Dataset - B2FIND

Mg/Ca and δ¹⁸O measurements of planktonic foraminifera from Sargasso Sea

Paired Mg/Ca and d18O measurements on planktonic foraminiferal species (G. ruber white, G. ruber pink, G. sacculifer, G. conglobatus, G. aequilateralis, O. universa, N....

Stable isotope record of planktonic foraminifera of sediment core TR163-19

Stable isotope data from eastern equatorial Pacific (EEP) core TR163-19 (2°15'N, 90°57'W, 2348 m) are presented for the surface-dwelling foraminifers Globigerinoides ruber and...

(Table 1) Foraminifera weight, size index and CO3 concentrations of core top ...

Down water column traverses of core top weights for three planktonic species confirm Lohmann's (1995) relationship between foraminifera shell weight loss and bottom water...

(Table 3) Mediterranean core-top δ¹⁸O values for various planktonic foraminif...

A box model is presented to simulate changes in Mediterranean long-term average salinity and d18O over the past 20,000 years. Simulations are validated by comparison with...

(Table 1) Radiocarbon ages of foraminifera from a Piston and a Trigger Weight...

Radiocarbon-age measurements on single species of foraminifera from a core on the Ceara Rise demonstrate the importance of the joint effect of bioturbation and variable rain...

Planktonic foraminiferal assemblages in sediment core KC01B

Planktonic foraminiferal assemblages were studied at high-resolution in core KC01B from the Ionian Sea. Quantitative analysis allowed us to distinguish the main climatic...

Stable isotope ratios on planktonic and benthic foraminifera in sediment core...

Sample at depth 2.1 m is from core catcher.

Stable isotopes and Mg/Ca ratios on foraminifera and Ba/Ca ratios of sediment...

The past variability of the South Asian Monsoon is mostly known from records of wind strength over the Arabian Sea while high-resolution paleorecords from regions of strong...

SST time-series for Eastern Arabian Sea recostructed from paired measurement ...

The deglacial transition from the last glacial maximum at ∼20 kiloyears before present (ka) to the Holocene (11.7 ka to Present) was interrupted by millennial-scale cold...