Dataset - B2FIND

Last Glacial Maximum seawater temperature estimates based on planktonic foram...

Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS...

Chemical composition of Pacific, Indian and Atlantic ocean manganese nodules ...

Manganese nodules, coatings and crusts from the Pacific and the Indian oceans were analyzed at Scripps Institution of Oceanography using X-ray emission spectrometry (XES)....

Downcore Florisphaera profunda

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SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...

Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES.

A summary of consistently dated Atlantic sediment cores over the last 40 thou...

Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear...

Metadata for a compilation of 127 benthic δ¹³C time series (20-6 ka)

Abbreviations for ocean and sea regionsINA: intermediate North Atlantic OceanUDNA: upper deep North Atlantic OceanLDNA: lower deep North Atlantic OceanISA: intermediate South...

Overview of literature values of foraminifera carbon stable isotopes in tropi...

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(Table 2) Termination depths and age estimations of various sediments cores

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Chemical composition of ocean manganese nodules from the Pacific Ocean using ...

From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other...

Chemical composition of ocean manganese nodules from the Pacific Ocean using ...

From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other...

(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...