Dataset - B2FIND

Synthesis of early Pliocene and mid-Pliocene carbon anomaly

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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.

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

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(Table S1) Site locations, statistics of temporal coverage

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(Supplement S3) Volcanic ash layer description and thickness analysis from di...

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Correlations between the proxy SST anomalies (annual, boreal summer and borea...

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(Appendix 1) Nd and Mn concentration in planktonic foraminifera of sea surfac...

Planktonic foraminifera size fraction >250 µm.

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...

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...

(Table T3) Geochemical composition and age of ODP Site 181-1123 sediments

In 1998 Ocean Drilling Program Leg 181 off southwest New Zealand obtained cores from Site 1123 (41°47.2'S, 171°29.9'W; 3290 m water depth) on the Chatham Rise. Site 1123 sampled...

Appendix A Table SD1. CaCO3, δ¹⁸O, δ¹³C and Sr isotopes from ODP Site 181-1120

An integrated chemostratigraphic (87Sr/86Sr, d13C and 18O) study of benthic foraminifera is presented for a 210 m-thick, intermediate depth (upper/middle bathyal transition),...