格里尔凸起沼泽沉积物记录的奥拉瓦—北塔格盆地晚冰期—全新世古环境变化

GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series Pub Date : 2016-01-01 DOI:10.4316/GEOREVIEW.2016.0.0.338

D. Michczyńska, W. Margielewski

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引用次数: 2

摘要

Grel凸起的泥炭沼泽位于Orawa-Nowy Targ盆地的Ludźmierz村庄附近。这个凸起的沼泽，泥炭圆顶严重退化，上面覆盖着许多挖掘后的坑，这些坑是为当地目的提取泥炭的结果。泥炭沼泽长满了桦树和松林以及典型的沼泽植被。Koperowa(1962)首次对泥炭沉积序列进行了孢粉学研究。泥炭沼泽形成的开始被认为是最古老的仙女木期。因此，Grel是奥拉瓦-诺伊塔格盆地泥炭地中最古老的泥炭沼泽

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Palaeoenvironmental changes of Orawa-Nowy Targ Basin in the Late Glacial and Holocene recorded in sediments of Grel raised bog

The Grel raised peat bog is located in the Ludźmierz village vicinity in the Orawa-Nowy Targ Basin. This raised bog, has heavily degraded peat dome covered with numerous post excavation pits which are the results of peat extraction for local purposes. Peat bog is overgrown with birch and pine forests and typical vegetation for raised bog. First palynological study of the peat depositional sequence was performed by Koperowa (1962). The beginning of the peat bog formation was then attributed to the Oldest Dryas. Consequently the Grel is the oldest peat bog in the peatland of the Orawa-Nowy Targ Basin

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GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series

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6 weeks