Dataset - B2FIND

Compiled Uk'37 data from PlioVAR

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Synthesis of early Pliocene and mid-Pliocene carbon anomaly

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Cenozoic TEX86-derived global SST compilation including new data from ODP/DSD...

Cenozoic global TEX86-derived sea surface temperature (SST) compilation from all published marine TEX86 records and new data measured in this study (ODP/DSDP Sites 516, 588,...

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.

Sea surface temperatures calculated from Mg/Ca ratio analysed on Globigerinoi...

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(Table 2) Stable carbon ond oxygen isotope ratios of planktonic foraminifera ...

Depth is composite depth (mcd)

Compilation of deglacial planktic d18O data from the North Pacific

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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 T1) Diatom stratigraphy of ODP Site 184-1143

Diatoms from Ocean Drilling Program Leg 184 Site 1143 in the southern South China Sea were analyzed for this paper. We found that diatoms are barren or scarce from 27.94 to...

(Table T2) Plankontic foraminifera stratigraphy of ODP Hole 184-1146A

DEPTH, sediment is given in mbsf. Abundance estimate as follows: P = <1% of the assemblage, R = 1%-5%, F = 5%-10%, A = 10%-30%, D = >30%, ? = Uncertain identification, - =...

(Table T1) Plankontic foraminifera stratigraphy of ODP Site 184-1143

DEPTH, sediment is given in mbsf. Abundance estimate as follows: P = <1% of the assemblage, R = 1%-5%, F = 5%-10%, A = 10%-30%, D = >30%, - = not found.