Not exact matches
Instead, the fossil record indicates they vanished during the Earth's
glacial - interglacial transition, which occurred about 12,000 years ago and led to much warmer conditions and the
start of the current Holocene
period.
The MIS 5a palaeosol is overlain by massive sands, representing a major change in the depositional regime, which we interpret as evidence for climatic desiccation at the
start of the last
glacial period (MIS 4), which would be consistent with other dated records for the region [13], [16], [18], [30].
It is very unlikely that the Milankovitch cycles can
start or end an ice age (series
of glacial periods):
There is a new
glacial period every approximately 11,500 years after the
start of an interglacial
period.
What is known is that during the
period called Little Ice Age, global
glacial were advancing, and
starting around 1850, instead advancing global glacier became retreating, this trend
of glacial retreat continues to the present time, but not all glaciers adding during the Little Ice Age have not yet melted.
Kent points out that according to the Milankovitch theory, we should be at the peak
of a 20,000 - some year warming trend that ended the last
glacial period; the Earth may eventually
start cooling again over thousands
of years, and possibly head for another glaciation.
Similarly, in a study
of air temperature and CO2 data obtained from Dome Concordia, Antarctica for the
period 22,000 - 9,000 BP — which time interval includes the most recent
glacial - to - interglacial transition — Monnin et al. (2001) found that the
start of the CO2 increase lagged the
start of the temperature increase by 800 years.
However I have found another with a CO2 level in the range we have experienced since the 1940's http://www.pnas.org/content/99/20/12567.full At 379 ppm within 35 ppm, the
start of the Namurian
period, 330 million years ago, should be deep in an
glacial period if CO2 was the answer to the faint sun paradox.
This also explains the shape
of the historical global temperature plots (straight up to
start an interglacial, but then following natural cooling curve downwards over much longer
periods back to
glacial equilibrium).