The Cd isotope composition of atmospheric aerosols from the Tropical Atlantic Ocean

Stable isotope compositions can potentially be used to trace atmospheric Cd inputs to the surface ocean and anthropogenic Cd emissions to the atmosphere. Both of these applications may provide valuable insights into the effects of anthropogenic activities on the cycling of Cd in the environment. How...

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Veröffentlicht in:Geophysical research letters 2017-03, Vol.44 (6), p.2932-2940
Hauptverfasser: Bridgestock, Luke, Rehkämper, Mark, Flierdt, Tina, Murphy, Katy, Khondoker, Roulin, Baker, Alex R., Chance, Rosie, Strekopytov, Stanislav, Humphreys‐Williams, Emma, Achterberg, Eric P.
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Sprache:eng
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Zusammenfassung:Stable isotope compositions can potentially be used to trace atmospheric Cd inputs to the surface ocean and anthropogenic Cd emissions to the atmosphere. Both of these applications may provide valuable insights into the effects of anthropogenic activities on the cycling of Cd in the environment. However, a lack of constraints for the Cd isotope compositions of atmospheric aerosols is currently hindering such studies. Here we present stable Cd isotope data for aerosols collected over the Tropical Atlantic Ocean. The samples feature variable proportions of mineral dust‐derived and anthropogenic Cd, yet exhibit similar isotope compositions, thus negating the distinction of these Cd sources by using isotopic signatures in this region. Isotopic variability between these two atmospheric Cd sources may be identified in other areas, and thus warrants further investigation. Regardless, these data provide important initial constraints on the isotope composition of atmospheric Cd inputs to the ocean. Key Points Novel Cd isotope composition data for aerosols are presented addressing an important gap in understanding of the global Cd cycle Similar Cd isotope compositions are observed for aerosols dominated by mineral dust‐derived and anthropogenic Cd These results provide useful constraints for studies concerning the marine biogeochemical Cd cycle
ISSN:0094-8276
1944-8007
DOI:10.1002/2017GL072748