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Inspired by ideas from the first Santa Fe conference two years ago, geomagnetists reconvened in Santa Fe last June to consider how findings in rock magnetism could increase understanding in the fields of global climate change and geodynamics. The conference, entitled Remagnetization and Environmental Rock Magnetism: Clues to Records of Past Geodynamic and Global Change, was sponsored by the Institute for Rock Magnetism (IRM) in Minneapolis and funded in part by the Earth Sciences Division of the National Science Foundation. Following lead talks that emphasized connections between geomagnetism and other geoscientific disciplines, more than 50 participants from the United States and Canada took part in an extended free-form discussion that resulted in a lively and fertile exchange of ideas.