It has long been known that characteristics of the Earth's orbit (its eccentricity, the degree to which it is tilted, and its «wobble») are slightly altered on timescales
of tens to hundreds of thousands of years.
A further reduction by carbonate sediment dissolution, and reactions with igneous rocks, such as silicate weathering and sediment burial, will take anything
from tens to hundreds of thousands of years, or even longer.
The average rate of injection of carbon into the climate system during these hyperthermals was slower than the present human - made injection of fossil fuel carbon, yet it was faster than the time scale for removal of carbon from the surface reservoirs via the weathering process [3], [208], which is
tens to hundreds of thousands of years.
«A lot of these events like the end - Permian and the Triassic - Jurassic, when they're linked to volcanism it does seem that these are relatively slow events overall, on timescales of
tens to hundreds of thousands of years,» says Ridgwell.
The average rate of injection of carbon into the climate system during these hyperthermals was slower than the present human - made injection of fossil fuel carbon, yet it was faster than the time scale for removal of carbon from the surface reservoirs via the weathering process [3], [208], which is
tens to hundreds of thousands of years.
They note that a «considerable fraction of the carbon emitted to date and in the next 100 years will remain in the atmosphere for
tens to hundreds of thousands of years.»