Dataset - B2FIND

Sea surface temperature anomalies for Pliocene interglacial KM5c (PlioVAR)

We examine a single interglacial during the late Pliocene (KM5c, ca. 3.205 +/- 0.01 Ma) when atmospheric CO2 concentrations were higher than pre-industrial, but similar to today...

δ18O and δ13C of Cibicidoides wuellerstorfi and related species and carbonate...

The δ13C composition of Cibicidoides wuellerstorfi and other Cibicidoides spp is an important tool to reconstruct past changes in the deep ocean carbon cycle. The species are...

Last interglacial and penultimate glacial sea surface temperature anomalies f...

Southern Ocean marine sediments provide an important archive of Quaternary glacial-interglacial climate changes. Sea surface temperature (SST) reconstructions in the Southern...

Carbon stable isotopes of Globigerina bulloides from 68 core tops in the sout...

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(Table S4c) Major and trace element compositions of ODP Hole 181-1123C tephras

All standard deviations = 2sd.

(Table S4b) Major and trace element compositions of ODP Hole 181-1123B tephras

All standard deviations = 2sd.

(Table S4a) Major and trace element compositions of ODP Hole 181-1123A tephras

All standard deviations = 2sd.

Maximum annual SST estimates during the early LIG (129-124 ka; 189 sites)

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.

Annual SST estimates for the Last Interglacial (129-116 ka BP)

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.