首页> 外文期刊>Quaternary International >Vegetation and climate changes during three interglacial periods represented in the Luochuan loess-paleosol section, on the Chinese Loess Plateau
【24h】

Vegetation and climate changes during three interglacial periods represented in the Luochuan loess-paleosol section, on the Chinese Loess Plateau

机译:黄土高原洛川黄土古土壤剖面三个间冰期的植被与气候变化

获取原文
获取原文并翻译 | 示例
           

摘要

Studies of vegetation successions related to climate changes during previous interglacial periods provide important insights into the mechanisms of climate change during the current interglacial and enable predictions of future climate impacts on ecosystems. The Chinese Loess Plateau (CLP), which is particularly sensitive to climate warming, presents an excellent site for such studies. However, few detailed records exist of vegetation and climate variations during interglacial periods on the CLP. This study obtained a series high resolution pollen records from the Luochuan loess-paleosol section on the CLP, and the paper discusses the vegetation and climate histories during three previous interglacial periods (MIS 9, MIS 7 and MIS 5). The Artemisia-Chenopodiaceae steppe vegetation that covered this area between 342 ka and 312 ka changed to Humulus-Chenopodiaceae steppe between 312 ka and 302 ka, and then reverted to Artemisia-Chenopodiaceae steppe after 302 ka. From 250 ka to 237 ka, the vegetation type remained Artemisia-Chenopodiaceae steppe, and then changed to Artemisia-Humulus steppe between 237 ka and 227 ka. Between 227 ka and 195 ka, the vegetation returned to Aremisia-Chenopodiaceae steppe. During MIS 5, vegetation of the study area changed from Pinus-Rosaceae-Chenopodiaceae forest-steppe between 129 ka and 117 ka, to Artemisia-Humulus-Ranunculaceae steppe from 117 ka to 96 ka. After 96 ka, the vegetation types changed to Pinus-Betula-Chenopodiaceae forest-steppe. Comparing these pollen records with other climatic proxies from the CLP and the oxygen isotope records from the Pacific Ocean suggests that vegetation and climate change features around the study site were synchronous with East Asian monsoon variations near 65° N. The regional tectonic uplift probably provided only a subordinate influence on vegetation and climate variation on the CLP during MIS 5.
机译:对前冰期之间与气候变化有关的植被演替的研究为了解当前冰期之间的气候变化机制提供了重要见解,并有助于预测未来气候对生态系统的影响。中国黄土高原(CLP)对气候变暖特别敏感,是开展此类研究的绝佳场所。然而,中电在冰期之间很少有植被和气候变化的详细记录。这项研究从中电洛川黄土古土壤剖面获得了一系列高分辨率花粉记录,并对前三个冰期(MIS 9,MIS 7和MIS 5)的植被和气候历史进行了讨论。覆盖在342 ka和312 ka之间的这一区域的蒿-藜科草原植被在312 ka和302 ka之间变成了Hum草-藜科草草原,然后在302 ka之后恢复为蒿-藜科草草原。从250 ka到237 ka,植被类型保持为艾蒿-藜科草原,然后在237 ka和227 ka之间变为艾蒿-Hu草草原。在227 ka和195 ka之间,植被恢复为Aremisia-藜科的草原。在MIS 5期间,研究区的植被从129 ka至117 ka的松树-蔷薇科-藜科的草原转变为从117 ka到96 ka的蒿-Humulus-毛un科的草原。 96 ka后,植被类型变为松-桦-藜科森林草原。将这些花粉记录与来自CLP的其他气候指标以及来自太平洋的氧同位素记录进行比较,表明研究地点周围的植被和气候变化特征与65°N附近的东亚季风变化同步。区域构造隆升可能仅提供了在MIS 5期间对CLP的植被和气候变化产生从属影响。

著录项

  • 来源
    《Quaternary International》 |2013年第16期|131-140|共10页
  • 作者单位

    Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China;

    College of Resource, Environment and Tourism, The Capital Normal University, Beijing 100048, China;

    College of Resource, Environment and Tourism, The Capital Normal University, Beijing 100048, China;

    Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou 730000, China;

    Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China;

    College of Resource, Environment and Tourism, The Capital Normal University, Beijing 100048, China;

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

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