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首页> 外文期刊>Quaternary International >Forest-savanna boundary shift on the plateau of Serra Sul dos Carajas (southeastern Amazonia) since the mid-Holocene; driving forces and limiting factors
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Forest-savanna boundary shift on the plateau of Serra Sul dos Carajas (southeastern Amazonia) since the mid-Holocene; driving forces and limiting factors

机译:自全新世中期以来,Serra Sul dos Carajas(东南亚马逊地区)高原上的森林-热带稀树草原边界转移;驱动力和限制因素

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摘要

The vegetation history of the savanna on the plateau of Serra Sul dos Carajas (PSSC) is well studied by three palynological records. Nonetheless there is no record from the forests around this plateau so that the long term forest-savanna boundary shift can be investigated. In this study, a sediment core taken from the forests on the slopes of the plateau is studied using a multi-proxy analysis. The palynological result is compared with the records from adjacent savanna. This study reveals that well-established forests have been present around the plateau during the last 6600 cal yr BP. Since the mid-Holocene owing to a change to favorable climatic conditions, forests started to move toward the savanna and after 3400-4000 years reached their modern borders in the savanna region. Because during this long period forest borders moved horizontally a relatively short distance (ca. 250 m), we concluded that there might be limiting factors that delayed forest expansion. Among different possible factors, fire and human may play an important role. However, the evidence suggests that the slow process of soil formation to produce a soil layer with sufficient depth is the main limiting factor that delayed the forest expansion. According to the previous hydroclimatic and palaeo-ecological studies, the southward displacement of Inter Tropical Convergence Zone (ITCZ) is more likely the trigger of forest expansion in the area since the mid-Holocene. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:通过三个孢粉学记录,对Serra Sul dos Carajas(PSSC)高原的热带稀树草原的植被历史进行了很好的研究。但是,没有高原地区森林的记录,因此可以调查长期的森林​​-热带稀树草原边界转移。在这项研究中,使用多重代理分析法研究了高原斜坡上森林中的沉积物芯。将古生物学结果与相邻大草原的记录进行比较。这项研究表明,在过去6600多年的BP期间,高原周围一直存在着完善的森林。由于全新世中期由于气候条件的变化,森林开始向热带稀树草原转移,并在3400-4000年后到达热带稀树草原边界。因为在这段较长的时间内,森林边界在水平方向上移动了相对较短的距离(约250 m),所以我们得出结论,可能有一些限制因素延迟了森林的扩张。在不同的可能因素中,火灾和人为可能起着重要作用。但是,有证据表明,土壤形成过程缓慢以产生具有足够深度的土壤层是延迟森林扩张的主要限制因素。根据先前的水文气候和古生态学研究,自全新世中期以来,热带辐合带(ITCZ)的向南移位很可能是该地区森林扩张的触发因素。 (C)2017爱思唯尔有限公司和INQUA。版权所有。

著录项

  • 来源
    《Quaternary International》 |2017年第25期|12-21|共10页
  • 作者单位

    Univ Gottingen, Albrecht von Haller Inst Plant Sci, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany;

    Univ Gottingen, Fac Geog, Dept Cartog GIS & Remote Sensing, Goldschmidtstr 5, D-37077 Gottingen, Germany;

    Univ Gottingen, Albrecht von Haller Inst Plant Sci, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany;

    Univ Gottingen, Albrecht von Haller Inst Plant Sci, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany;

    Fed Univ Para, Geosci Inst, Ave Augusto Correa 1, BR-66075110 Belem, Para, Brazil;

    Univ Gottingen, Albrecht von Haller Inst Plant Sci, Dept Palynol & Climate Dynam, Untere Karspule 2, D-37073 Gottingen, Germany;

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

    Carajas; Vegetation history; Palynology; Soil properties; Fire; Holocene;

    机译:卡拉加斯;植被历史;植物学;土壤性质;火;全新世;
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