Surprising conservativity of trace metals along a costal embayment salinity gradient

Chen and co-workers (2021, see reference below) analyzed an array of trace metals (manganese, iron, nickel, copper and zinc) together with Rare Earth Elements (REE) in a salinity gradient in the Jinhae Bay, the largest semi-enclosed bay in South Korea. Despite the occurrence of a significant scavenging activity revealed by the REE behaviors and intensive biological removal processes revealed by dissolved inorganic nutrients depletion, these trace elements showed higher concentrations in lower salinity waters and significant positive correlations with terrestrial humic substances. This thorough speciation study led the authors to hypothesize that when associated with terrestrial humic substances, these trace elements survive particle scavenging and biological consumption in the coastal mixing zone. This shuttling effect of terrestrial trace elements by humic substances in a coastal ocean is challenging the current paradigm assessing that trace elements are intensively removed in such salinity gradient.

Figure: The salinity plots for REE fractionation ((Nd/Er)PAAS) values and dissolved inorganic nitrogen (DIN) concentrations revealed significant particle scavenging of REE and biological removal of DIN in the inner Jinhae bay. However, trace elements (e.g. Mn and Zn) showed a good positive correlation with terrestrial humic substances (C peak), which behaved conservatively throughout the bay.

Reference:

Chen, X., Seo, H., Han, H., Seo, J., Kim, T., & Kim, G. (2021). Conservative behavior of terrestrial trace elements associated with humic substances in the coastal ocean. Geochimica et Cosmochimica Acta. https://doi.org/10.1016/J.GCA.2021.05.020

Latest highlights

23 million years of productivity reconstructed in the Central Pacific Ocean using past and modern proxies

Using diverse geochemical proxies, Chu and colleagues analysed an iron–manganese crust to reconstruct central Pacific productivity over the past 23 million years.

Lead isotopes reveal that hydrothermal variability is driven by Sea‐Level change and transient magmatism

De and colleagues present the first millennial-scale reconstruction of hydrothermal variability at a mid-ocean ridge using lead isotopes from iron-manganese coatings…

Long-range transport of iron via the Agulhas Current and counter-current: a boon for the phytoplankton

Authors establish that significant iron fertilisation via the Agulhas current explains the Indian Subantarctic blooms…

Hydrothermal activity detected above the ultra-slow South West Indian Ridge, using a multi-proxy approach

Baudet and colleagues demonstrate the occurrence of hydrothermal venting on the Southwest Indian Ridge…

Rechercher