Dataset - B2FIND

(Table A1) Stable isotope ratios and paleotemperature calculation of selected...

Paleotemperature estimates were calculated using the equation of Erez and Luz (1983), with seawater delta18O = -1.2 per mil PDB corresponding to a continental ice-free world...

(Table A1) Stable isotope ratios and paleotemperature calculation of selected...

Paleotemperature estimates were calculated using the equation of Erez and Luz (1983), with seawater delta18O = -1.2 per mil PDB corresponding to a continental ice-free world...

Stable oxygen and carbon isotope ratios for Early to Middle Cretaceous benthi...

Stable isotopic measurements have been made on planktonic and benthic foraminifera of Early to mid-Cretaceous (Early Albian-Cenomanian) age from DSDP site 463 located in the...

(Table 2) Paleolatitude and reconstructed temperatures for Cretaceous samples...

AGE [ka BP] is an estimated age. Absolute ages of samples are estimated from sedimentation rate curves for the Leg 207 sites (Erbacher et al., 2004) and have an estimated...

(Table 1) B/Ca ratios in planktonic foraminifera from core top sediments

This dataset has no description

(Table 2) In situ δ¹⁸O measurements in muricae of ODP Site 143-865

This dataset has no description

(Table 2) Temperature and depth of formation of cherts at DSDP Leg 62 Holes

Sediment depth is given in mbsf. Empty cells mean no data.

(Table 2) Stable isotopes at DSDP Site 87-583

This dataset has no description

(Table S2) Stable oxygen isotope ratios of Neogloboquadrina pachyderma and se...

Sediment depth is given in mcd. Age after Domack et al. (2001, doi:10.1191/095968301673881493)

(Appendix A) Temperature estimation for sediments of the Peru Margin

Stable oxygen isotope datas have been previously published by Meister et al. (2007) dataset: doi:10.1594/PANGAEA.763067 and by Thornburg and Suess (1990) dataset:...