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The Pre-Boreal began with a sudden rise in temperature that abruptly changed this ecosystem. Forest replaced the open lands in Europe, and forest-dwelling animals spread from southern refugia and replaced the ice-age tundra mammals; new climax ecosystems developed. The old fauna persisted in Central Asia, but were soon hunted out, as they were ...
Pre-Boreal sharp rise in temperature over 50 years (B-S), precedes Boreal 8500–6900: Boreal (B-S), rising sea levels, forest replaces tundra in northern Europe 7500–3900: Neolithic Subpluvial/African humid period in North Africa, wet 7000–3000: Holocene climatic optimum, or Atlantic in northern Europe (B-S) 6200: 8.2-kiloyear event cold ...
End of the pre-Boreal period of European climate change. Pollen Zone IV Pre-boreal, associated with juniper, willow, birch pollen deposits. Neolithic era begins in Ancient Near East. Evidence of the earliest settlement in Jericho; In Antarctica, long-term melting of the Antarctic ice sheets is commencing.
The Preboreal is an informal stage of the Holocene epoch. It is preceded by the Tarantian and succeeded by the Boreal . It lasted from 10,300 to 9,000 BP in radiocarbon years or 8350 BC to 7050 BC in Gregorian calendar years ( 8th millennium BC ).
The Younger Dryas (YD, Greenland Stadial GS-1) [2] was a period in Earth's geologic history that occurred circa 12,900 to 11,700 years Before Present (BP). [3] It is primarily known for the sudden or "abrupt" cooling in the Northern Hemisphere, when the North Atlantic Ocean cooled and annual air temperatures decreased by ~3 °C (5.4 °F) over North America, 2–6 °C (3.6–10.8 °F) in Europe ...
The pre-Boreal period was followed by the Boreal period, which began around 7,500 BC and saw a much warmer and drier climate. Accordingly, the composition of the wildwood began to change with the arrival from continental Europe of tree species that were able to thrive in the new conditions.