Dataset - B2FIND

(Table S1) Palynology of IODP Hole 302-M0004A

The Palaeocene/Eocene thermal maximum, 55 million years ago, was a brief period of widespread, extreme climatic warming (Zachos et al., 2003; Kennett and Stott, 1991,...

Results of foraminifer and ostracode analyses of Hole 302-M0004A

Abundance: A = abundant, F = few, C = common, R = rare, B = barren

Nitrogen isotope and biomarker composition of IODP Hole 302-M0004A

This dataset has no description

(Table 2b) Trace element analysis of sediments from IODP Exp302 sites

Sediment depth is given in revised meters composite depth [rmcd]. In the paper, various parts of Table 2b were transposed. The corrected table appears here (see also...

A compilation of published pyrite sulfur isotopic compositions from the past ...

This dataset contains a compilation of the sulfur isotopic composition of pyrite from outcrop and sediment cores over the past 165 million years. The compilation includes 3754...

Planktonic foraminifera and microfossil composition of IODP Hole 302-M0004C

Calcareous microfossils are widely used by paleoceanographers to investigate past sea-surface hydrology. Among these microfossils, planktonic foraminifera are probably the most...

(Table 1) Late Pleistocene planktonic foraminifera of Hole 302-M0004C

Planktonic foraminifera populations were studied throughout the top 25 meters of the IODP ACEX 302 Hole 4C from the central Arctic Ocean at a resolution varying from 5cm (at the...