They are
called hyperthermals - periods of intense and sudden rises in temperature, lasting tens of thousands of years.
The discovery of other, smaller magnitude, rapid greenhouse warming events (
called hyperthermals) in the millions of years following the PETM provides further opportunities to examine the response of organisms to global climate change.
Not exact matches
These so -
called «modest
hyperthermals» (meaning a rapid, pronounced period of global warming) had shorter durations and recoveries (about a 40,000 year cycle) and involved an exchange of carbon between surface reservoirs into the atmosphere and then into sediment.