophic leakage is still equivocal, the amounts of methane stored in permafrost and
ocean sediments strongly argue for a precautionary approach to the risks of widespread release.
[15] Through study of Pacific
Ocean sediments, other researchers have shown that the transition from warm Eocene ocean temperatures to cool Oligocene ocean temperatures took only 300,000 years, [11] which strongly implies that feedbacks and factors other than the ACC were integral to the rapid coo
Ocean sediments, other researchers have shown that the transition from warm Eocene
ocean temperatures to cool Oligocene ocean temperatures took only 300,000 years, [11] which strongly implies that feedbacks and factors other than the ACC were integral to the rapid coo
ocean temperatures to cool Oligocene
ocean temperatures took only 300,000 years, [11] which strongly implies that feedbacks and factors other than the ACC were integral to the rapid coo
ocean temperatures took only 300,000 years, [11] which
strongly implies that feedbacks and factors other than the ACC were integral to the rapid cooling.