Evidence for the zircon origin of cadmium anomalies in bottom sediments from the littoral zone of the northern part of Lake Ladoga


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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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