ADVANCES IN POLAR SCIENCE ›› 2013, Vol. 25 ›› Issue (2): 105-112.DOI: 10.3724/SP.J.1084.2013.00105

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SPATIAL DISTRIBUTION OF GE IN THE SEDIMENTS OF PRYDZ BAY, SOUTHERN OCEAN

Shen Chen1,Hu Chuanyu1,2,Sun Weiping1,Zhang Haisheng1,2   

  1. 1Lab of Marine Ecosystem and Biogeochemistry, SOA,Second Institute of Oceanography, SOA, Hangzhou 310012, China; 2 China University of Geosciences, Wuhan 430074, China
  • Received:2012-10-15 Revised:2013-01-28 Online:2013-06-30 Published:2013-06-30

Abstract: The spatial distribution and concentration of Germanium (Ge) was investigated in sediments from the Southern Ocean (Prydz Bay). The content of Getotal in surface sediments ranged from 1.14×10-6—2.35×10-6, with a mean of 1.71×10-6. The highest Getotal content was found in P3-9 station, which was in the deeper open sea area out of the Prydz Bay. The lowest Getotal was recorded at the P4-13 station, which was near the edge of the Amery ice shelf. In the surface sediments, Gebio accounted for 16%—68% of Getotal.Spatially,Gebio and Getotal had similar distribution patterns, with higher values recorded outside, and lower contents in the south area of 67°S. The vertical distribution of Ge decreased with depth  in the core sediments. In the surface sediments outside of the Polynyas, there was a positive correlation between Gebio and biogenic silica(BSiO2). Specifically, the depth profiles of Gebio and BSiO2 were similar in the sediments from the P3-16 station.

Key words: Ge, sediment, Prydz Bay, Southern Ocean