Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution

During the 2014 GEOVIDE transect, seawater samples were collected for dissolved Pb and Pb isotope analysis. These samples provide a high-resolution snapshot of the source regions for the present Pb distribution in the North Atlantic Ocean. Some of these stations were previously occupied for Pb from...

Full description

Bibliographic Details
Main Authors: Wu, Jingfeng, Planquette, Hélène, Shelley, Rachel, Boutorh, Julia, Cheize, Marie, Contreira, Leonardo, Menzel Barraqueta, Jan-Lukas, Lacan, François, Sarthou, Géraldine, Zurbrick, Cheryl M, Boyle, Edward A, Kayser, Richard A, Reuer, Matthew K.
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Published: Copernicus GmbH/European Geosciences Union 2018
Online Access:http://hdl.handle.net/1721.1/118292
https://orcid.org/0000-0003-4964-757X
https://orcid.org/0000-0002-6394-1866
_version_ 1826208798038032384
author Wu, Jingfeng
Planquette, Hélène
Shelley, Rachel
Boutorh, Julia
Cheize, Marie
Contreira, Leonardo
Menzel Barraqueta, Jan-Lukas
Lacan, François
Sarthou, Géraldine
Zurbrick, Cheryl M
Boyle, Edward A
Kayser, Richard A
Reuer, Matthew K.
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
author_facet Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Wu, Jingfeng
Planquette, Hélène
Shelley, Rachel
Boutorh, Julia
Cheize, Marie
Contreira, Leonardo
Menzel Barraqueta, Jan-Lukas
Lacan, François
Sarthou, Géraldine
Zurbrick, Cheryl M
Boyle, Edward A
Kayser, Richard A
Reuer, Matthew K.
author_sort Wu, Jingfeng
collection MIT
description During the 2014 GEOVIDE transect, seawater samples were collected for dissolved Pb and Pb isotope analysis. These samples provide a high-resolution snapshot of the source regions for the present Pb distribution in the North Atlantic Ocean. Some of these stations were previously occupied for Pb from as early as 1981, and we compare the 2014 data with these older data, some of which are reported here for the first time. Lead concentrations were highest in subsurface Mediterranean Water (MW) near the coast of Portugal, which agrees well with other recent observations by the US GEOTRACES program (Noble et al., 2015). The recently formed Labrador Sea Water (LSW) between Greenland and Nova Scotia is much lower in Pb concentration than the older LSW found in the West European Basin due to decreases in Pb emissions into the atmosphere during the past 20 years. Comparison of North Atlantic data from 1989 to 2014 shows decreasing Pb concentrations consistent with decreased anthropogenic inputs, active scavenging, and advection/convection. Although the isotopic composition of northern North Atlantic seawater appears more homogenous compared to previous decades, a clear spatiotemporal trend in isotope ratios is evident over the past 15 years and implies that small changes to atmospheric Pb emissions continue. Emissions data indicate that the relative proportions of US and European Pb sources to the ocean have been relatively uniform during the past 2 decades, while aerosol data may suggest a greater relative proportion of natural mineral Pb. Using our measurements in conjunction with emissions inventories, we support the findings of previous atmospheric analyses that a significant portion of the Pb deposited to the ocean in 2014 was natural, although it is obscured by the much greater solubility of anthropogenic aerosols over natural ones.
first_indexed 2024-09-23T14:12:29Z
format Article
id mit-1721.1/118292
institution Massachusetts Institute of Technology
last_indexed 2024-09-23T14:12:29Z
publishDate 2018
publisher Copernicus GmbH/European Geosciences Union
record_format dspace
