Dataset - B2FIND

Benthic foraminiferal d13C and Cd/Ca studies suggest that deep Atlantic circulation during the Last Glacial Maximum was very different from today, with high-nutrient (low d13C,...

(Table 1) Stable oxygen isotope ratios of benthic foraminifera from Pacific O...

The thermal structure of the Pacific Ocean between water depths of about 1 and 4.5 kilometers is estimated from the oxygen isotopic ratio of benthonic foraminifera from...

(Table 1) Trace element concentrations and Sr isotope ratios of carbonates

Measurements of marine carbonate samples indicate that during the past 2.5 million years the 87Sr/86Sr ratio of seawater has increased by 14 * 10**-5. The high average rate of...

Composition of planktonic foraminifera species from 310 sediments samples dur...

Species list does not include G. menardii and G. tumida. These species were counted, but are not included in this analysis of the data.

(Table 1) Stable oxygen isotope ratios of Neogloboquadrina pachyderma sinistr...

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(Table 1) Carbonate content in surface sediments

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(Table 3) CaCO3 contents at the core top sediments below 4.2 km in the tropic...

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(Table 5) Age determination of sediment cores V19-27, V21-40 and V28-238

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(Table 2) Size of several planktic foraminifer species in surface sediments

An extended version of this table is availabel via the URL given as data detail

Calculated sea surface temperatures for the last glacial maximum

SST (1-12) is estimated mean annual Sea Surface Temperature in degrees C at the LGM depth. SST res is the difference between the LGM temperature estimate from this core, and the...

Sea surface temperature reconstructed from foraminifera in surface sediments ...

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196 datasets found