When covariance of trace metals and prokaryotic taxa are tagging water masses (Southern Indian Ocean)

Although recognised key for biogeochemical processes, the interplay between bioactive trace metals and marine microbes still remains largely unexplored. Zhang et al. (2024, see reference below) investigated the potential reciprocal links between diverse prokaryotic taxa (16S rRNA gene sequencing) and concentrations of dissolved iron (Fe), manganese (Mn), copper (Cu), and nickel (Ni) as well as apparent oxygen utilisation across 12 well-defined water masses in the Indian Sector of the Southern Ocean (SWINGS, GEOTRACES GS02 Section cruise). A refined statistical co-analysis (Partial Least Squares Regression) of the relative abundance of abundant microbial taxa and the distribution of trace metals revealed clear biogeochemical signatures of distinct water masses. These ‘biogeo’ gradients, that are a combination of the spatial distribution of microbial taxa and trace metals, provide a novel perspective, and opens insights on the potential interactions between abundant microbial taxa and trace metals in relation to organic matter remineralisation in the ocean.

Figure: Cross-section (see inserted map) showing the vertical distribution of some water masses sampled at the stations indicated on the upper x-axis during the SWINGS cruise (A). Localisation of samples used for Partial Least Squares Regression (PLSR) analyses on temperature-salinity diagrams (B, C, D). The colour coding corresponds to the first, second and third component of scores extracted from the PLSR, or microbial ‘biogeo’-gradients (BG).

Reference:

Zhang, R., Blain, S., Baudet, C., Planquette, H., Vivier, F., Catala, P., Crispi, O., Guéneuguès, A., Marie, B., Debeljak, P., & Obernosterer, I. (2024). Tagging of water masses with covariance of trace metals and prokaryotic taxa in the Southern Ocean. Limnology and Oceanography Letters, 9, 776–784. Access the paper: 10.1002/lol2.10429

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