Aluminium, manganese, iron, cobalt, and lead display contrasting fate along north–south and east–west sections in the North Pacific Ocean

Science Highlights

31 January 2024

Chan and co-authors report the distribution of the dissolved and labile particulate aluminium (Al), manganese (Mn), iron (Fe), cobalt (Co), and lead (Pb) in the subarctic Pacific Ocean during the GEOTRACES Japan KH-17-3 cruise and along the 47° N zonal transect (GEOTRACES GP02 Line). This provides a comprehensive view of dissolved and particulate trace metal distribution in the subarctic Pacific Ocean:

  • The trace metals behave differently along the north–south and east–west transects of the cruise. An intensive boundary scavenging occurs off the coast of Alaska -covering ca 250 km width-, limiting the impact of the continental sources (fluvial and sediment inputs) in this area.
  • At the easternmost station, the effect of the hydrothermal activity of the Juan de Fuca Ridge was detected.
  • Isopycnal transport of dMn and lpMn from the Okhotsk and Bering Seas to the western subarctic Pacific is also discussed.
  • Last but not least, this work proposes a temporal study of Pb distributions, which confirm that declining anthropogenic emissions of Pb resulted in a decadal change in dPb in the middle of the subarctic gyre.
Figure 1: Map of sampling stations during the R/V Hakuho Maru KH-17-3 cruise. Major ocean currents are indicated by orange arrows.
Figure 2: Distributions of a–e dM and f–i lpM on an isopycnal surface of 25.90 σθ.
The depth of this isopycnal surface is ~ 30 m in the west and ~ 120 m in the east generally below the surface mixed layer. Dissolved and particulate Al, Mn, Fe, and Co show isopycnal transport from the Okhotsk and Bering Seas to the western subarctic Pacific. In the Gulf of Alaska, boundary scavenging limits the spread of the continental supply of metals. Dissolved Pb has a distinct isopycnal distribution that reflects the anthropogenic aerosol supply from Asian countries and Russia.

Reference:

Chan, C.-Y., Zheng, L., & Sohrin, Y. (2024). The behaviour of aluminium, manganese, iron, cobalt, and lead in the subarctic Pacific Ocean: boundary scavenging and temporal changes. Journal of Oceanography. Access the paper: 10.1007/s10872-023-00710-8

Latest highlights

Mercury content and isotopes in bird’s guano: a window to reconstruct past climates

By analysing peat cores, Chuxian Li and her colleagues have shown how populations of nesting seabirds have fluctuated on a sub-Antarctic Island over the last 8,000 years.

Contraction of North Atlantic Deep Water during glacial times: a paradigm called into question

Blaser and co-authors propose a new distribution of deep-water masses in the Atlantic Ocean during the Last Glacial Maximum and the Heinrich Stadial..

Authigenic radiogenic neodymium isotope composition traces millennial-scale overturning circulation variability in the Arabian Sea

The neodymium isotopic signature of the sediment authigenic fraction is, a priori, a valuable proxy for reconstructing deep-water mass trajectories…

Magmatic activity at the Carlsberg Ridge in the Indian Ocean triggered by glacial sea-level variation

De and colleagues provide a high-resolution record of magmatic input and associated hydrothermal activity over the past 49 kyr from a core recovered from a magmatic segment of the slow-spreading Carlsberg Ridge in the Indian Ocean.

Rechercher