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 <i>Journal of Geophysical Research: Solid Earth</i>. This material contains three tables of magnetic parameters (Table S1), hysteresis loop parameters (Table S2), and IRM acquisition results (Table S3).<br>