Chemical analyzes show that interstitial waters from ore-bearing bottom sediments of the Atlantis II and Discovery Deeps are enriched in Fe, Mn, Cu, Ni, Co, Zn, Pb, and Cd compared to sea water. Enrichment factors of these trace elements in the interstitial waters of the Atlantis II Deep relative to the sea water vary within the following ranges: for Fe from 100 to 7000, for Mn from 19047 to 32738, for Zn from 500 to 1600, for Pb from 78333 to 190000, for Cu from 107 to 654. Comparison of average weighted concentrations of Fe, Mn, Zn, Pb, Cu, Ni in the bottom sediments and the interstitial waters of the Atlantis II Deep indicates common regularities and good relationship in distribution of these elements along sediment cores. Differences in concentrations and distribution of the studied trace elements in the interstitial waters of the Atlantis II and Discovery Deeps result from different chemical compositions of hydrothermal fluids entering these deeps.

Supplement to: Pushkina, Zinaida V; Stepanets, M I; Orlova, L P; Sinani, T I (1981): Fe, Mn, Cu, Co, Ni, Zn, Pb, Cd, B, Si in interstitial waters of metalliferous sediments of the Red Sea (Atlantis II and Discovery Deeps). Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 16(6), 62-69