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the Allerød clay pit in Denmark, first recognized and described the Younger Dryas.
Within the Blytt-Sernander classification of north European climatic phases, the prefix ‘Younger’ refers to the recognition that this original ‘Dryas’ period was preceded by a warmer stage, the Allerød oscillation, which in turn was preceded by the Older Dryas around 14,000 calendar years BP.
They argue that Younger Dryas events might be an intrinsic feature of deglaciations that occur at the end of glacial periods.The application of alkenone paleothermometers to high-resolution paleotemperature reconstructions of older glacial terminations have found that very similar Younger Dryas-like paleoclimatic oscillations occurred during Terminations II and IV. singl börse Saale If so, then the Younger Dryas is not the unique paleoclimatic event, in terms of size, extent, and rapidity, as it has been often regarded to be.The Younger Dryas was a period of climatic change, but the effects were complex and variable.In the southern hemisphere, and some areas of the north such as southeastern North America, there was a slight warming.
Both of these cold periods are comparable in duration and intensity with the Older Dyras and began and ended quite abruptly.These cold periods have been recognized in sequence and relative magnitude in paleoclimatic records from Greenland ice cores, European lacustrine sediments, Atlantic Ocean sediments, and the Cariaco Basin, Venezuela. Temperature-sensitive lipids, long chain alkenones, found in lake and marine sediments are well-regarded as a powerful paleothermometer for the quantitative reconstruction of past continental climates.In addition to the Younger, Older, and Oldest dryases, a century-long period of colder climate similar to the Younger Dryas in abruptness has occurred within both the Bølling oscillation and the Allerød oscillation interstadials.The cold period, which occurred within the Bølling oscillation, is known as the intra-Bølling cold period (ICBP) and the cold period, which occurred within the Allerød oscillation, is known as the intra-Allerød cold period (ICAP ). Leaves of Dryas octopetala are occasionally abundant in the Late Glacial, often minerogenic-rich, like the lake sediments of Scandinavian lakes.
It is named after an indicator genus, the alpine-tundra wildflower Dryas octopetala.HP is committed to working with and providing reasonable accommodation to qualified individuals with physical and mental disabilities.If you need assistance in filling out the employment application or require a reasonable accommodation while seeking employment, please e-mail [email protected] is not securely dated, and estimates vary by 400 years, but it is generally accepted that it lasted around 200 years.In northern Scotland the glaciers were thicker and more extensive than during the Younger Dryas.