Matches in DBpedia 2016-04 for { ?s ?p "The Allerød oscillation (Danish: Allerødtiden) was a warm and moist global interstadial that occurred at the end of the last glacial period. It raised temperatures in the northern Atlantic region to almost present-day levels, before they declined again in the succeeding Younger Dryas period, which was followed by the present interglacial period.In some regions, especially in northern Eurasia, there is evidence for a cold period known as the Older Dryas interrupting the interstadial. In such regions the shorter oscillation ending with the Older Dryas is known as the Bølling oscillation, and the Allerød period is the interstadial following the Older Dryas.The Allerød period was named after a type site in Furesø municipality in Sjælland, Denmark (near Copenhagen), where deposits created during the period were first identified in work published in 1901 by Hartz and Milthers. This Blytt-Sernander period corresponds to Pollen zone II."@en }
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- Allerød_oscillation abstract "The Allerød oscillation (Danish: Allerødtiden) was a warm and moist global interstadial that occurred at the end of the last glacial period. It raised temperatures in the northern Atlantic region to almost present-day levels, before they declined again in the succeeding Younger Dryas period, which was followed by the present interglacial period.In some regions, especially in northern Eurasia, there is evidence for a cold period known as the Older Dryas interrupting the interstadial. In such regions the shorter oscillation ending with the Older Dryas is known as the Bølling oscillation, and the Allerød period is the interstadial following the Older Dryas.The Allerød period was named after a type site in Furesø municipality in Sjælland, Denmark (near Copenhagen), where deposits created during the period were first identified in work published in 1901 by Hartz and Milthers. This Blytt-Sernander period corresponds to Pollen zone II.".
- Q1418589 abstract "The Allerød oscillation (Danish: Allerødtiden) was a warm and moist global interstadial that occurred at the end of the last glacial period. It raised temperatures in the northern Atlantic region to almost present-day levels, before they declined again in the succeeding Younger Dryas period, which was followed by the present interglacial period.In some regions, especially in northern Eurasia, there is evidence for a cold period known as the Older Dryas interrupting the interstadial. In such regions the shorter oscillation ending with the Older Dryas is known as the Bølling oscillation, and the Allerød period is the interstadial following the Older Dryas.The Allerød period was named after a type site in Furesø municipality in Sjælland, Denmark (near Copenhagen), where deposits created during the period were first identified in work published in 1901 by Hartz and Milthers. This Blytt-Sernander period corresponds to Pollen zone II.".