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.
Researchers at the Laboratoire Ecologie des Systèmes Marins Côtiers (CNRS / IRD / Universités Montpellier 1 and 2 / IFREMER) and the Laboratoire CoRéUs 2 (IRD) have shown that the
current distribution of tropical marine biodiversity is mainly due to the persistence of such refugia
during glacial periods in the Quaternary.
The results, which include information
during the last
glacial and interglacial
periods, showed that relief from the
current dry spell across the interior of the Middle East is unlikely within the next 10,000 years.
At this early stage of knowledge, what was being studied were the
glacial periods within the past few hundred thousand years,
during the
current ice age.
[2] The only
current ice sheets are in Antarctica and Greenland;
during the last
glacial period at Last Glacial Maximum (LGM) the Laurentide ice sheet covered much of North America, the Weichselian ice sheet covered northern Europe and the Patagonian Ice Sheet covered southern South A
glacial period at Last
Glacial Maximum (LGM) the Laurentide ice sheet covered much of North America, the Weichselian ice sheet covered northern Europe and the Patagonian Ice Sheet covered southern South A
Glacial Maximum (LGM) the Laurentide ice sheet covered much of North America, the Weichselian ice sheet covered northern Europe and the Patagonian Ice Sheet covered southern South America.
For example, atmospheric carbon dioxide grew by approximately 30 %
during the transition from the most recent cold
glacial period, about 20,000 years ago, to the
current warm interglacial
period; the corresponding rate of decrease in surface ocean pH, driven by geological processes, was approximately 50 times slower than the
current rate driven largely by fossil fuel burning.
The emergence of civilization
during our
current interglacial, the Holocene, has been attributed to the «relative climate quiescence» of this
period relative to the massive, abrupt shifts in climate that characterized
glacial periods in the form of D - O events.»