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Combining environmental history and soil phytolith analysis at the City of Rocks National Reserve: Developing new methods in historical ecology.

机译:结合岩石历史国家保护区的环境历史和土壤植物石板分析:开发历史生态学的新方法。

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Historical ecology is an emerging and interdisciplinary field that seeks to explain the changes in ecosystems over time through a synthesis of information derived from human records and biological data. The methods in historical ecology cover a wide range of temporal and spatial scales. However, methods for the more recent past (about 200 years) are largely limited to the human archive and dendrochronological evidence which can be subject to human bias, limited in spatial extent or not appropriate for non-forested systems. There is a need to explore new methods by which biological data can be used to understand historic vegetation and disturbance regimes over the recent past especially in arid ecosystem types. Soil phytolith analysis has the potential to provide much needed information regarding historical conditions in both areas. Phytoliths are structures formed in plants through deposition and accumulation of silica within and around cell walls that are released from plants and preserved in sediments long after death and decay of plant material. The City of Rocks National Reserve in southern Idaho was an excellent place to develop new methods in historical ecology because the human records of historic environmental conditions were so rich. There were two overarching and interconnected objectives for this dissertation research. The first was to reconstruct an ecological history of the City of Rocks National Reserve from the period of overland emigration to present. The second objective was to explore the utility of soil phytolith analysis for inferring vegetation and disturbance regime change over the recent past by testing its sensitivity to record known changes. I employed modern analogue studies, a multi-core approach and detailed core analysis to test for known changes through analysis of extraction weights, relative abundance of phytolith assemblages, microscopic charcoal and burned (darkened) phytoliths. My results showed that this combination of history and soil phytolith analysis would be a useful approach for inferring vegetation changes (e.g. increases in introduced grasses) and disturbances (e.g. fire) in ecological histories.
机译:历史生态学是一个新兴的交叉学科领域,它试图通过综合人类记录和生物数据中的信息来解释生态系统随时间的变化。历史生态学中的方法涵盖了广泛的时空尺度。但是,近来(约200年)的方法在很大程度上限于人类档案和树木年代学证据,这些证据可能会受到人类的偏见,空间范围的限制或不适用于非森林系统。有必要探索新的方法,通过这些方法,可以使用生物学数据来了解最近的历史植被和干扰状况,特别是在干旱的生态系统类型中。土壤植物硅酸盐分析有可能提供有关这两个地区历史条件的急需信息。植硅石是通过二氧化硅在细胞壁内和细胞壁周围和周围沉积和积累而在植物中形成的结构,这些二氧化硅从植物中释放出来,并在植物材料死亡和腐烂很长时间后保存在沉积物中。爱达荷州南部的岩石市国家自然保护区是开发历史生态学新方法的绝佳场所,因为人类对历史环境条件的记录如此丰富。本论文研究有两个总体目标和相互联系的目标。首先是重建从陆路移民到现在的岩石城国家自然保护区的生态历史。第二个目标是通过测试土壤植石分析法记录已知变化的敏感性,探索土壤植石分析在推断近期植被和干扰状况变化中的实用性。我采用了现代模拟研究,多核方法和详细的核分析方法,通过分析提取重量,植物石料组合的相对丰度,细微的木炭和燃烧的(变暗的)植物石来测试已知变化。我的结果表明,将历史和土壤植物石质分析结合起来,将有助于推断生态历史中的植被变化(例如引入的草类增加)和干扰(例如火灾)。

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