Arid
DOI10.1007/s12633-015-9323-6
Spatial and Temporal Distribution Differences Among Phytoliths of Phragmites Communis in Northeast China
Liu, Lidan1,2,3; Jie, Dongmei1,2,3; Liu, Hongyan1,2,3; Lu, Meijiao1,2,3; Gao, Zhuo1,2,3; Gao, Guizai1,2,3; Li, Dehui1,2,3; Guo, Jixun3; Qiao, Zhihe4
通讯作者Jie, Dongmei
来源期刊SILICON
ISSN1876-990X
EISSN1876-9918
出版年2017
卷号9期号:4页码:593-602
英文摘要

Phragmites communis phytoliths were extracted from the xerophytic habitat of 12 sampling sites in northeast (NE) China during June-October in 2011 and 2012. The changes of P. communis phytolith concentrations in different temperature zones and growth stages were used to reveal the ecological environmental significance of P. communis phytoliths. The purpose of the study is to provide a scientific reference for quantitative reconstruction of paleoenvironment and studies of phytolith formation. The main phytolith types extracted from the 12 sampling sites and different growth stages were identical; however, the phytolith concentrations differed markedly. In NE China, from the temperate to the warm temperate zone, as temperature increased, the saddle phytoliths, bulliform phytoliths and the silicified stomata concentrations all increased, whereas the lanceolate phytolith concentration decreased. Moreover, in the humid, semi-humid and semi-arid areas, there were different responses of P. communis phytolith concentrations to temperature. Consequently, the spatial results showed that P. communis phytolith concentrations in NE China were closely related to temperature, which enabled inference of the change in temperature from phytolith concentration; however, they were also somewhat affected by humidity. During June-October, the temporal variation results of P. communis phytolith concentrations revealed that there were high lanceolate and bulliform phytolith concentrations in September or October; whereas the saddle phytolith concentration was high in July or August, and the maximum concentration for silicified stomata was in July. These findings may improve the understanding of phytolith formation, and provide useful information to further interpret phytolith assemblages in sediments.


英文关键词Temperature Humidity Growth period Phytolith Phragmites communis Northeast Chin
类型Article
语种英语
国家Peoples R China
收录类别SCI-E
WOS记录号WOS:000405509700015
WOS关键词SONGNEN GRASSLAND ; LEYMUS-CHINENSIS ; SIMULATION ; DEPOSITION ; VEGETATION ; CLIMATE ; CARBON
WOS类目Chemistry, Physical ; Materials Science, Multidisciplinary
WOS研究方向Chemistry ; Materials Science
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/202422
作者单位1.Northeast Normal Univ, Sch Geog Sci, Changchun 130024, Peoples R China;
2.State Environm Protect Key Lab Wetland Ecol & Veg, Changchun 130024, Peoples R China;
3.Minist Educ, Key Lab Vegetat Ecol, Changchun 130024, Peoples R China;
4.Daqing Normal Univ, Daqing 163712, Peoples R China
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GB/T 7714
Liu, Lidan,Jie, Dongmei,Liu, Hongyan,et al. Spatial and Temporal Distribution Differences Among Phytoliths of Phragmites Communis in Northeast China[J],2017,9(4):593-602.
APA Liu, Lidan.,Jie, Dongmei.,Liu, Hongyan.,Lu, Meijiao.,Gao, Zhuo.,...&Qiao, Zhihe.(2017).Spatial and Temporal Distribution Differences Among Phytoliths of Phragmites Communis in Northeast China.SILICON,9(4),593-602.
MLA Liu, Lidan,et al."Spatial and Temporal Distribution Differences Among Phytoliths of Phragmites Communis in Northeast China".SILICON 9.4(2017):593-602.
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