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Article: Lead concentrations and isotopes in corals and water near Bermuda, 1780-2000
Title | Lead concentrations and isotopes in corals and water near Bermuda, 1780-2000 | ||||||||||
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Authors | |||||||||||
Keywords | Global Anthropogenic Pollution Lead Lead Isotopes Pb Pb Isotopes | ||||||||||
Issue Date | 2009 | ||||||||||
Publisher | Elsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/epsl | ||||||||||
Citation | Earth And Planetary Science Letters, 2009, v. 283 n. 1-4, p. 93-100 How to Cite? | ||||||||||
Abstract | The 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. © 2009 Elsevier B.V. All rights reserved. | ||||||||||
Persistent Identifier | http://hdl.handle.net/10722/151282 | ||||||||||
ISSN | 2023 Impact Factor: 4.8 2023 SCImago Journal Rankings: 2.294 | ||||||||||
ISI Accession Number ID |
Funding Information: We thank E. Druffel and S. Griffin who generously provided the NR coral samples and chronology shown here, R. Smith and A. Cohen who provided the JSB coral samples, F. Duclas for sharing his Pb isotope database, and R. Kayser and B. Grant for laboratory assistance, and two anonymous reviewers for their constructive criticism. This research was supported by NSF Grant OCE-0751409 and partially supported by the Kuwait/MIT Center for Natural Resources and the Environment, a partnership between MIT and the Kuwait Foundation for the Advancement of Science (KFAS). | ||||||||||
References |
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Kelly, AE | en_US |
dc.contributor.author | Reuer, MK | en_US |
dc.contributor.author | Goodkin, NF | en_US |
dc.contributor.author | Boyle, EA | en_US |
dc.date.accessioned | 2012-06-26T06:20:01Z | - |
dc.date.available | 2012-06-26T06:20:01Z | - |
dc.date.issued | 2009 | en_US |
dc.identifier.citation | Earth And Planetary Science Letters, 2009, v. 283 n. 1-4, p. 93-100 | en_US |
dc.identifier.issn | 0012-821X | en_US |
dc.identifier.uri | http://hdl.handle.net/10722/151282 | - |
dc.description.abstract | The 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. © 2009 Elsevier B.V. All rights reserved. | en_US |
dc.language | eng | en_US |
dc.publisher | Elsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/epsl | en_US |
dc.relation.ispartof | Earth and Planetary Science Letters | en_US |
dc.rights | Earth and Planetary Science Letters. Copyright © Elsevier BV. | - |
dc.subject | Global Anthropogenic Pollution | en_US |
dc.subject | Lead | en_US |
dc.subject | Lead Isotopes | en_US |
dc.subject | Pb | en_US |
dc.subject | Pb Isotopes | en_US |
dc.title | Lead concentrations and isotopes in corals and water near Bermuda, 1780-2000 | en_US |
dc.type | Article | en_US |
dc.identifier.email | Goodkin, NF:goodkin@hkucc.hku.hk | en_US |
dc.identifier.authority | Goodkin, NF=rp00700 | en_US |
dc.description.nature | link_to_subscribed_fulltext | en_US |
dc.identifier.doi | 10.1016/j.epsl.2009.03.045 | en_US |
dc.identifier.scopus | eid_2-s2.0-65749118834 | en_US |
dc.identifier.hkuros | 155509 | - |
dc.relation.references | http://www.scopus.com/mlt/select.url?eid=2-s2.0-65749118834&selection=ref&src=s&origin=recordpage | en_US |
dc.identifier.volume | 283 | en_US |
dc.identifier.issue | 1-4 | en_US |
dc.identifier.spage | 93 | en_US |
dc.identifier.epage | 100 | en_US |
dc.identifier.isi | WOS:000267513700010 | - |
dc.publisher.place | Netherlands | en_US |
dc.identifier.scopusauthorid | Kelly, AE=7402153459 | en_US |
dc.identifier.scopusauthorid | Reuer, MK=7801554446 | en_US |
dc.identifier.scopusauthorid | Goodkin, NF=12446578100 | en_US |
dc.identifier.scopusauthorid | Boyle, EA=24368009800 | en_US |
dc.identifier.issnl | 0012-821X | - |