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Benthic foraminifera abundance of Hole 41-366
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Abundance of living benthic foraminifera in sediment core CD86_10_BC4
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_09_BC1
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_08_BC5
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_07_BC4
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_06_BC5
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_05_BC5
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_04_BC4
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_03_BC4
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_02_BC5
This dataset has no description
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Abundance of living benthic foraminifera in sediment core CD86_01_BC1
This dataset has no description
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Abundance of dead benthic foraminifera in sediment core CD86_08_BC5
This dataset has no description
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Abundance of dead benthic foraminifera in sediment core CD86_07_BC4
This dataset has no description
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Abundance of dead benthic foraminifera in sediment core CD86_06_BC5
This dataset has no description
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Abundance of dead benthic foraminifera in sediment core CD86_05_BC5
This dataset has no description
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Abundance of dead benthic foraminifera in sediment core CD86_03_BC4
This dataset has no description
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Abundance of dead benthic foraminifera in sediment core CD86_02_BC5
This dataset has no description
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Abundance of dead benthic foraminifera in sediment core CD86_01_BC1
This dataset has no description
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Percentages of sand-sized material and biogenic components in sediment core G...
The paleo-oceanography of the southeastern North Atlantic Ocean during the last 150,000 yr has been studied using biogenous and terrigenous components of hemipelagic sediments... -
(Table AT1) Grain size distribution and stable isotope record of benthic fora...
The Walvis Paradox states that opal accumulation fluctuates in counterphase to general productivity on Walvis Ridge, off northern Namibia. Sediments of early Quaternary age from...