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Response of phytoliths in Phragmites australis to environmental factors in northeast China

机译:东北芦苇中的植物石器对环境因子的响应

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Accuracy of paleovegetation reconstruction and understanding of phytolith formation would both be improved by further study of phytolith size in the Phragmites australis under different environmental conditions. Leaves of P. australis were collected from 11 sampling sites in northeast China with differences in temperature, precipitation and habitat. Principal component analysis of environmental factors (climatic and edaphic) indicated that the annual averages of temperature and precipitation were the main factors influencing phytolith size. Moreover, three-way analyses of variance (ANOVAs) further showed that phytolith size differed significantly under conditions of different temperature or precipitation gradients, whereas habitat differences had little effect. The changes in phytolith size with temperature differed in the humid, semi-humid and semi-arid areas of northeast China. In the humid and semi-humid areas, moving from the temperate to the warm temperate zone, increasing temperature reduced phytolith size; whereas in the semi-arid area, phytolith became larger with increasing temperature. In the warm temperate and temperate zones, the changes of phytolith size with precipitation showed the same trend moving from the semi-arid to semi-humid to humid areas, as precipitation increased, phytolith grew larger. Finally, ANOVA revealed that phytoliths were also sensitive to habitat. These findings demonstrated that the size of P. australis phytoliths was sensitive to environmental factors: for regional research, the annual averages of temperature and precipitation were the major factors influencing size, but in the same climate district, habitat differences seemed to also have a significant impact on phytolith size. Consequently, phytolith analysis has potential utility in the study of global climate change, palaeoenvironment reconstruction, and environmental conservation and restoration. (C) 2016 Elsevier B.V. All rights reserved.
机译:通过进一步研究芦苇在不同环境条件下的植物体大小,将提高古植被重建的准确性和对植物体形成的理解。从中国东北的11个采样点采集了澳大利亚的P. austtralis叶片,它们的温度,降水和生境都存在差异。对环境因素(气候和生态环境)的主成分分析表明,温度和降水的年平均水平是影响植硅体大小的主要因素。此外,三向方差分析(ANOVA)进一步表明,在不同温度或降水梯度的条件下,植硅石大小差异显着,而生境差异几乎没有影响。在东北的湿润,半湿润和半干旱地区,植硅体大小随温度的变化有所不同。在湿润和半湿润地区,从温带向温暖的温带区域移动,增加温度会降低植硅体的大小;而在半干旱地区,随着温度的升高,硅藻土变大。在温暖的温带和温带地区,随着降水量的增加,植硅体的大小随降水的变化呈现出从半干旱到半湿润再到湿润地区的相同趋势,随着降水的增加,植硅体的体积变大。最后,方差分析表明植硅石对生境也很敏感。这些发现表明,澳大利亚假单胞菌的石块大小对环境因素敏感:对于区域研究,温度和降水的年均平均值是影响大小的主要因素,但在同一气候区,栖息地差异似乎也有很大影响。对植石大小的影响。因此,硅藻土分析在全球气候变化,古环境重建以及环境保护和恢复研究中具有潜在的实用性。 (C)2016 Elsevier B.V.保留所有权利。

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