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Title: Anthropogenic Signatures of Lead in the Northeast Atlantic [Anthropogenic signatures of lead in North West European margin]

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1002/2017GL076825· OSTI ID:1466150
ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [1]; ORCiD logo [3]; ORCiD logo [2]; ORCiD logo [2]; ORCiD logo [4]; ORCiD logo [5]; ORCiD logo [6]; ORCiD logo [7]; ORCiD logo [8]; ORCiD logo [9];  [2];  [10]
  1. University of Southampton (United Kingdom). Ocean and Earth Sciences, National Oceanography Centre; GEOMAR Helmholtz Centre for Ocean Research, Kiel (Germany)
  2. University of Plymouth (United Kingdom). School of Geography, Earth and Environmental Sciences
  3. Univ. of Edinburgh, Scotland (United Kingdom). School of Geosciences
  4. GEOMAR Helmholtz Centre for Ocean Research, Kiel (Germany)
  5. University of Southampton (United Kingdom). Ocean and Earth Sciences, National Oceanography Centre; University of Plymouth (United Kingdom). School of Geography, Earth and Environmental Sciences
  6. Université de Bretagne Occidentale, Brest (France)
  7. NIOZ Royal Netherlands Institute for Sea Research, Texel (Netherlands). Department of Ocean Systems
  8. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States). Nuclear and Chemical Sciences Division
  9. GEOMAR Helmholtz Centre for Ocean Research Kiel, (Germany)
  10. National Oceanography Centre Southampton (United Kingdom)

Anthropogenic activities have resulted in enhanced lead (Pb) emissions to the environment over the past century, mainly through the combustion of leaded gasoline. Here we present the first combined dissolved (DPb), labile (LpPb), and particulate (PPb) Pb data set from the Northeast Atlantic (Celtic Sea) since the phasing out of leaded gasoline in Europe. Concentrations of DPb in surface waters have decreased by fourfold over the last four decades. We demonstrate that anthropogenic Pb is transported from the Mediterranean Sea over long distances (>2,500 km). Benthic DPb fluxes exceeded the atmospheric Pb flux in the region, indicating the importance of sediments as a contemporary Pb source. A strong positive correlation between DPb, PPb, and LpPb indicates a dynamic equilibrium between the phases and the potential for particles to “buffer” the DPb pool. This study provides insights into Pb biogeochemical cycling and demonstrates the potential of Pb in constraining ocean circulation patterns.

Research Organization:
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE National Nuclear Security Administration (NNSA)
Grant/Contract Number:
AC52-07NA27344
OSTI ID:
1466150
Report Number(s):
LLNL-JRNL-756246; 943734
Journal Information:
Geophysical Research Letters, Vol. 45, Issue 6; ISSN 0094-8276
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 19 works
Citation information provided by
Web of Science

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  • Chen, Mengli; Boyle, Edward A.; Lee, Jong-Mi
  • Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, Vol. 374, Issue 2081 https://doi.org/10.1098/rsta.2016.0054
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Cited By (2)

Precessional Cyclicity of Seawater Pb Isotopes in the Late Miocene Mediterranean journal December 2019
Controls on redox-sensitive trace metals in the Mauritanian oxygen minimum zone journal January 2019

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