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首页> 外文期刊>The Science of the Total Environment >Holocene vegetation-hydrology-climate interactions of wetlands on the Heixiazi Island, China
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Holocene vegetation-hydrology-climate interactions of wetlands on the Heixiazi Island, China

机译:全新世植被 - 水文 - 气候互动湿地在河口岛湿地,中国

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摘要

An integrated view of wetland's evolution is currently poorly understood due to a lack of knowledge on long-term interactions of multiple ecological factors. Here, we present a cored palynological record covering the Ho-locene Epoch from a depressional wetland on Heixiazi Island (China). With the aid of principal component analysis and cluster analysis of the palynological data, the historical vegetation regime has been well reconstructed for wetlands on the island. With further assistance from the published data on local hydrology and regional East Asian summer monsoon (EASM) variations, the interactions of vegetation, hydrology, and climate in the island's wetlands have been thoroughly analyzed with correlation analysis of the three factors. The results indicate that a strong EASM generally led to a high water level in the wetlands from increased monsoonal precipitation, causing an increase in arboreal vegetation and a decrease in herbs. Alternatively, a weak EASM generally led to low water levels due to decreased monsoonal precipitation, causing a decrease in arboreal vegetation and an increase in herbs. The local vegetation regime during the early Holocene was marked by an increase in tree/herb ratio due to rising water levels under the influence of an increasingly strengthened EASM. Subsequently, a general decline of the tree/herb ratio occurred from a gradual decrease in water level during the mid and late Holocene when the EASM gradually retreated. The wettest stage marked by the highest water level and tree/herb ratio occurred 8.0-4.6 ka BP with the strongest EASM. The driest stage occurred during the last 0.4 ka BP, which was attributed to both the weakest EASM influence and anthropogenic disturbance. Our study provides an integrated view of the wetlands' ecological dynamics incorporating multi-factor interactions, which further sheds light on the EASM driving mechanisms on wetlands evolution during the Holocene Epoch.
机译:由于缺乏关于多种生态因素的长期相互作用的知识,湿地演化的综合观点目前很差。在这里,我们提出了一种覆盖Ho-Locene时代的核心宫科学记录,来自海克西亚岛(中国)的萧条湿地。借助于对腭相关的主要成分分析和聚类分析,历史植被制度在岛上的湿地重建了很好的重建。根据本地水文和区域东亚夏季季风(EASM)变异的进一步援助,岛屿湿地的植被,水文和气候的相互作用已经彻底分析了三种因素的相关性分析。结果表明,强劲的EASM通常导致湿地的高水位来自季风沉淀增加,导致树栖植被增加和草药的减少。或者,由于季铵沉淀降低,弱EASM通常导致水平的低水位,导致树栖植被降低和草药的增加。由于越来越强化的EASM的影响,由于水平升高,本体早期全新世的植被制度标志着树质/草药比例。随后,当EASM逐渐退回时,树/草药比例的一般性下降是从中期和晚期水平的水平逐渐减少。最高水位和树木/草药比率标记的最潮湿阶段发生8.0-4.6 kA BP,具有最强的EASM。最干燥的阶段发生在最后0.4 kA BP期间,这归因于最弱的EASM影响和人为干扰。我们的研究提供了包含多因素相互作用的湿地生态动态的综合图,该综合性是多因素相互作用,在全新世纪时代期间进一步阐明了湿地演化的EASM驱动机制。

著录项

  • 来源
    《The Science of the Total Environment》 |2020年第15期|140777.1-140777.10|共10页
  • 作者单位

    School of Geographic and Environmental Sciences Tianjin Normal University Tianjin 300387 China Key Laboratory of Wetland Ecology and Environment Northeast Institute of Geography and Agroecology Chinese Academy of Sciences Changchun 130102 China;

    Department of Natural Sciences University of Michigan-Dearborn Dearborn Ml 48128 USA;

    Key Laboratory of Wetland Ecology and Environment Northeast Institute of Geography and Agroecology Chinese Academy of Sciences Changchun 130102 China;

    College of Resources and Environment Science Hebei Normal University Shijiazhuang 050024 China;

    Key Laboratory of Wetland Ecology and Environment Northeast Institute of Geography and Agroecology Chinese Academy of Sciences Changchun 130102 China Jillin Provincial Joint Laboratory of Changbai Mountain Wetland and Ecology Northeast Institute of Geography and Agroecology Chinese Academy of Sciences Changchun 130102 China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Holocene; Wetland; Monsoon; Heixiazi Island; Pollen;

    机译:全新世;湿地;季风;乔西岛;花粉;

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