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(Figure 2a) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3209

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(Figure 2b) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3206

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(Figure 1g) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3174

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(Figure 1f) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3175BC

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(Table 4) Concentrations of chemical elements in tests of planktonic and benthic foraminifera from bottom sediments of the Ashadze-1 Hydrothermal Field

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(Figure 1h) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3171-4-6

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(Figure 1a) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3180

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(Figure 2d) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3245

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(Table 2b) Relative abundance of planktonic foraminiferas in samples of surface sediments and in sediments accumulated about 18 ky ago from typical cores in the area of the Benguela upwelling

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(Table 3) Vertical fluxes of sediment matter, carbon, nitrogen, and phosphorus at Station Vy20-3178

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(Table 1E) Distribution of Paleocene index and selected Cretaceous-Tertiary radiolarians in DSDP Hole 21-208 on the Lord Howe Rise off northwest New Zealand

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(Table 1) Contents of rock-forming and ore elements in air dried matter of bottom sediments from the Ashadze-1 Hydrothermal Field

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(Figure 2c) Distribution of planktonic foraminifera in bottom sediments of Core Vy20-3239

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(Table 2b) Species of planktonic foraminifera found in surface layer bottom sediment at Station Vy20-3217GR

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(Table 2) Relative contents of planktonic foraminifera in bottom sediments from the Ashadze-1 Hydrothermal Field

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