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Bølling interstadial

Bølling interstadial A relatively warm period that occurred towards the end of the last (Devensian) glaciation in north-western Europe, and which is named after the type site in Denmark. The event took place about 13 000–12 000 radiocarbon years bp. In Britain, the Bølling is not usually distinguished from the Allerød. See also Dryas.

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"Bølling interstadial." A Dictionary of Ecology. . Encyclopedia.com. 20 Aug. 2017 <http://www.encyclopedia.com>.

"Bølling interstadial." A Dictionary of Ecology. . Encyclopedia.com. (August 20, 2017). http://www.encyclopedia.com/science/dictionaries-thesauruses-pictures-and-press-releases/bolling-interstadial

"Bølling interstadial." A Dictionary of Ecology. . Retrieved August 20, 2017 from Encyclopedia.com: http://www.encyclopedia.com/science/dictionaries-thesauruses-pictures-and-press-releases/bolling-interstadial

Bølling interstadial

Bølling interstadial A relatively warm period that occurred towards the end of the last (Weichselian) glaciation in north-western Europe, and which is named after the type site in Denmark. The event took place about 13000–12000 radiocarbon years BP.

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"Bølling interstadial." A Dictionary of Plant Sciences. . Encyclopedia.com. 20 Aug. 2017 <http://www.encyclopedia.com>.

"Bølling interstadial." A Dictionary of Plant Sciences. . Encyclopedia.com. (August 20, 2017). http://www.encyclopedia.com/science/dictionaries-thesauruses-pictures-and-press-releases/bolling-interstadial-0

"Bølling interstadial." A Dictionary of Plant Sciences. . Retrieved August 20, 2017 from Encyclopedia.com: http://www.encyclopedia.com/science/dictionaries-thesauruses-pictures-and-press-releases/bolling-interstadial-0