Rare Earth Elements in the Bottom Sediments of the East Arctic Seas of Russia as Indicators of Terrigenous Input


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The REE distribution was studied in the bottom sediments of the East Arctic shelf of Russia. It is established that sediments of the Laptev and western East Siberian seas are significantly enriched in REEs, the contents of which are much higher than those of other near-continental basins. The main REE sources are runoff of the Lena River, the basin of which comprises ancient crystalline shields and magmatic rocks enriched in LREEs with significant contribution from the coastal erosion of the ice complex from the Laptev Sea and western East Siberian Sea. The terrigenous flux with a specific REE composition is supplied to the Chukchi Sea through the Bering Strait.

作者简介

A. Astakhov

Il’ichev Pacific Oceanological Institute, Far East Branch

编辑信件的主要联系方式.
Email: astakhov@poi.dvo.ru
俄罗斯联邦, Vladivostok, 690041

I. Semiletov

Il’ichev Pacific Oceanological Institute, Far East Branch

Email: astakhov@poi.dvo.ru
俄罗斯联邦, Vladivostok, 690041

V. Sattarova

Il’ichev Pacific Oceanological Institute, Far East Branch

Email: astakhov@poi.dvo.ru
俄罗斯联邦, Vladivostok, 690041

Xuefa Shi

First Institute of Oceanography

Email: astakhov@poi.dvo.ru
中国, Qingdao, 266061

Limin Hu

First Institute of Oceanography

Email: astakhov@poi.dvo.ru
中国, Qingdao, 266061

K. Aksentov

Il’ichev Pacific Oceanological Institute, Far East Branch

Email: astakhov@poi.dvo.ru
俄罗斯联邦, Vladivostok, 690041

Yu. Vasilenko

Il’ichev Pacific Oceanological Institute, Far East Branch

Email: astakhov@poi.dvo.ru
俄罗斯联邦, Vladivostok, 690041

M. Ivanov

Il’ichev Pacific Oceanological Institute, Far East Branch

Email: astakhov@poi.dvo.ru
俄罗斯联邦, Vladivostok, 690041

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