Evidence for the zircon origin of cadmium anomalies in bottom sediments from the littoral zone of the northern part of Lake Ladoga
- Autores: Ivanter E.V.1, Slukovskii Z.I.2, Dudakova D.S.3, Medvedev A.S.2, Svetov S.A.2
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Afiliações:
- Petrozavodsk State University
- Institute of Geology, Karelian Research Centre
- Institute of Limnology
- Edição: Volume 468, Nº 2 (2016)
- Páginas: 607-610
- Seção: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/188520
- DOI: https://doi.org/10.1134/S1028334X16060118
- ID: 188520
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Resumo
The minor-element composition of bottom sediments from the littoral zone of the northern part of Lake Ladoga was studied. Close relationships between the anomalous Cd concentrations in lake sediments and Quaternary glacial formations on the territory of Karelia were shown. A negative correlation of Cd with other heavy metals and a positive correlation with Zr were observed. Most likely, Cd is an impurity in zircons from sandy and sandy loam sedimentary formations on the northern coastal area of Lake Ladoga.
Sobre autores
E. Ivanter
Petrozavodsk State University
Autor responsável pela correspondência
Email: slukovsky87@gmail.com
Rússia, Petrozavodsk
Z. Slukovskii
Institute of Geology, Karelian Research Centre
Email: slukovsky87@gmail.com
Rússia, Petrozavodsk
D. Dudakova
Institute of Limnology
Email: slukovsky87@gmail.com
Rússia, ul. Sevastiyanova 9, St. Petersburg, 196105
A. Medvedev
Institute of Geology, Karelian Research Centre
Email: slukovsky87@gmail.com
Rússia, Petrozavodsk
S. Svetov
Institute of Geology, Karelian Research Centre
Email: slukovsky87@gmail.com
Rússia, Petrozavodsk
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