Holocene
The Holocène is the geological last time extending on the 10 000 last years. It is frequently subdivided according to Palynozone S
The name is derived from the Greek holos , “entirety (ement)” and ceno , “new”.
A climatic definition
The Holocene one is a Interglaciaire, period hot which follows the last Glaciaire of the Pléistocène (called Weichselien in Northern Europe, Wisconsin in North America or Würm in the Alps). The Holocene one is the fourth and last time of the Néogène, one of many Interglacial of the Quaternaire.
The postglacial transgression
The increase of the level of the Océan S (started at the end of the Glacial with approximately -100 meters with the beginning of the cast iron of the Ice cap of the northern hemisphere) continued, since approximately -35 meters, up to the current level, reached there is approximately 6 000 years. The Black Sea filled approximately 8000 years ago. The Ice caps jointly finish melting and the grounds located below or at the margin of the old ice caps, released from the weight of the ice, go up (Glacio-isostasy). Jointly with the warming, moderate fauna and flora reconquer the averages and high latitudes and the ecosystems of cold climates are isolated in ecological niches.The increase of water allowed a temporary Transgression in the grounds in margins of the Ice caps. Fossile S sailors can be found in the Ontario, the Vermont, the Quebec, the Michigan. In-outside zones of high latitudes where the sea advanced following the glacial depression, one finds this type of fossils in the bed of the lakes, the plains of flood, and the deposits inside the caves.
Internal events with the Holocene one
During Holocene itself, ic changes Climat occurred. The livable zones shifted towards north. The the Sahara was transformed into Désert and of many lakes are now arid extents . That marks also the beginning of the Mesolithic in Archéologie. The continental drift is negligible over one period of also short duration - less than one kilometer. Fauna and the flora did not evolve/move much, but the distribution of the species was modified. A important extinction of the species takes place. The Mégafaune was strongly reduced, thus the équidés and the Chameau X - inter alia - disappeared from North America and that the Mammouth S and tigers with teeth of saber disappeared from the Earth.In Archeology, the Holocene one corresponds to the advent of the Mesolithic , the Neolithic and the later cultures.
See too
Internal bonds
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