Concentrations of rare earth elements (REEs) were determined in three ornithogenic sediment profiles excavated at active Adelie penguin (Pygoscelis adeliae) colonies in McMurdo Sound, Ross Sea, Antarctica. The distribution of REEs in each profile fluctuated with depth. REEs measured in environmental media (including bedrock, guano, and algae) and analysis on the correlations of Sigma REE-lithological elements and Sigma REE-bio-elements in the profiles indicated that sedimentary REEs were mainly from weathered bedrock in this area, and the non-crustal biogenetic REEs from guano and algae were minor. Further discussion on the slopes and Ce and Eu anomalies of chondrite-normalized REE patterns indicated that a mixing process of weathered bedrock, guano and algae was the main controlling factor for the fluctuations of REEs with depth in the sediments. An end-member equation was developed to calculate the proportion of REEs from the three constituents in the sediments. The calculation functioned well in estimating bedrock-derived REEs and the magnitude of ornithogenic influence in different profiles. In general, REEs in the ornithogenic sediments showed anti bio-element patterns and thus can be used as an additional proxy to reconstruct historical penguin populations. (C) 2014 Elsevier B.V. All rights reserved.
机构:
Univ Tokyo, Ocean Res Inst, Marine Inorgan Chem Div, Nakano Ku, Tokyo 164, JapanUniv Tokyo, Ocean Res Inst, Marine Inorgan Chem Div, Nakano Ku, Tokyo 164, Japan
Alibo, DS
Nozaki, Y
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机构:
Univ Tokyo, Ocean Res Inst, Marine Inorgan Chem Div, Nakano Ku, Tokyo 164, JapanUniv Tokyo, Ocean Res Inst, Marine Inorgan Chem Div, Nakano Ku, Tokyo 164, Japan
机构:
Univ Tokyo, Ocean Res Inst, Marine Inorgan Chem Div, Nakano Ku, Tokyo 164, JapanUniv Tokyo, Ocean Res Inst, Marine Inorgan Chem Div, Nakano Ku, Tokyo 164, Japan
Alibo, DS
Nozaki, Y
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h-index: 0
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Univ Tokyo, Ocean Res Inst, Marine Inorgan Chem Div, Nakano Ku, Tokyo 164, JapanUniv Tokyo, Ocean Res Inst, Marine Inorgan Chem Div, Nakano Ku, Tokyo 164, Japan