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首页> 外文期刊>Quaternary International >Evaluation of the potential of surface pollen spectra from caves in SW China for vegetation reconstruction
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Evaluation of the potential of surface pollen spectra from caves in SW China for vegetation reconstruction

机译:评价SW中国洞穴表面花粉谱的潜力为植被重建

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摘要

Pollen analysis is rarely applied to cave sediments because of the complex range of processes influencing the origin, transport and taphonomy of pollen grains in caves. In order to evaluate the potential of pollen spectra from within caves for vegetation reconstruction, we compared the modern pollen from the interior and exterior of four caves in Guangxi and Guizhou, in southwestern China. The results show that the pollen spectra from within the sack-shaped caves, and from the front and middle of a long, narrow caves, were similar to those outside the caves, and therefore that the pollen spectra from these caves can reliably be used for palaeovegetation reconstruction. Wind is the major transport medium for the pollen entering caves, but animals may be additional transport medium. In addition, cave geometry is likely to be responsible for the observed spatial distribution of pollen concentrations in caves. In long, narrow caves, the entrance is the optimum sampling location for pollen analysis; however, in sack-shaped caves an optimum sampling location cannot be specified due to the gradient in pollen concentration between the entrance and the rear, together with its irregular distribution.
机译:花粉分析很少适用于洞穴沉积物,因为影响了花粉颗粒在洞穴中的起源,运输和Taphonomy的复杂过程。为了评估来自植被重建的洞穴中花粉光谱的潜力,我们将在中国西南部的广西和贵州的四洞内外的现代花粉与中国西南部。结果表明,从袋状腔内的花粉光谱和长狭窄的前部和中间,与洞穴外部类似,因此可以可靠地使用来自这些洞穴的花粉光谱PalaeoveGetation重建。风是花粉进入洞穴的主要运输培养基,但动物可能是额外的运输培养基。此外,洞穴几何体可能负责观察到洞穴中的花粉浓度的空间分布。在长狭窄的洞穴中,入口是花粉分析的最佳采样位置;然而,在袋状洞中,由于入口和后部的花粉浓度的梯度,并且与其不规则分布在一起,不能指定最佳采样位置。

著录项

  • 来源
    《Quaternary International》 |2021年第30期|119-128|共10页
  • 作者单位

    Chinese Acad Sci Inst Vertebrate Paleontol & Paleoanthropol Key Lab Vertebrate Evolut & Human Origin Beijing 100044 Peoples R China|CAS Ctr Excellence Life & Paleoenvironm Beijing 100044 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Vertebrate Paleontol & Paleoanthropol Key Lab Vertebrate Evolut & Human Origin Beijing 100044 Peoples R China|CAS Ctr Excellence Life & Paleoenvironm Beijing 100044 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Vertebrate Paleontol & Paleoanthropol Key Lab Vertebrate Evolut & Human Origin Beijing 100044 Peoples R China|CAS Ctr Excellence Life & Paleoenvironm Beijing 100044 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Vertebrate Paleontol & Paleoanthropol Key Lab Vertebrate Evolut & Human Origin Beijing 100044 Peoples R China|CAS Ctr Excellence Life & Paleoenvironm Beijing 100044 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Chinese Acad Sci Inst Vertebrate Paleontol & Paleoanthropol Key Lab Vertebrate Evolut & Human Origin Beijing 100044 Peoples R China|CAS Ctr Excellence Life & Paleoenvironm Beijing 100044 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Guangxi Univ Nationalities Inst Hist & Culture Sci & Technol Nanning 530006 Peoples R China;

    Chinese Acad Sci Inst Vertebrate Paleontol & Paleoanthropol Key Lab Vertebrate Evolut & Human Origin Beijing 100044 Peoples R China|CAS Ctr Excellence Life & Paleoenvironm Beijing 100044 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

    Shandong Univ Inst Cultural Heritage Qingdao 250100 Peoples R China;

    Chinese Acad Sci Inst Vertebrate Paleontol & Paleoanthropol Key Lab Vertebrate Evolut & Human Origin Beijing 100044 Peoples R China|CAS Ctr Excellence Life & Paleoenvironm Beijing 100044 Peoples R China|Univ Chinese Acad Sci Beijing 100049 Peoples R China;

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

    Cave palynology; Taphonomy; Palaeovegetation; Southwestern China;

    机译:Cave Palynology;taphonomenty;Palaeovegetation;中国西南;

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