Prokaryotic communities display elevated trace metal concentrations in Pacific oxygen deficient zone

Local particulate maxima in many bioactive trace metals (cadmium, Cd; cobalt, Co; nickel, Ni; vanadium, V; and zinc, Zn) are found in the upper Oxygen Deficient Zone (ODZ), coincident with particulate phosporous (P) maxima that indicate biomass enrichments. This observation was made by Ohnemus and colleagues during the US GEOTRACES Eastern Pacific Zonal Transect (GP16) cruise which crossed the Pacific ODZ and oligotrophic gyre. Their data suggest elevated biotic accumulation of trace metals by ODZ organisms, by factors of 2 to 9 over surface mixed layer communities.

These observations raise many questions regarding the metal requirements and stoichiometric flexibilities of prokaryotes that dominate the ocean interior: Are particulate trace metal (pTM) associations unique to the ODZ? Do they occur because of access to generally larger inventories of dissolved TMs in the subsurface? Which metal enrichments are associated with which organisms? How do elevated–pTM associations in prokaryotic biomass relate to local and global cycling of pTMs throughout the oceans? There is no doubt that these new results open a wide field of research!

 

16 Ohnemus l
Figure: Metal:P biomass ratios in bulk particulate ODZ samples (black dots) compared to local mixed layer samples (red lines) demonstrate the elevated trace metal content of ODZ prokaryotic communities. All samples have been corrected for metals in lithogenic and scavenged iron-oxide phases. Click on the figure to view it larger.

Reference:

Ohnemus, D. C., Rauschenberg, S., Cutter, G. A., Fitzsimmons, J. N., Sherrell, R. M. and Twining, B. S. (2016), Elevated trace metal content of prokaryotic communities associated with marine oxygen deficient zones. Limnol. Oceanogr. doi:10.1002/lno.10363

Latest highlights

Continuous record of the Antarctic Circumpolar Current latitude over the last glacial-interglacial cycles

The meridional positions of the oceanic fronts separating subtropical and Antarctic waters are key to constraining the mechanisms that drive the degassing of deeply-stored CO2 at the end of the glacial periods…

23 Million Years of iron sources reconstructed in the Northwest Pacific Ocean using iron isotopes in a ferromanganese crust

Using iron isotopes and elemental records, Chu and co-workers analysed an iron-manganese crust recovered from the Hongyan Seamount, and reconstructed the sources of dissolved Fe to the Northwest Pacific Ocean…

Variability of the past deep-water masses in the Arabian Sea over the last 41ka

Shukla and colleagues propose a high-resolution authigenic ƐNd record measured from a sediment core located in the eastern Arabian Sea…

Arctic outflows to Davis Strait and the Labrador Sea traced by radionuclide distributions

This study demonstrates that Arctic outflows through the Canadian Arctic Archipelago play a much more significant role than previously recognised.

Rechercher