Tambiev, Sergey B; Baturin, Gleb N (1982): (Table 1) Contents of P2O5, organic carbon, and REE in recent diatomaceous ooze and phosphorites from the Namibian shelf. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.778161, In supplement to: Tambiev, SB; Baturin, GN (1982): Rare earth elements in the process of ocean phosphorite formation. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 17(2), 3-15
Always quote above citation when using data! You can download the citation in several formats below.
Changes in concentration levels and speciation of heavy metals during sedimentation on example of a typical semi-closed bay, where bottom sediments have formed due to river run-off, are under consideration. It is shown that due to desorption of mobile manganese, zinc and copper entered the bay with river suspended matter, their total contents in bottom sediments decrease and percentages of lithogenic forms increase. Contents and speciation of iron in bottom sediments are determined by its participation in coagulation of river colloids in the mixing zone and by mechanical differentiation of sedimentary material.
Median Latitude: -22.400000 * Median Longitude: 14.108333 * South-bound Latitude: -22.666667 * West-bound Longitude: 13.966667 * North-bound Latitude: -22.133333 * East-bound Longitude: 14.250000
Minimum Elevation: -87.0 m * Maximum Elevation: -85.0 m
0 = not found.
206 data points