...
首页> 外文期刊>Journal of paleolimnology >The first dated preglacial diatom record in Lake Ladoga: long-term marine influence or redeposition story?
【24h】

The first dated preglacial diatom record in Lake Ladoga: long-term marine influence or redeposition story?

机译:Lake Lake Lake Lake Lake Marine影响或重新沉积故事

获取原文
获取原文并翻译 | 示例

摘要

Preglacial environments in Lake Ladoga, the largest European lake, located within the limits of the Scandinavian glaciations, are very poorly investigated compared to postglacial ones. They were primarily reconstructed based on the studies of terrestrial boreholes and outcrops, often incomplete and poorly dated. Previous diatom studies established that during the Eemian marine transgression, the Ladoga basin became a part of the marine Baltic-White Sea connection. However, the environments established in Lake Ladoga after the regression of the Eemian Sea are not known. This article discusses the first Early Weichselian (MIS5, similar to 118-80 ka) diatom record in Lake Ladoga obtained within the frame of the Russian-German research project PLOT. Low concentrations and selective preservation of diatoms in the preglacial sediments point to unstable high-energy environments. The presence of marine diatoms is thought to result from reworking of marine Eemian sediments, rather than direct marine influence. We argue that post-Eemian environments in Lake Ladoga were neither marine nor glaciolacustrine, as previously suggested. The Early Weichselian diatom record formed in a shallow-water part of a lake affected by inflowing streams transporting large amounts of eroded material. No analogues of the preglacial environments can be found in the postglacial Lake Ladoga. Our record demonstrates close similarity to other Early Weichselian diatom records in the Ladoga region suggesting their formation under the same conditions. Similar trends in concentrations of diatoms, diatom fragments and other siliceous microfossils reflect changing sediment supply, hydrodynamics or reworking intensity. Their lower values similar to 118-113 and similar to 90-80 ka could reflect the Early Weichselian cooling stages, while their increase between similar to 113 and 90 ka might indicate enhanced erosion intensity and increased sediment supply corresponding to the climate amelioration.
机译:拉多加湖是欧洲最大的湖泊,位于斯堪的纳维亚冰川活动的范围内,与冰后期相比,其冰前环境的研究非常薄弱。它们主要是基于对陆地钻孔和露头的研究而重建的,这些钻孔和露头往往不完整,年代也不准确。此前的硅藻研究证实,在伊米安海侵期间,拉多加盆地成为波罗的海-白海连接的一部分。然而,埃米安海海退后在拉多加湖建立的环境尚不清楚。本文讨论了在俄罗斯-德国研究项目地块框架内获得的拉多加湖第一个早期魏氏(MIS5,类似于118-80ka)硅藻记录。冰期前沉积物中硅藻的低浓度和选择性保存表明高能环境不稳定。海洋硅藻的存在被认为是由于海洋沉积物的改造,而不是直接的海洋影响。我们认为,拉多加湖的后伊米安环境既不是海洋环境,也不是冰川沉积环境,正如之前所说的那样。早期魏氏硅藻记录形成于湖泊的浅水部分,受流入的溪流影响,输送大量侵蚀物质。在冰期后的拉多加湖中,找不到类似冰期前的环境。我们的记录与拉多加地区的其他早期魏氏硅藻记录非常相似,表明它们是在相同条件下形成的。硅藻、硅藻碎片和其他硅质微体化石浓度的类似趋势反映了沉积物供应、水动力学或改造强度的变化。它们的较低值(类似于118-113和90-80 ka)可能反映了魏氏早期的冷却阶段,而它们在类似于113和90 ka之间的增加可能表明侵蚀强度增强,沉积物供应增加,与气候改善相对应。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号