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Birch leaf compositions above different types of bedrock in glaciated areas

 

作者: Per-Olov Ehlin,  

 

期刊: Geologiska Föreningen i Stockholm Förhandlingar  (Taylor Available online 1985)
卷期: Volume 107, issue 3  

页码: 223-231

 

ISSN:0016-786X

 

年代: 1985

 

DOI:10.1080/11035898609453060

 

出版商: Taylor & Francis Group

 

关键词: Birch leaf composition;A0;A2;B2;C soils;chemical composition;rock influence;soil influence;wetland;metal contents;trace elements;minor elements;plasma spectrometry analysis;N 6530;N 6630;E 2030;E 2280

 

数据来源: Taylor

 

摘要:

Birch leaves (Betula alba), as well as A0, A2, B2and C soils can only rarely indicate the underlying rock type. Plants may show only anomalous concentrations of characteristic elements such as Ca above limestone and Cr or Ni above gabbro. If the plant compositions are used to distinguish types of basement rock, they could differentiate slightly between limestone and quartzite, limestone and granite, and porphyrite and granite, using their Ti, Al and Cu data, respectively. B2soil analyses could differentiate between limestone and silicate rocks in the basement, using Ca or Mg data. Plants have also a limited capacity to reflect the underlying soil, only Fe data are highly correlated with those of C and A0soil. Compositional correlations between plants and soil or rock are strongest in wetlands. 3 out of 5 such sites have anomalous contents of some metal in both birch and soil.

 

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