Datasets - B2FIND

The H2O is determined by air-drying the nodule samples at 200°C for two hours. The loss on ignition (LOI) is then measured after a one hour heating at 1100°C. In reducing the...

(Table XXX, pages 182-221) Chemical analyses of manganese nodules and crusts ...

The H2O is determined by air-drying the nodule samples at 200°C for two hours. The loss on ignition (LOI) is then measured after a one hour heating at 1100°C. In reducing the...

(Pages 133-183) Bottom photographs of manganese nodules fields and crusts obs...

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(Pages 128-131) Illustrations of samples of manganese nodules and crusts retr...

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Compilation of planktonic foraminiferal census data for Heinrich Stadial 1 fo...

Compilation of planktonic foraminiferal census data for Heinrich Stadial 1 of those five species modeled by PLAFOM, i.e., N. pachyderma, N. incompta, G. bulloides, G. ruber...

Chemical analyses of manganese nodules and crusts from the Pacific Ocean usin...

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(Table 3) Coretop foraminifer results

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(Table 1) Sample locations, salinity and sea surface temperatures (SST) annua...

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