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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >Ecohydrological evolution of Lake Naivasha (central Rift Valley, Kenya) during the past 1650 years, as recorded by ostracod assemblages and stable-isotope geochemistry
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Ecohydrological evolution of Lake Naivasha (central Rift Valley, Kenya) during the past 1650 years, as recorded by ostracod assemblages and stable-isotope geochemistry

机译:奥斯特拉科德集会和稳定同位素地球化学记录在过去1650年中纳瓦莎(中央裂谷,肯尼亚)的生态学演变

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Lake Naivasha (central Rift Valley, Kenya) is regionally unique in having accumulated a continuous sediment record of climate-driven palaeohydrological change over the past 1650 years, attesting to dramatic shifts between freshwater high-stands and either fresh or saline low-stands. This study employs fossil ostracod assemblages and stable-isotope (delta O-18 and delta C-13) signatures to disclose the lake's ecohydrological history and explain the evolving non-linearity between lake level and salinity. The original age model and lithology-based lake-level reconstruction are revised, and the diatom-inferred salinity reconstruction is expanded to the lower (pre-770 CE) part of the record. The stable-isotope time series showed limited coherence with the other proxies, probably due to complexities related to hydrological connections between different surface- and groundwater components shifting through time. Ostracod palaeoecological data indicate that between ca 350 and 1200 CE the system often veered towards hydrological closure, with frequent and high-amplitude shifts in lake level and salinity preventing long-term establishment of wetland vegetation. Low lake-level and saline conditions dominated between ca 900 and 1200 CE. After that time and particularly since the onset of more permanent Malewa River inflow ca 1430 CE, hydrologically open conditions prevailed. Salinity shifts exhibited lower amplitude and frequency, promoting the expansion of wetland vegetation and associated biota including benthivorous fish. With lake water balance strongly influenced by variation in river inflow, high-amplitude lake-level fluctuations continued throughout the freshwater phase of the past 600 years, notably creating a pronounced high-stand dated to ca 1600-1780 CE and the well-documented extreme low-stand of the early 1800s. (C) 2019 Elsevier Ltd. All rights reserved.
机译:纳瓦希岛(中央裂谷,肯尼亚)是在过去的1650年中积累了持续沉积的气候驱动古水系统造成的持续沉积物记录,证明了淡水高架和新鲜或盐水低位之间的戏剧性变化。本研究采用化石Ostracod组装和稳定同位素(Delta O-18和Delta C-13)签名,以披露湖泊的生态文化历史,并解释湖泊水平和盐度之间的不良线性。修订了原始年龄模型和基于岩性的湖泊级重建,并且硅藻推断的盐度重建扩展到记录的较低(770章)部分。稳定同位素时间序列显示出与其他代理相干有限,可能是由于与不同表面和地下水部件之间的水文连接相关的复杂性。 Ostracod古生学数据表明,CA 350和1200 CE之间的系统经常转向水文闭合,湖泊水平和盐度频繁和高幅度的变化,防止了湿地植被的长期建立。低湖级和盐水条件,在CA 900和1200 CE之间占主导地位。之后,特别是自从更永久的Malalwa河流入Ca 1430 Ce的开始以来,水文开放的条件普遍存在。盐度变化表现出较低的幅度和频率,促进湿地植被的扩展和相关的生物群,包括孤独的鱼类。随着湖水平衡受到河流流入变异的强烈影响,在过去600年的淡水阶段,高幅度的湖泊水平波动仍在继续,特别是创造了一个日期为CA 1600-1780 CE和良好的极端的明显高位。 18世纪初的低头。 (c)2019年elestvier有限公司保留所有权利。

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