文摘
Because the isotopic composition of anthropogenic Os isnormally distinctive in comparison to continental crustand is precisely measurable, this platinum-group elementis attractive as a tracer of transport pathways forcontaminated sediments in estuaries. Evidence herein andelsewhere suggest that biomedical research institutionsare the chief source of anthropogenic Os. In the ChesapeakeBay region, uncontaminated sediments bear a crustal 187Os/188Os signature of 0.73 ± 0.10. Slightly higher 187Os/188Osratios occur in Re-rich Coastal Plain deposits due to post-Miocene 187Re decay. The upper Susquehanna Basinyields sediments also with higher 187Os/188Os. Beginning inthe late 1970s, this signal was overprinted by a low 187Os/188Os (anthropogenic) source in the lower Susquehanna Basin.In the vicinity of Baltimore, which is a major center ofheavy industry as well as biomedical research, anthropogenicOs has been found only in sediments impacted by theprincipal wastewater treatment plant. Surprisingly, a mid-Bay site distant from anthropogenic sources containsthe strongest anthropogenic Os signal in the data set, havingreceived anthropogenic Os sporadically since the mid-20th Century. Transport of particles to this site overrodethe northward flowing bottom currents. Finding anthropogenicOs at this site cautions that other particle-borne substances,including hazardous ones, could be dispersed broadlyin this estuary.