A vivid picture of particle distribution and sources in the Arctic Ocean

Gardner and co-workers (2022, see reference below) proposed an extensive description of particle concentrations and chlorophyll-a fluorescence (Chl-a) distribution along GEOTRACES sections across the Arctic Ocean. The optical data in the sections were paired with particle composition on filtered samples through the whole water column. Particle distributions in the Arctic are affected by currents, stratification, ice coverage and thickness, nutrient and light availability, and biological processes. The combination of cp (a proxy for particular matter and particulate organic carbon) sections plotted with salinity, temperature, and Chl-a contours, adds a background and baseline across the entire Arctic Ocean that is useful in deciphering some of the particle dynamics of the Arctic.

Figure: Sections of cp (m-1, a proxy for PM or POC) from the Bering Strait to Norway. Contours: a) salinity; b) temperature, °C ; and c) Chl-a, µg l-1. Range of cp is 0-0.3 m-1 in 0-500m layer (horizontal bar) and 0-0.05 m-1 in 500-5000m layer (vertical bar) to enhance cp changes at depth. Blue lines at the top – ice cover: dashed – 20% to 80%, dark blue – >80%, light-blue – ice reported from R/V Polarstern. No line ~ ice-free. Orange line on map – stations included in these sections.

Reference:

Gardner, W. D., Richardson, M. J., Mishonov, A. V., Lam, P. J., & Xiang, Y. (2022). Distribution, Sources, and Dynamics of Particulate Matter Along Trans‐Arctic Sections. Journal of Geophysical Research: Oceans, 127(6). Access the paper: 10.1029/2021jc017970

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