Vegetation and Stratigraphic Interpretation of the Mazovian (Holsteinian) Interglacial Profile from Dobropol and other New Sites in the West Polesie Region (SE Poland)

IF 0.6 Q4 GEOSCIENCES, MULTIDISCIPLINARY
A. Hrynowiecka, M. Żarski, H. Winter
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引用次数: 3

Abstract

Abstract Geological mapping in eastern Poland resulted in the new find of organic deposits near Włodawa. Pollen and plant macrofossils analyses at the Dobropol site proved deposition during the Mazovian (Holsteinian) Interglacial (MIS 11). Pollen spectra indicated strong predominance of Carpinus in the optimum phase (pollen period III), suggesting intensive influence of continental climate in this part of Po land. The paleolake Dobropol was shallow, with many species of rushes in a littoral zone. During the Liviecian (MIS 10) and the Krznanian (MIS 8) Glaciations the reservoir was occupied by an ice-dam lake, in which silt and clay de position prevailed. The Mazovian Interglacial organic deposits were also recorded in immediate surroundings of the study area. Based on geological and paleobotanical examination of the Dobropol site, the ice sheet of the Krznanian Glaciation seemed to have reached at least the southern part of Włodawa. The ice sheet has not covered pre sum ably the whole study area as its advance occurred in several lobes. The surroundings of Włodawa in the West Polesie Region are the third largest Mazovian paleo-lakeland area in Po land, apart from the vicinities of Biała Podlaska and the Łuków Plain.
波兰西部多布罗波尔等新址马佐夫世(荷尔斯泰因世)间冰期剖面的植被和地层解释
在波兰东部的地质填图中,在Włodawa附近发现了新的有机矿床。在多布罗波尔遗址进行的花粉和植物大化石分析证实了在马佐夫世(荷斯泰因世)间冰期(MIS 11)沉积。花粉谱显示,在最佳花粉期(花粉期III),石竹属占优势,表明该地区受大陆性气候影响较大。古多布罗波尔湖很浅,沿岸有许多种类的灯心草。在李维纪(MIS 10)和克拉兹尼亚纪(MIS 8)冰期,水库被一个冰坝湖泊所占据,其中泥沙和粘土沉积为主。研究区周边还发现了马佐夫系间冰期有机质沉积。根据对多布罗波尔遗址的地质和古植物学研究,Krznanian冰期的冰盖似乎至少到达了Włodawa的南部。冰盖可能没有覆盖整个研究区域,因为它的推进发生在几个裂片上。除了Biała Podlaska和Łuków平原以外,西波利西地区Włodawa的周边地区是波河地区第三大的马祖纪古湖区。
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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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