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(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,... -
Paleomagnetic chron boundaries of holes 302-M0002A and 302-M0004A
core depth as mcd -
Sedimentation rates for Expedition 302 holes
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Summary of lithologic units and occurrences by section, Holes 302-M0002A, M00...
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Calcareous microfossils index events of Holes 302-M0003A and 302-M0004C
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Silicoflagellates index events of Holes 302-M0002A and 302-M0004A
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Dinoflagellate cysts and organic microfossils index events of Holes 302-M0002...
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Pore water samples and chemistry from drill mud (filtered) of Expedition 302
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Pore water samples and chemistry from surface seawater of Expedition 302
Surface Seawater (n=5) -
List of tie points used to create the composite depth record for IODP-MSP Exp...
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Environmental corrected high resolution gamma-ray, pass2 of Hole 302-M0004B
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Environmental corrected high resolution gamma-ray, pass1 of Hole 302-M0004B
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Natural gamma-ray spectrometry-pass2 of Hole 302-M0004B
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Natural gamma-ray spectrometry-pass1 of Hole 302_M0004B
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Seismic velocity-pass2 of Hole 302-M0004B
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Seismic velocity-pass1 of Hole 302-M0004B
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Downhole logging caliper data-pass2 of Hole 302-M0004B
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Downhole logging caliper data-pass1 of Hole 302-M0004B
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Density of Hole 302-M0004C
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Density of Hole 302-M0004B
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