Controls of cadmium-phosphate systematic unraveled by Neural Networks and Ocean Circulation Inverse Model

Science Highlights

23 June 2021

Since cadmium (Cd) is correlated with phosphate (PO43-) in the modern ocean and seawater Cd concentration is recorded in micro-fossils, Cd can be used as a nutrient/circulation paleoceanographic tracer.  However, such paleo application is complicated because the processes responsible for this correlation are not fully understood. Roshan and DeVries (2021a, see references below) explore the similarities and contrasts between oceanic Cd and PO43- cycles using an Artificial Neural Network mapping technique and Ocean Circulation Inverse Model  (see figure).

A summary of their results:

  • The Cd:PO43- ratio in exported particles and its ratio to Cd:PO43- concentration ratio (known as “fractionation factor”) vary remarkably across regions, with an overall effect of depleting Cd relative to PO43- during the formation of water masses in the surface ocean.
  • High Cd:PO43- export ratio and fractionation factor correspond to low-iron regions.
  • The Cd:PO43- ratio during regeneration of the particles also varies vertically throughout the water column and horizontally across regions of different dissolved oxygen levels, with a global maximum at ~1,500 m.

By implementing a counterfactual scenario, Roshan and DeVries (2021a) find that widespread variability of the fractionation factor is the main destroyer of the Cd-PO43- correlation while the differential Cd:PO43- regeneration is a slight remediator. The produced dissolved Cd climatology is downloadable from Roshan and DeVries (2021b) and can benefit the calibration of seawater dissolved Cd concentration against core-top foraminiferal Cd/Ca ratio for paleoceanographic applications.   

Figure: Varying and greater-than-one Cd:PO43- fractionation factor in the surface ocean and depth-varying Cd:PO43- regeneration ratio in the subsurface ocean control Cd-PO43- relationship and Cd* (Cd *= Cd – 0.315 PO43-) distribution in the global ocean.

References:

Roshan, S., & DeVries, T. (2021a). Global Contrasts Between Oceanic Cycling of Cadmium and Phosphate. Global Biogeochemical Cycles, 35(6), e2021GB006952. DOI: https://doi.org/10.1029/2021GB006952

Roshan, Saeed; DeVries, Tim (2021b): Dissolved Cadmium Climatology. figshare. Dataset. https://doi.org/10.6084/m9.figshare.13536845.v1

Latest highlights

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…

To Ba or not to Ba: Evaluating water column excess particulate barium as a proxy for water column respiration

Rahman and co-workers examine the relationship between excess particulate barium and organic matter respiration in the water column…

Assessment of the Solomon Sea’s dissolved iron contribution to the Equatorial Under Current

Sarthou and co-workers analysed 11 vertical profiles of dissolved iron at the entrance, within, and at the exit of the Solomon Sea…

Major controls on the fate of dissolved manganese in the northeastern Indian Ocean

Malla and Singh investigated the key factors controlling dissolved manganese in the northeastern Indian Ocean.

Rechercher