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Interdisciplinary investigations of the first reported laminated lacustrine sediments in Romania

机译:罗马尼亚首次报告的层积湖相沉积物的跨学科研究

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摘要

An interdisciplinary study (cartographic and historical records, geomorphological, geological and bathymetric survey, water analysis, sediment coring and analysis and AMS radiocarbon dating) of two small and previously unreported lakes (Iezer and Bolatau) in Obcina Feredeului Mountains, northeastern Romania, provides new data into the environmental history and possible human impacts over the last millennium in this region. The first recorded historical reference to Iezer Lake dates to 1594 AD, and to Bolatau Lake to 1806 AD. Two sediment cores (420 cm for Iezer and 540 cm for Bolatau) of finely banded lake sediments and a radiocarbon age estimate at Iezer Lake suggest that this lake may represent the oldest landslide lake in Romania. The geomorphological, geological, and morphometric surveys indicate that these lakes' origins relate to landslide activity. Coarse grained, lighter sediment bands are generally characterized by higher values in magnetic susceptibility, Saturation Isothermal Remanent Magnetisation (SIRM), as well in geochemical indicators such as Ti and Zr, and low organic content, possibly indicating periods of increased runoff. Conversely, finer-grained, dark sediment bands show lower values in magnetic susceptibility, SIRM, Ti and Zr and higher organic content, and are likely to suggest quieter deposition periods. However, there are two significant episodes of markedly increased surface erosion. The oldest occurs between 100 and 110 cm, and might be coincident with the terminal part of Little Ice Age (LIA), whereas the youngest in the top 30 cm coincides with recent land use. These lakes hold significant potential in providing an important perspective on the environmental conditions over the last millennium and, more specifically, to supply new information about the Medieval Warm Period (MWP) and LIA signals in the NE Romanian Carpathians. These two landslide-dammed lakes should be defined as scientific reserves to ensure their protection and to enhance their use as a scientific and educational resource.
机译:在罗马尼亚东北部的奥比纳·费雷德鲁伊山上两个未曾报告的小湖泊(Iezer和Bolatau)的跨学科研究(地理和历史记录,地貌,地质和测深测量,水分析,沉积物取芯和分析以及AMS放射性碳定年)提供了新的领域数据记录了该地区最近一千年的环境历史和可能的人类影响。关于伊泽尔湖的最早历史记载可追溯到公元1594年,到博拉陶湖的历史可追溯到公元1806年。细带状湖泊沉积物的两个沉积物核心(伊泽尔为420厘米,博拉陶为540厘米)以及伊泽尔湖的放射性碳年龄估计表明该湖可能代表了罗马尼亚最古老的滑坡湖。地貌,地质和形态计量学调查表明,这些湖泊的起源与滑坡活动有关。粗粒状,较轻的沉积物带通常具有磁化率,饱和等温剩余磁化强度(SIRM)以及Ti和Zr等地球化学指示值较高,有机物含量较低的特征,这可能表明径流增加。相反,较细的暗沉积带显示出较低的磁化率,SIRM,Ti和Zr值以及较高的有机物含量,并可能暗示较安静的沉积期。然而,有两个明显的事件是表面侵蚀明显增加。最古老的发生在100到110厘米之间,可能与小冰河时代(LIA)的末端相吻合,而最顶端的30厘米则与最近的土地利用相吻合。这些湖泊具有很大的潜力,可以提供有关上一个千年的环境状况的重要观点,更具体地说,可以提供有关罗马尼亚东北喀尔巴阡山脉的中世纪暖期(MWP)和LIA信号的新信息。应将这两个滑坡坝湖泊定义为科学保护区,以确保对其进行保护并增强其作为科学和教育资源的用途。

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  • 来源
    《Quaternary International》 |2013年第19期|219-230|共12页
  • 作者单位

    University ofSuceava, Department of Geography, Universitatii Street, Suceava 720229, Romania;

    University ofSuceava, Department of Geography, Universitatii Street, Suceava 720229, Romania;

    School of Environment and Life Sciences, University ofSalford, Salford M5 4WT, UK;

    University ofSuceava, Department of Geography, Universitatii Street, Suceava 720229, Romania;

    Senckenberg Research Institute and Natural History Museum & Biodiversity and Climate Research Centre (BiK-F), Senckenberganlage 25, 60325 Frankfurt am Main, Germany;

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