Variation in the isotopic composition of zinc in the natural environment and the use of zinc isotopes in biogeosciences: a review

被引:207
作者
Cloquet, Christophe [1 ,2 ]
Carignan, Jean [2 ]
Lehmann, Moritz F. [3 ]
Vanhaecke, Frank [1 ]
机构
[1] Univ Ghent, Dept Analyt Chem, B-9000 Ghent, Belgium
[2] Ctr Rech Petrog & Geochim, CNRS, F-54501 Vandoeuvre Les Nancy, France
[3] Univ Quebec, GEOTOP UQAM McGill, Montreal, PQ H3C 3P8, Canada
关键词
Zn isotopes; isotopic variation; biogeosciences; source tracer; fractionation mechanisms;
D O I
10.1007/s00216-007-1635-y
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
Zinc (Zn) is a trace element that is, as a building block in various enzymes, of vital importance for all living organisms. Zn concentrations are widely determined in dietary, biological and environmental studies. Recent papers report on the first efforts to use stable Zn isotopes in environmental studies, and initial results point to significant Zn isotope fractionation during various biological and chemical processes, and thus highlight their potential as valuable biogeochemical tracers. In this article, we discuss the state-of-the-art analytical methods for isotopic analysis of Zn and the procedures used to obtain accurate Zn isotope ratio results. We then review recent applications of Zn isotope measurements in environmental and life sciences, emphasizing the mechanisms and causes responsible for observed natural variation in the isotopic composition of Zn. We first discuss the Zn isotope variability in extraterrestrial and geological samples. We then focus on biological processes inducing Zn isotope fractionation in plants, animals and humans, and we assess the potential of Zn isotope ratio determination for elucidating sources of atmospheric particles and contamination. Finally, we discuss possible impediments and limitations of the application of Zn isotopes in (geo-) environmental studies and provide an outlook regarding future directions of Zn isotope research.
引用
收藏
页码:451 / 463
页数:13
相关论文
共 70 条
[21]   Use of isotope ratios to assess sources of Pb and Zn dispersed in the environment during mining and ore processing within the Orlovka-Spokoinoe mining site (Russia) [J].
Dolgopolova, A ;
Weiss, DJ ;
Seltmann, R ;
Kober, B ;
Mason, TFD ;
Coles, B ;
Stanley, CJ .
APPLIED GEOCHEMISTRY, 2006, 21 (04) :563-579
[22]   Magnesium isotope heterogeneity of the isotopic standard SRM980 and new reference materials for magnesium-isotope-ratio measurements [J].
Galy, A ;
Yoffe, O ;
Janney, PE ;
Williams, RW ;
Cloquet, C ;
Alard, O ;
Halicz, L ;
Wadhwa, M ;
Hutcheon, ID ;
Ramon, E ;
Carignan, J .
JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY, 2003, 18 (11) :1352-1356
[23]   Interaction between zinc and freshwater and marine diatom species:: Surface complexation and Zn isotope fractionation [J].
Gélabert, A ;
Pokrovsky, OS ;
Viers, J ;
Schott, J ;
Boudou, A ;
Feurtet-Mazel, A .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2006, 70 (04) :839-857
[24]  
Granger J., 2006, THESIS U BRIT COLUMB
[25]   Comparison of three different instrumental approaches to the determination of iron and zinc isotope ratios in clinical samples [J].
Ingle, CP ;
Langford, N ;
Harvey, LJ ;
Dainty, JR ;
Turner, PJ ;
Sharp, BL ;
Lewis, DJ .
JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY, 2004, 19 (03) :404-406
[26]  
John SG, 2005, GEOCHIM COSMOCHIM AC, V69, pA546
[27]  
JOHN SG, IN PRESS LIMNOL OCEA
[28]  
JOHN SG, CHEM GEOL
[29]   Overview and general concepts [J].
Johnson, CM ;
Beard, BL ;
Albarède, F .
GEOCHEMISTRY OF NON-TRADITIONAL STABLE ISOTOPES, 2004, 55 :1-24
[30]   A review of mass-dependent fractionation of selenium isotopes and implications for other heavy stable isotopes [J].
Johnson, TM .
CHEMICAL GEOLOGY, 2004, 204 (3-4) :201-214