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Holocene$35561$ - translation to italian
![Vegetation and water bodies in northern and central Africa in the [[Eemian]] (bottom) and [[Holocene]] (top)](https://commons.wikimedia.org/wiki/Special:FilePath/Journal.pone.0076514.g004.png?width=200 "Vegetation and water bodies in northern and central Africa in the [[Eemian]] (bottom) and [[Holocene]] (top)")
Definition
Wikipedia
The Holocene Climate Optimum (HCO) was a warm period that occurred in the interval roughly 9,500 to 5,500 years ago BP, with a thermal maximum around 8000 years BP. It has also been known by many other names, such as Altithermal, Climatic Optimum, Holocene Megathermal, Holocene Optimum, Holocene Thermal Maximum, Hypsithermal, and Mid-Holocene Warm Period.
The warm period was followed by a gradual decline, of about 0.1 to 0.3 °C per millennium, until about two centuries ago (when this trend was rapidly reversed due to human-produced greenhouse gas emissions). However, on a sub-millennial scale, there were regional warm periods superimposed on this decline.
- For other temperature fluctuations, see temperature record.
- For other past climate fluctuation, see paleoclimatology.
- For the pollen zone and Blytt–Sernander period, associated with the climate optimum, see Atlantic (period).
