Ferromanganese concretions spread out on the bottom of the shallow northwest part of the Black Sea are mainly represented by Fe and Mn nodules on shells and substituted worm tubes. Element composition of these formations was measured by methods of chemical, atomic absorbtion, neutron activation, and ICP-MS analyses. It was established that Fe and Mn contents and Mn/Fe ratio in the concretions varied considerably and which controlled occurrence of several associated metals and minor elements; some of them have not been studied in Black Sea concretions before.
Supplement to: Baturin, Gleb N (2010): Element composition of ferromanganese concretions in the Black Sea. Translated from Okeanologiya, 2010, 50(1), 89-98, Oceanology, 50(1), 83-92, doi:10.1134/S0001437010010108
