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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Understanding Amazonian fluvial rias based on a Late Pleistocene-Holocene analog
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Understanding Amazonian fluvial rias based on a Late Pleistocene-Holocene analog

机译:基于晚更新世-全新世类似物了解亚马逊河河谷

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摘要

Fluvial rias are elongated lakes at tributary mouths that can reach dozens of kilometers in length, constituting one of the most remarkable features in the Amazonian landscape. Thus far, definitive data which documents the genesis of fluvial rias have not been published. The main goal of this work was to integrate morphological, sedimentological and chronological information in order to characterize fluvial paleorias in the interfluve of the Purus and Madeira Rivers and discuss the most likely hypothesis for their genesis. These paleorias were first observed through remote sensing imagery as several elongated and interconnecting belts of open vegetation that are in sharp contact with the surrounding dense forest. The belts are branched and form a dendritic pattern similar to many modern drainage networks. The sedimentary record of these belts revealed the prevalence of sharp-based sandstones and mudstones arranged into fining-upward successions, which are compatible with deposition within channels. Active channel and abandoned channel deposits were recognized. These are topped by continuous mudstones related to rapid channel abandonment and formation of a low energy basin or ria environment. Radiocarbon dating of these deposits recorded only Late Pleistocene and Holocene ages ranging from 21 547-22 285calyrbp to 5928-6124calyrbp. This chronology for sediment deposition is not compatible with the hypothesis of Amazonian rias being formed by fluvial erosion during the Last Glaciation Maximum low sea level, with sediment accumulation during the subsequent Holocene transgression. Instead, the studied paleorias record previous tributaries of the Madeira River that became abandoned as the position of this river shifted southeastward and its interfluve tilted northward, inverting the drainage systems. Therefore, a neotectonic origin of some Amazonian paleorias seems most likely. This hypothesis should be considered in further investigations aiming at understanding the origin of numerous modern fluvial rias that typify the Amazonian landscape. Copyright (c) 2014 John Wiley & Sons, Ltd.
机译:河流河口是在支流口处拉长的湖泊,可长达数十公里,是亚马孙地区最显着的特征之一。迄今为止,还没有公开记载河流性尿道炎的确切数据。这项工作的主要目的是整合形态学,沉积学和年代学信息,以表征普鲁斯河和马德拉河交汇处的河流古古迹,并讨论最可能的假说。这些古地理首先通过遥感图像被观察到,它们是与周围茂密森林紧密接触的几条细长且相互连接的开放植被带。这些带是分支的,形成类似于许多现代排水网络的树状图案。这些带的沉积记录表明,以尖锐的砂岩和泥岩的分布为精细向上的演替,这与河道内的沉积相容。活跃渠道和废弃渠道的存款得到确认。这些被连续的泥岩所覆盖,这些泥岩与快速通道的废弃和低能盆地或ria环境的形成有关。这些沉积物的放射性碳测年仅记录了晚更新世和全新世的年龄,范围从21 547-22 285 calyrbp至5928-6124 calyrbp。这种沉积物沉积的时间顺序与最后一次冰川最大低海平面期间河流侵蚀形成的亚马逊河里亚斯假说不符,随后的全新世海侵则沉积物堆积。取而代之的是,所研究的古希腊记录了马德拉河的先前支流,该支流由于该河的位置向东南移动而其河道向北倾斜,从而使排水系统倒置而被废弃。因此,某些亚马逊古生物的新构造起源似乎是最有可能的。在进一步的研究中应考虑这一假设,以了解众多代表亚马逊地区景观的现代河流河谷的起源。版权所有(c)2014 John Wiley&Sons,Ltd.

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