Non-Pollen Palynomorphs Characteristic for the Dystrophic Stage of Humic Lakes in the Wigry National Park, Ne Poland

IF 0.6 Q4 GEOSCIENCES, MULTIDISCIPLINARY Studia Quaternaria Pub Date : 2015-06-01 DOI:10.1515/squa-2015-0003
M. Fiłoc, M. Kupryjanowicz
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引用次数: 6

Abstract

Abstract The numerous dystrophic (humic) lakes are a very important feature of Wigry National Park, NE Poland. As the most recent palaeoecological data indicate, at the beginning of its development (in the Late Glacial and Early and Middle Holocene) these water bodies functioned as harmonious lakes, and their transformation into dystrophic lakes and the stabilization of the trophic state took place at the beginning of the Subboreal. Palynological analysis of sediments from two such lakes (Lake Ślepe and Lake Suchar II), with special emphasis on non-pollen palynomorphs (NPPs), was aimed at a detailed biological characterization of dystrophic lakes during their long-lasting existence. The obtained results allowed for the designation of organisms characteristic for dystrophic lakes, of which representatives appeared with the decreasing pH of the water and the formation of Sphagnum peat around lakes. These organisms were divided into four groups: algae, fungi, testate amoebas, and animals. Their representatives appear invarious developmental stages of dystrophic lakes.
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波兰威格里国家公园腐殖质湖泊营养不良阶段的非花粉孢谱特征
波兰东北部威格里国家公园众多的营养不良(腐殖质)湖泊是一个非常重要的特征。最新的古生态资料表明,这些水体在其发育初期(晚冰期和全新世早中期)为和谐湖泊,在亚北纬期开始向营养不良湖泊转变,营养状态趋于稳定。通过对两个营养不良湖泊(Ślepe湖和Suchar II湖)沉积物的孢粉学分析,重点分析了非花粉孢粉形态(NPPs),旨在详细了解营养不良湖泊长期存在的生物学特征。所得结果可用于指定营养不良湖泊的特征生物,其代表性生物出现在水体pH值下降和湖泊周围泥炭的形成。这些生物被分为四组:藻类、真菌、睾丸变形虫和动物。它们的代表是营养不良湖泊发育的各个阶段。
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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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