spelling mit-1721.1/1182922024-05-15T05:40:13Z Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution Wu, Jingfeng Planquette, Hélène Shelley, Rachel Boutorh, Julia Cheize, Marie Contreira, Leonardo Menzel Barraqueta, Jan-Lukas Lacan, François Sarthou, Géraldine Zurbrick, Cheryl M Boyle, Edward A Kayser, Richard A Reuer, Matthew K. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Zurbrick, Cheryl M Boyle, Edward A Kayser, Richard A Reuer, Matthew K During the 2014 GEOVIDE transect, seawater samples were collected for dissolved Pb and Pb isotope analysis. These samples provide a high-resolution snapshot of the source regions for the present Pb distribution in the North Atlantic Ocean. Some of these stations were previously occupied for Pb from as early as 1981, and we compare the 2014 data with these older data, some of which are reported here for the first time. Lead concentrations were highest in subsurface Mediterranean Water (MW) near the coast of Portugal, which agrees well with other recent observations by the US GEOTRACES program (Noble et al., 2015). The recently formed Labrador Sea Water (LSW) between Greenland and Nova Scotia is much lower in Pb concentration than the older LSW found in the West European Basin due to decreases in Pb emissions into the atmosphere during the past 20 years. Comparison of North Atlantic data from 1989 to 2014 shows decreasing Pb concentrations consistent with decreased anthropogenic inputs, active scavenging, and advection/convection. Although the isotopic composition of northern North Atlantic seawater appears more homogenous compared to previous decades, a clear spatiotemporal trend in isotope ratios is evident over the past 15 years and implies that small changes to atmospheric Pb emissions continue. Emissions data indicate that the relative proportions of US and European Pb sources to the ocean have been relatively uniform during the past 2 decades, while aerosol data may suggest a greater relative proportion of natural mineral Pb. Using our measurements in conjunction with emissions inventories, we support the findings of previous atmospheric analyses that a significant portion of the Pb deposited to the ocean in 2014 was natural, although it is obscured by the much greater solubility of anthropogenic aerosols over natural ones. 2018-10-01T13:36:29Z 2018-10-01T13:36:29Z 2018-08 2018-07 2018-09-20T17:24:08Z Article http://purl.org/eprint/type/JournalArticle 1726-4189 http://hdl.handle.net/1721.1/118292 Zurbrick, Cheryl M. et al. “Dissolved Pb and Pb Isotopes in the North Atlantic from the GEOVIDE Transect (GEOTRACES GA-01) and Their Decadal Evolution.” Biogeosciences 15, 16 (August 2018): 4995–5014 © 2018 Author(s) https://orcid.org/0000-0003-4964-757X https://orcid.org/0000-0002-6394-1866 http://dx.doi.org/10.5194/bg-15-4995-2018 Biogeosciences Creative Commons Attribution 4.0 International License http://creativecommons.org/licenses/by/4.0/ application/pdf Copernicus GmbH/European Geosciences Union European Geosciences Union
spellingShingle Wu, Jingfeng
Planquette, Hélène
Shelley, Rachel
Boutorh, Julia
Cheize, Marie
Contreira, Leonardo
Menzel Barraqueta, Jan-Lukas
Lacan, François
Sarthou, Géraldine
Zurbrick, Cheryl M
Boyle, Edward A
Kayser, Richard A
Reuer, Matthew K.
Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
title Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
title_full Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
title_fullStr Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
title_full_unstemmed Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
title_short Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
title_sort dissolved pb and pb isotopes in the north atlantic from the geovide transect geotraces ga 01 and their decadal evolution
url http://hdl.handle.net/1721.1/118292
https://orcid.org/0000-0003-4964-757X
https://orcid.org/0000-0002-6394-1866
work_keys_str_mv AT wujingfeng dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT planquettehelene dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT shelleyrachel dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT boutorhjulia dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT cheizemarie dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT contreiraleonardo dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT menzelbarraquetajanlukas dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT lacanfrancois dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT sarthougeraldine dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT zurbrickcherylm dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT boyleedwarda dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT kayserricharda dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution
AT reuermatthewk dissolvedpbandpbisotopesinthenorthatlanticfromthegeovidetransectgeotracesga01andtheirdecadalevolution