Atlantic period

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The Atlantic in palaeoclimatology was the warmest and moistest Blytt–Sernander period, pollen zone and chronozone of Holocene northern Europe. The climate was generally warmer than today. It was preceded by the Boreal, with a climate similar to today's, and was followed by the Subboreal, a transition to the modern.

Excerpt from the Wikipedia article “Atlantic period”, under the CC BY-SA 4.0 license. Read the article on Wikipedia

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