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 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

Stable carbon isotope ratios of alkane of IODP Hole 302-M0004A

The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme global warming approx ~55 million years ago, superimposed on an already warm world (Zachos et al.,...