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.
This was
during glacial periods suggesting they were well adapted to these harsh
conditions.
The sequence of climatic forcings and responses
during deglaciations (transitions from full
glacial conditions to warm interglacials) are well documented.
The current secondary contact is thought to result from a range expansion associated with the amelioration of climatic
conditions after the last
glacial maximum (∼ 18000 ya)[20], although previous
glacial / interglacial cycles
during the Pleistocene may have provided multiple opportunities for vicariant and past hybridization events.
Based on previous studies it was assumed that the entire region was much drier
during the Last
Glacial Maximum compared to present
conditions, «Niedermeyer concludes.
During the last part of the Pleistocene there were actually five major periods of glaciation with four periods of warmer non
glacial conditions between them.
The diversification events influencing island and mainland gray foxes closely correspond to climatic fluctuations, particularly the shift from fully
glacial to non-
glacial conditions during the past 20,000 years.
Aren't the neo-
glacial readvances and other signs of a cooling climate
during the past 3,000 years evidence of a gradual return to
glacial conditions (prior to the anthropogenic influence brought on by the industrial revolution)?
During glacial states near permanent El Nino
conditions exist.
Carbon starvation, which apparently sometimes occurs
during glacial periods due to the low levels of CO2 that are reached, has the same effect on C3 plants * trees, shrubs, and such) as do warm, dry
conditions when the warm is excesaive.
Müller, C. Reconstruction of the paleontological
conditions at the Laptev Sea continental margin
during the last two
glacial / interglacial cycles based on sedimentological and mineralogical investigations.
This type of behavior is especially evident
during transitions from
glacial to interglacial
conditions, when climate is affected by a wide variety of time - varying influences and is relatively unstable.
each period of warming
during the descent to the next
glacial stage should be more intense than the previous ones, as climatic variability increases outside the warm
conditions of an interglacial climatic optimum.
We know that
during the LIA sea - ice reached Scotland in the winter, so it is very counter-intuitive that under much colder
glacial conditions sea ice would actually be reduced.
Other processes must be responsible for the 40 - to 50 - ppm pCO2 drawdown
during the initial transition from interglacial to
glacial conditions as well as for a comparable pCO2 increase
during the latter part of
glacial terminatins.