Allerød oscillation
 | This article needs additional citations for verification. (April 2011) |
| Allerød | |
|---|---|
| Usage information | |
| Celestial body | Earth |
| Regional usage | Regional |
| Definition | |
| Chronological unit | Chron |
| Stratigraphic unit | Chronozone |
The Allerød oscillation (Template:Lang-da) was a warm and moist global interstadial that occurred c.13,900 to 12,900 BP,[1] nearly 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 glacial Younger Dryas, which was followed by the present warm Holocene.
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.
Dating
The start of the Allerød depends on whether an Older Dryas is present and how much time is to be allotted to the latter. A conventional date of 14,000 BP is typical. Roberts (1998) uses 13,000 BP for the end of the period.
The Greenland oxygen isotope record shows the warming identified with the Allerød to be after about 14,100 BP and before about 12,900 BP. C-14 dates from an excavation on the shore of Lake Neuchatel, Switzerland, furnish a date of 14,000 BP, calibrated, for the start of the Allerød. Pollen cores from Berezina plain, Belarus, give 11,800–10,900 BP uncal. Various researchers have similar ranges: 12,000–11,000, 11,700–11,000, etc. They all seem to roughly concur. The interstadial ended abruptly with a cold period that reduced temperatures back to near-glacial levels within a decade.[2]
The Allerød occurred during the last interstadial of the Pleistocene: the Windermere of Britain, the Woodgrange of Ireland and the Two Creeks Interval of North America. Although interstadials are defined by region, the Allerød period is not, being global in its effects; that is, the temperature and sea level rose everywhere, not just in north Europe.
Flora
During the Allerød, which foreshadowed the modern climate, mixed evergreen and deciduous forests prevailed in Eurasia, more deciduous toward the south, just as today. Birch, aspen, spruce, pine, larch and juniper were to be found extensively, mixed with oak and hazel. Grasses were to be found in more open regions.
Fauna
Some animals hunted were the red deer, moose, horse, Irish elk and beaver. The ubiquitous brown bear was present as well.
Humans
Humans in north Eurasia were still in the hunting-gathering stage. A variety of Palaeolithic cultures prevailed in Europe: the Federmesser, Lyngby, Bromme, Ahrensburg and Swiderian. In the Levant, early alcohol use may have occurred during this time. [3]
Sources
- ^ Ashton, Nick (2017). Early Humans. London: William Collins. p. 313. ISBN 978-0-00-815035-8.
- ^ Wade, Nicholas, "Before the Dawn", Penguin Press, 2006. pp. 123
- ^ Liu, Li; Wang, Jiajing; Rosenberg, Danny; Zhao, Hao; Lengyel, György; Nadel, Dani (October 2018). "Fermented beverage and food storage in 13,000 y-old stone mortars at Raqefet Cave, Israel: Investigating Natufian ritual feasting". Journal of Archaeological Science: Reports. 21: 783–793. doi:10.1016/j.jasrep.2018.08.008.