Dataset - B2FIND

(Table 1) Spores and pollen in upper Jurassic and lower Cretaceous sediments ...

This dataset has no description

(Table 5) Distribution of benthic foraminifers in the late Cretaceous of DSDP...

The book is devoted to stratigraphy of Cretaceous deposits from high latitudes of the southern hemisphere (subantarctic part of the ocean), as well as to geological and climatic...

(Table 1) Oxygen and carbon isotopic values for planktonic and benthic forami...

This dataset has no description

(Table 3) Oxygen and carbon isotopes from late Eocene and early Oligocene for...

Empty cells indicate missing data, because there was not enough material for analysis or material was lost during analysis.

(Table 2) Oxygen and carbon isotope data from middle Eocene foraminifers at D...

Empty cells indicate missing data, because there was not enough material for analysis or material was lost during analysis.

(Table 1) Trace and rare elements and CO2 at DSDP Hole 71-511

This dataset has no description

(Table 5) Geochemistry at DSDP Site 71-513

P2O5 was not measured.

(Table 1) Geochemistry at DSDP Hole 71-511

P2O5 was not measured.

(Figure 4) Distribution of benthic foraminifers in the Upper Cretaceous of DS...

X = present, - = absent.

(Figure 3) Distribution of benthic foraminifers in the Albian of DSDP Hole 71...

X = present, - = absent.

(Figure 2) Distribution of planktonic foraminifers in the Albian of DSDP Hole...

Species abundance: C = common, F = few, R = rare, VR = very rare, - = not observed. The Albian section is assumed to begin between Samples 71-511-49-5,102-104 and...

(Table 26) Contents of Li, Rb, Cs, and Be in Late Mesozoic deposits from DSDP...

Contents in air-dried matter.

(Figure 6) Distribution of benthic foraminifers in middle-upper and Quaternar...

X = present, - = absent.

(Data Set S1) Compiled benthic foraminiferal stable isotopic values

d13C_adj: carbon isotopic value adjusted to Cibicidoides equivalent.d18O_adj: oxygen isotopic value adjusted to Cibicidoides equivalent.