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dc.contributor.authorKelly, Amy E.
dc.contributor.authorReuer, Matthew K.
dc.contributor.authorGoodkin, Nathalie F.
dc.contributor.authorBoyle, Edward A.
dc.date.accessioned2011-05-25T14:50:14Z
dc.date.available2011-05-25T14:50:14Z
dc.date.issued2009-05
dc.date.submitted2009-03
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1721.1/63109
dc.description.abstractThe history of the oceanic anthropogenic lead (Pb) transient in the North Atlantic Ocean for the past 220 yr is documented here from measurements of Pb concentration and isotope ratios from annually-banded corals that grew in coastal seawaters near Bermuda and from seawater samples collected during the last 20 yr of the 20th century. Anthropogenic Pb emissions in this area have been dominated by the industrialization of North America beginning in the 1840s, the introduction of leaded gasoline beginning in the 1920s and its phase-out that began in the mid-1970s. The phase-out of leaded gasoline was largely completed by the late 1990s. Coral Pb concentrations occur at a constant low level of about 5 nmol Pb/mol Ca (~ 15 pmol/kg in seawater) from the late 1700s to ~ 1850. From ~ 1850 to ~ 1900 there is a small increase rising to a plateau at ~ 25 nmol Pb/mol Ca (~ 80 pmol/kg in seawater) in the 1930s until the late 1940s, at which point Pb concentrations rapidly increase to ~ 60 nmol Pb/mol Ca (~ 200 pmol/kg in seawater). In the mid 1970s, Pb began to decline to ~ 25 nmol Pb/Ca (40 pmol/kg in seawater) by the end of the 20th century, comparable to levels occurring in the early 20th century. Pb isotope ratios (Pb I.R.) show maximum 206Pb/207Pb = 1.21 and 208Pb/207Pb = 2.49 in the middle of the 19th century. We conclude that this signal is a reflection of the early dominance of Upper Mississippi Valley Pb ore in the United States, as previously seen in the estuarine sediments of Rhode Island. After 1900, Pb I.R. decrease only slightly until the 1960s when there is a significant local maximum in the 1970s to 206Pb/207Pb = 1.19 and 208Pb/207Pb = 2.45 as low-Pb I.R. sources were phased out in the United States. Then, as US leaded gasoline utilization decreased more rapidly than European Pb gas utilization (which has lower Pb I.R.), western North Atlantic Pb I.R. decreased to 206Pb/207Pb = 1.17 and 208Pb/207Pb = 2.44, their lowest values in the past two centuries.en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (NSF Grant OCE-0751409)en_US
dc.description.sponsorshipKuwait Foundation for the Advancement of Sciencesen_US
dc.description.sponsorshipMassachusetts Institute of Technologyen_US
dc.language.isoen_US
dc.publisherElsevier B.V.en_US
dc.relation.isversionofhttp://dx.doi.org/10.1016/j.epsl.2009.03.045en_US
dc.rightsCreative Commons Attribution-Noncommercial-Share Alike 3.0en_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/3.0/en_US
dc.sourceProf. Boyle via Anne Grahamen_US
dc.titleLead Concentrations and Isotopes in Corals and Water near Bermuda, 1780-2000 A.D.en_US
dc.typeArticleen_US
dc.identifier.citationKelly, Amy E. et al. “Lead Concentrations and Isotopes in Corals and Water Near Bermuda, 1780-2000.” Earth and Planetary Science Letters 283.1-4 (2009) : 93-100.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.approverBoyle, Edward A.
dc.contributor.mitauthorKelly, Amy E.
dc.contributor.mitauthorReuer, Matthew K.
dc.contributor.mitauthorGoodkin, Nathalie F.
dc.contributor.mitauthorBoyle, Edward A.
dc.relation.journalEarth and Planetary Science Lettersen_US
dc.eprint.versionAuthor's final manuscripten_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.orderedauthorsKelly, Amy E.; Reuer, Matthew K.; Goodkin, Nathalie F.; Boyle, Edward A.en
dc.identifier.orcidhttps://orcid.org/0000-0002-6394-1866
mit.licenseOPEN_ACCESS_POLICYen_US
mit.metadata.statusComplete


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