Unique winter dataset of particulate and dissolved cadmium in the Indian sector of the Southern Ocean

Science Highlights

6 September 2021

Cloete and collaborators (2021, see reference below) analysed particulate and dissolved cadmium (pCd and dCd respectively) at 7 stations in austral winter along a North South section between 41°S and 58°S, off South Africa. This heroic sampling effort and the subsequent analyses allowed these authors to establish that: 1) biological activity was still ongoing in winter although weaker than in summer; 2) biologically driven particulate Cd/P variations were observed along the section reflecting a stronger demand of Cd by diatoms in the Antarctic Zone compared to surface waters to the North; 3) the uptake of Cd is driven predominantly by the availability of dCd as well as a complex interplay involving dissolved iron (dFe), zinc (dZn) and manganese (dMn).

This last observation leads to distinct regional trends in Cd (vs phosphate, P) uptake and remineralization. The authors discuss the implications of the differential particulate Cd and P remineralization for the dCd to PO4 ratios in the upper water column. They also identify that in intermediate and deep waters, dCd distributions are largely the result of mixing between northward traveling waters of Antarctic origin (high dCd/dPO4 signatures) and southward traveling North Atlantic Deep Water (low dCd/dPO4 signature).

Figure: Particulate cadmium (pCd; black bars) and phosphorus (P; gray bars) normalized to profile maximum values (bottom axis) are plotted with absolute pCd:P ratios (red dots) to investigate potential differences in remineralization length scales. The plots show different trends in the pCd:P profiles, across the transect and with depth, reflecting variations in phytoplankton community structure, their Cd uptake characteristics and the relative remineralization length scales for pCd and P.

Reference:

Cloete R, Loock JC, van Horsten NR, Fietz S, Mtshali TN, Planquette H and Roychoudhury AN (2021) Winter Biogeochemical Cycling of Dissolved and Particulate Cadmium in the Indian Sector of the Southern Ocean (GEOTRACES GIpr07 Transect). Front. Mar. Sci. 8:656321. doi: 10.3389/fmars.2021.656321

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