Magnetism results for "Paleoenvironmental significance of magnetofossils in pelagic sediments in the equatorial Pacific Ocean before and after the Eocene/Oligocene boundary".doc

The assemblage
patterns of magnetofossils may archive the change of paleoenvironment. A turning
point of the Cenozoic climate evolution has been proposed in the Eocene-Oligocene
transition (EOT). We study the magnetofossils from the sediment of eastern equatorial
Pacific Ocean during this period. The manuscript has been submitted to the Journal of Geophysical Research: Solid Earth.
This material contains three tables of magnetic parameters (Table S1), hysteresis
loop parameters (Table S2), and IRM acquisition results (Table
S3).