Volume 12 Issue 4
Aug.  2016
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JIANG Yan′e, FANG Zhanqiang, LIN Zhaojin, ZHANG Peng, CHEN Zuozhi. Trace elements in statoliths of Sthenoteuthis oualaniensis in the South China Sea[J]. South China Fisheries Science, 2016, 12(4): 71-79. DOI: 10.3969/j.issn.2095-0780.2016.04.009
Citation: JIANG Yan′e, FANG Zhanqiang, LIN Zhaojin, ZHANG Peng, CHEN Zuozhi. Trace elements in statoliths of Sthenoteuthis oualaniensis in the South China Sea[J]. South China Fisheries Science, 2016, 12(4): 71-79. DOI: 10.3969/j.issn.2095-0780.2016.04.009
shu

Trace elements in statoliths of Sthenoteuthis oualaniensis in the South China Sea

  • 1.

    Key Lab. of South China Sea Fishery Resources Exploitation & Utilization, Ministry of Agriculture; Scientific Observing and Experimental Station of South China Sea Fishery Resources and Environment, Ministry of Agriculture; South China Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Guangzhou 510300, China

  • 2.

    Key Lab. of Ecology and Environmental Science in Guangdong Higher Education, College of Life Science, South China Normal University, Guangzhou 510631, China

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  • Received Date: March 16, 2016
  • Revised Date: April 28, 2016
    Graphical Abstract
    • Abstract

  • The trace elements of Sthenoteuthis oualaniensis collected from the South China Sea during September to October, 2012 were analyzed by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). The top 10 abundant elements are calcium (Ca), strontium (Sr), sodium (Na), phosphorus (P), potassium (K), magnesium (Mg), zinc (Zn), aluminum (Al), copper (Cu) and nickel (Ni). The analysis of variance (ANOVA) reveals significant difference in Ca (P=0.017), Sr (P=0.016) and Na (P=0.042) between middle-form (M-form) and dwarf-form (D-form) of S.oualaniensis (P < 0.05);significant difference of M-form existed in Ca (P=0.026), Sr (P=0.021) and Na(P=0.042) in sex (P < 0.05), but no significant difference of D-form existed in sex (P>0.05);significant difference of M-form existed in Cu (P=0.002), Ni (P=0.001) at different ages (P < 0.05), and significant difference of D-form existed in P (P=0.000), Mg (P=0.002), Zn (P=0.023), Al (P=0.000) and Cu (P=0.003) at different ages (P < 0.05). Sr in statolith declined as latitude decreased, and the concentration of 0 dah was higher than that of 10 dah.

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