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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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MICHAEL ALLABY. "Bølling interstadial." A Dictionary of Ecology. 2004. Encyclopedia.com. 28 May. 2012 <http://www.encyclopedia.com>. MICHAEL ALLABY. "Bølling interstadial." A Dictionary of Ecology. 2004. Encyclopedia.com. (May 28, 2012). http://www.encyclopedia.com/doc/1O14-Bllinginterstadial.html MICHAEL ALLABY. "Bølling interstadial." A Dictionary of Ecology. 2004. Retrieved May 28, 2012 from Encyclopedia.com: http://www.encyclopedia.com/doc/1O14-Bllinginterstadial.html |
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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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Cite this article
MICHAEL ALLABY. "Bølling interstadial." A Dictionary of Plant Sciences. 1998. Encyclopedia.com. 28 May. 2012 <http://www.encyclopedia.com>. MICHAEL ALLABY. "Bølling interstadial." A Dictionary of Plant Sciences. 1998. Encyclopedia.com. (May 28, 2012). http://www.encyclopedia.com/doc/1O7-Bllinginterstadial.html MICHAEL ALLABY. "Bølling interstadial." A Dictionary of Plant Sciences. 1998. Retrieved May 28, 2012 from Encyclopedia.com: http://www.encyclopedia.com/doc/1O7-Bllinginterstadial.html |
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