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DOIhttps://doi.org/10.1594/PANGAEA.763935
Tab. 1: Age of biogene material from the ice margin, Kofoed-Hansen Bræ and Storstrømmen
Weidick; Anker; Andreasen; Claus; Oerter; Hans; Reeh; Niels
发布日期2011-08-17
数据集类型dataset
英文简介Early Holocene recession of the ice cover over Germania Land in North-East Greenland 7.5 ka B.P. brought the Inland Ice margin back to a position close to the present. Continued recession after that time lead to the formation of a "Storstrømmen Sound" which separated Germania Land from mainland Greenland in the period from about 6 to 1 ka B.P. The present filling of the approximately 100 km long sound by the glaciers of Storstrømmen and Kofoed-Hansen Bræ must therefore have taken place during the Little lce Age. In an archaeological sense this implies deterioration of the living conditions of Neo-Eskimos compared to those of Palaeo-Eskimos.
空间范围Median Latitude: 77.153412 * Median Longitude: -21.955353 * South-bound Latitude: 77.079000 * West-bound Longitude: -21.995000 * North-bound Latitude: 77.235000 * East-bound Longitude: -21.868000
语种英语
国家国际
学科大类气候变化
学科子类冰冻圈
文献类型数据集
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/213814
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GB/T 7714
Weidick,Anker,Andreasen,et al. Tab. 1: Age of biogene material from the ice margin, Kofoed-Hansen Bræ and Storstrømmen.2011-08-17.https://doi.org/10.1594/PANGAEA.763935.
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