...
首页> 外文期刊>Quaternary International >Carbonate features in the uppermost layers of Quaternary deposits, Northern Armenia, and their significance for paleoenvironmental reconstruction
【24h】

Carbonate features in the uppermost layers of Quaternary deposits, Northern Armenia, and their significance for paleoenvironmental reconstruction

机译:亚美尼亚北部第四纪沉积最上层的碳酸盐特征及其对古环境重建的意义

获取原文
获取原文并翻译 | 示例
           

摘要

Recent archaeological studies in the Lori Depression of Armenia (Lesser Caucasus) revealed a series of multilevel Early Paleolithic (Acheulian) sites belonging to the Early-Middle Pleistocene stage of occupation of the Caucasus. In the uppermost layers of these sites, the paleosols and sediments contain carbonate features (CFs) whereas the lower layers are absolutely free from carbonates. The aim of this work is to examine the role of detected CFs as an indicator for reconstructions of the Early-Middle Pleistocene paleoenvironments, to determine the source, time and conditions of carbonates' accumulation in initially non-calcareous and high-degree weathered humid paleosols. Three sections were studied: Kurtan I, points 1-2 and Muradovo. There are different forms of CFs represented by the calcified root cells in the layer 1, the hard nodules in the layer 2 and the laminae-like carbonates in the layer 3 of the sites studied. All the CFs are of the aqueous (hydrogenic) origin. The CFs of the uppermost layers 1 and 2 in the Kurtan I, point 2 were accumulated in the Holocene lake. The calcified root cells were formed on the swamp shore whereas the hard nodules on the lake bottom under stagnant water. The laminae like carbonates in the layer 3 were accumulated in the Kurtan I and Muradovo sections due to strong erosion cycle(s) in the Late Pleistocene interglacial period(s) that led to the limestone scour in the region by ground and surface water. They reflect the earliest stage of the allochthonous carbonate accumulation in the area dated by radiocarbon method to approximately 20 ka cal BR Therefore, all the CFs cannot be regarded as indicative of Early and Middle Pleistocene environmental changes, as they appeared in the uppermost layers of the studied sections much later than the time of formation for the surrounding groundmass. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:最近在亚美尼亚洛里洼地(Lesser高加索地区)的考古学研究表明,一系列多层次的旧石器时代(Acheulian)遗址属于高加索占领的中更新世早期。在这些站点的最上层,古土壤和沉积物包含碳酸盐特征(CFs),而下层绝对不含碳酸盐。这项工作的目的是检验检测到的CFs作为重建中早更新世古环境的指标的作用,以确定最初非钙质和高度风化的潮湿古土壤中碳酸盐岩堆积的来源,时间和条件。 。研究了三个部分:Kurtan I,第1-2点和Muradovo。有不同形式的CFs,由第1层中的钙化根细胞,第2层中的硬结节和第3层中的层状碳酸盐表示。所有的CF都是水源(水合)。 Kurtan I,点2的最上层1和2的CF聚集在全新世湖中。积水形成了钙化的根细胞,而湖底形成了硬结节。第3层中的层状碳酸盐由于在晚更新世间冰期强烈的侵蚀循环而聚集在Kurtan I和Muradovo剖面中,导致该地区的石灰石冲刷受到地下水和地表水的冲刷。它们反映了通过放射性碳法测定的大约20 ka cal BR内该地区碳酸盐碳酸盐堆积的最早阶段。因此,所有CFs都不能被视为指示早更新世和中更新世环境的变化,因为它们出现在该地区的最上层。研究断面的时间要比周围地面的形成时间晚得多。 (C)2015 Elsevier Ltd和INQUA。版权所有。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
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