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Beginning with our work on ODP Leg 113, Site 690, Jim Pospichal has developed considerable evidence to demonstrate how Ir spikes above and below the boundary can be generated by secondary processes, including bioturbation. He has shown that large-bodied bioturbators can move sediment down section as much as one meterat deep-sea sites with paleodepths over 2000 m. By this msg I'll ask him to post a few of his key references for you. --Woody Wise
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