Climate Change Data Portal
DOI | https://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 |
推荐引用方式 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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