Sr and Nd Isotopes in Mineral Fractions of Ferromanganese Crusts from the Northernmost Pacific

• Published in: Journal of Marine Science and Engineering
• Main Authors: Pavel Mikhailik, Irina Vishnevskaya, Liang Yi, Natalia Soloshenko, Vadim Pellinen
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2023
• Subjects: ferromanganese crusts; mineral fractions; Sr and Nd isotopes; REE complexes; northernmost Pacific; Naval architecture. Shipbuilding. Marine engineering; VM1-989; Oceanography; GC1-1581; Anadyr; Anadyr'; Kamchatka; Kuskokwim; Yukon river; Yukon
• Online Access: https://doi.org/10.3390/jmse11101920; https://doaj.org/article/c225b4c50ddf486ba79353f1905ca535

A study of the isotopic compositions of neodymium and strontium in four mineral fractions of the hydrogenous ferromanganese crusts of the northernmost Pacific has been carried out for the first time. The relationship of the 87 Sr/ 86 Sr ratio and ε Nd value of the residual fraction in heterochronous layers of the ferromanganese crusts have shown that the sources of detrital matter are from rock weathering by the Yukon River, the Kuskokwim River, the Anadyr River and the rivers of Kamchatka. The amount of aluminosilicate impurity does not affect the isotopic compositions of the chemogenic (loosely bound, Mn oxides or manganese, hydrous Fe oxides or ferrous) fractions. The decreased ε Nd value in the ferrous fraction seems to be related to the presence of rare earth element (REE) phosphate complexes in seawater. The increase in those complexes is a consequence of melt waters entering the ocean during warming periods. Our data indicate that the carbonate REE complexes are not the dominant form of the REEs in the northernmost Pacific, which leads to the fact that the neodymium isotopic compositions of the manganese and ferrous fractions of hydrogenous ferromanganese crusts are different. A decrease in ε Nd value in the ferrous fraction may be a marker of a local increase in the surface water bioproductivity. Our data also show that the increase of the REE in the ferrous fraction relative to the manganese fraction does not reflect the participation of hydrothermal matter in the formation of mixed hydrogenous–hydrothermal crusts but is a consequence of an increase in the REE phosphate complexes.