Dataset - B2FIND

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...

(Table 2) Mean abundance of ebridian taxa in each ebridian assemblage group f...

Sediment depth is given in mbsf.A = Interval: from sample 302-M0004A-11X-4, 48-50cm (302.31mbsf) to 302-M0004A-9X-1, 14-16cm (287.44 mbsf).B = Interval: from sample...

(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 palynological analysis of Hole 302-M0004A

Abundance: A = abundant, P = poor, B = barren. Preservation: M = moderate. Depth = provisional. Numerical values are abundance in counts.

Results of palynological analysis of Hole 302-M0004B

A = abundance, B = barren, M = moderate. Numerical values are abundance in counts.

Results of palynological analysis of Hole 302-M0002A

Abundance: A = abundant, C = common, F = few, R = rare, B = barren. Preservation: M = moderate. Numerical values are abundance in counts.

Results of diatom analysis of Hole 302-M0004A

Abundance: A = abundant, C = common, R = rare, B = barren. Preservation: G = good, P = poor.

Results of diatom analysis of Hole 302-M0002A

Relative abundance: A = abundant, C = common, F = few, R = rare, B=barren (numerical values are abundance in counts) / + = ?

Nannofossil abundance of Hole 302-M0004C

Relative abundance: A = abundant, C = common, F = few, R = rare, B=barren (numerical values are abundance in counts) / cf. = conferatur, probably belongs to the identified species

Nannofossil abundance of Hole 302-M0002A

Relative abundance: A = abundant, C = common, F = few, R = rare, B=barren (numerical values are abundance in counts) / cf. = conferatur, probably belongs to the identified species