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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >Late Weichselian and Holocene record of the paleoenvironmental changes in a small river valley in Central Poland
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Late Weichselian and Holocene record of the paleoenvironmental changes in a small river valley in Central Poland

机译:波兰中部小河谷古魏世晚期和全新世记录的古环境变化

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摘要

The developmental history, from the Oldest Dryas to the Late Holocene, of a paleolake and mire located in a river valley in Central Poland was studied using high-resolution records of pollen, macrofossils, Cladocera, sedimentology, and geochemistry from a C-14 dated sediment core. We inferred temperature and water level dynamics using cladocerans and palynological and geochemical methods were employed to investigate natural fluvial activity, particularly for these elements that are difficult to find through sedimentological methods. Our research demonstrates how climate fluctuation in the Late Glacial and Holocene periods influenced the development of a paleolake and mire in a small river valley and shows the importance of long-term research to establish hydroclimatic conditions in biogenic sediments. We propose that water level fluctuations were important in modifying biotic assemblages. The results of our multiproxy analysis clearly suggest that the main driver of changes in aquatic and terrestrial ecosystems, as well as in geomorphological processes in the valley, was climate: reconstructed temperatures generally follow the known trends, showing an increase at the beginning of the Balling, Allerod, and Holocene and a decrease at the beginning of the Oldest and Younger Dryas. Similarly, periods of water level increase are synchronous with climatic changes. However, the local environmental forces were a significant factors affecting biotic diversity in the studied time span. Fish predation, macrophyte structure, pH, and calcium content partly influence the results of the cladoceran-based water depth reconstruction in particular. Interestingly, the cladoceran-inferred summer temperature reconstruction for Pawlowa appear realistic. Although the temperature trends can be considered reliable, our results indicate the important role of local factors which control the species composition of the subfossil assemblages. (C) 2016 Elsevier Ltd. All rights reserved.
机译:研究人员使用高分辨率的花粉,大型化石,克拉德克拉,沉积学和地球化学数据(来自C-14),研究了波兰中部河谷古灰和泥沼从最古老的树蛙到新世晚期的发展历史。沉积物核心。我们利用枝ado推断温度和水位动态,并采用孢粉学和地球化学方法研究自然河流活动,特别是对于那些难以通过沉积学方法找到的元素。我们的研究表明,冰川晚期和全新世晚期的气候波动如何影响小河流域的古湖和泥潭的发展,并显示了长期研究在生物成因沉积物中建立水文气候条件的重要性。我们认为水位波动对于改变生物组成很重要。我们的多代理分析结果清楚地表明,气候变化的主要驱动力是山谷中水生和陆地生态系统以及地貌过程的变化:重建的温度通常遵循已知的趋势,在Balling开始时呈上升趋势。 ,Allerod和全新世,而最早和最年轻的树妖开始减少。同样,水位上升时期与气候变化同步。然而,在所研究的时间范围内,当地环境力量是影响生物多样性的重要因素。鱼的捕食,大型植物的结构,pH和钙含量在一定程度上影响了基于角叉菜的水深重建的结果。有趣的是,用锁骨蜡推断的Pawlowa夏季温度重建似乎是现实的。尽管可以认为温度趋势是可靠的,但我们的研究结果表明了控制次化石组合物种组成的局部因素的重要作用。 (C)2016 Elsevier Ltd.保留所有权利。

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