Significant role of dissolved/particulate neodymium from the Ganga–Brahmaputra river system and Bay of Bengale margin in contributing to the dissolved Nd budget of the global oceans.

Data on dissolved Nd concentrations and isotopic compositions measured along a 87 E transect (GI01 section, “Indian GEOTRACES”) have been used in an inverse model in order to identify the respective effects of water mass mixing and Nd release from particulate matter in balancing this tracer budget in the Bay of Bengal. Results clearly underline that release from particulate phases supplied by the Ganga–Brahmaputra river system is required to explain both the distribution and budget of the Nd parameters. Calculations also evidence that supply of Nd from continental margin sediments is occurring at places identified at places identified as “hotspots of Nd release”.

sunil_figure_l

Click on the image to view it larger.

Reference:

Satinder Pal Singh, Sunil Kumar Singh, Vineet Goswami, Ravi Bhushan, Vinai Kumar Rai (2012), Spatial distribution of dissolved neodymium and εNd in the Bay of Bengal: Role of particulate matter and mixing of water masses: Geochimica et Cosmochimica Acta, ELSEVIER (94) p. 38-56, DOI : 10.1016/j.gca.2012.07.017.

Latest highlights

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.

Zinc and lead isotopes reveal human footprint on the most remote oceanic regions

Benaltabet and co-workers analysed suspended particles collected on GEOTRACES GP21 cruise tracked from Chile to New Caledonia.

Organic binding site heterogeneity controls amorphous ferric oxy-hydroxides oceanic sink

In oxygenated seawater iron binds to hydroxide ions, which results in authigenic Fe precipitation as amorphous ferric oxy-hydroxide…

Rechercher