Late Glacial and Holocene Vegetation Changes in the Wigry National Park, NE Poland – New Pollen Data from Three Small Dystrophic Lakes

IF 0.6 Q4 GEOSCIENCES, MULTIDISCIPLINARY
M. Fiłoc, M. Kupryjanowicz, D. Drzymulska
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引用次数: 7

Abstract

Abstract The main phases of the Late Glacial and Holocene development of vegetation in the Wigry National Park were reconstructed based on the pollen analysis of sediments from three small dystrophic lakes (Lake Suchar Wielki, Lake Suchar II and Lake Ślepe). At the current stage of research, the age of the studied deposits was determined by AMS radiocarbon dating of few samples only. This meant that the chronology of the investigated sections had to be estimated also indirectly using their palynological correlation with the radiometrically well-dated section from Lake Wigry. The obtained pollen data confirmed the picture of the postglacial vegetation changes of the Wigry National Park, which was based on earlier studies of Lake Wigry. Furthermore, it documented the existence, mainly in the Preboreal and Atlantic chronozones, of temporary changes in vegetation, which might be a reaction to a short-lived cold fluctuations of climate.
波兰东北部威格里国家公园晚冰期和全新世植被变化——来自三个小营养不良湖泊的新花粉数据
摘要通过对威格里国家公园(Wigry National Park) 3个小型营养不良湖泊(Suchar Wielki湖、Suchar II湖和Ślepe湖)沉积物的花粉分析,重建了该地区晚冰期和全新世植被发育的主要阶段。在目前的研究阶段,所研究沉积物的年龄仅通过AMS放射性碳定年法对少数样品进行测定。这意味着研究剖面的年代学也必须通过孢粉学与威格里湖放射学上确定年代的剖面的对比来间接估计。获得的花粉数据证实了威格里国家公园冰川后植被变化的图像,这是基于对威格里湖的早期研究。此外,它还记录了主要在前寒带和大西洋时间带存在的植被的暂时变化,这可能是对短暂的寒冷气候波动的反应。
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来源期刊
Studia Quaternaria
Studia Quaternaria GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
自引率
0.00%
发文量
0
期刊介绍: Studia Quaternaria is designed to publish scientific works concerning the Quaternary, on local, regional and global scale. Studia Quaternaria is interested in all fields of research dealing with stratigraphy and reconstruction of the past environments, including palaeogeography, palaeoecology, palaeoclimatology, palaeohydrology etc. The journal is also open to studies of natural environmental processes, and to recognition of mechanisms involved in the dynamics of our environment. The clue is that the Quaternary is still ongoing and vivid, and understanding of its past and present development support each other.
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