Reconstruction of the Dead (Grey) Dune evolution along the Curonian Spit, Southeastern Baltic

被引:18
|
作者
Dobrotin, Nikita [1 ]
Bitinas, Albertas [2 ]
Michelevicius, Dainius [3 ]
Damusyte, Aldona [4 ]
Mazeika, Jonas [5 ]
机构
[1] Klaipeda Univ, Coastal Res & Planning Inst, LT-92294 Klaipeda, Lithuania
[2] Klaipeda Univ, Coastal Res & Planning Inst, Dept Geophys Sci, LT-92294 Klaipeda, Lithuania
[3] Vilnius State Univ, Fac Nat Sci, LT-03100 Vilnius, Lithuania
[4] Lithuanian Geol Survey, LT-03123 Vilnius, Lithuania
[5] Nat Res Ctr, Inst Geol & Geog, LT-03223 Vilnius, Lithuania
关键词
ground-penetrating radar; paleosols; artifacts; absolute age; C-14; paleogeography; Holocene; Curonian Spit; Lithuania; CALIBRATION; RIDGE;
D O I
10.17741/bgsf/85.1.004
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
One of the unique places in Europe in both environmental and cultural terms is the Curonian Spit - a massive sandy barrier separating the Curonian Lagoon from the Baltic Sea. Straddling both the Lithuanian and the Russian parts, the spit is included into the UNESCO list of cultural heritage monuments. From the geological point of view, it is still an "alive" environment dominated by aeolian deposits. With the help of modern geophysical and geochronological techniques (ground-penetrating radar [GPR] surveys, LIDAR data, and radiocarbon [C-14] dating), detailed investigations of paleosois were carried out in the Dead (Grey) Dunes massif located between Juodkrante and Pervalka settlements on the Lithuanian half of the Curonian Spit. Several soil-forming generations (phases) during 5800-4500, 3900-3100, 2600-2400, and from 1900 calendar years BP until the present have been distinguished. GPR surveys enabled a series of paleogeographic reconstructions of the massif for different time intervals of its evolutionary history.
引用
收藏
页码:53 / 64
页数:12
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