English
 
Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT

Released

Journal Article

Global continental and marine dfigetrital εNd: An updated compilation for use in understanding marine Nd cycling

Authors

Robinson,  Suzanne
External Organizations;

Ivanovic,  Ruza
External Organizations;

van de Flierdt,  Tina
External Organizations;

/persons/resource/blanchet

Blanchet,  Cécile L.
4.3 Climate Dynamics and Landscape Evolution, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Tachikawa,  Kazuyo
External Organizations;

Martin,  Ellen E.
External Organizations;

Cook,  Carys P.
External Organizations;

Williams,  Trevor
External Organizations;

Gregoire,  Lauren
External Organizations;

Plancherel,  Yves
External Organizations;

Jeandel,  Catherine
External Organizations;

Arsouze,  Thomas
External Organizations;

External Ressource
No external resources are shared
Fulltext (public)

5005609.pdf
(Publisher version), 15MB

Supplementary Material (public)
There is no public supplementary material available
Citation

Robinson, S., Ivanovic, R., van de Flierdt, T., Blanchet, C. L., Tachikawa, K., Martin, E. E., Cook, C. P., Williams, T., Gregoire, L., Plancherel, Y., Jeandel, C., Arsouze, T. (2021): Global continental and marine dfigetrital εNd: An updated compilation for use in understanding marine Nd cycling. - Chemical Geology, 567, 120119.
https://doi.org/10.1016/j.chemgeo.2021.120119


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5005609
Abstract
Understanding the role of sediment-water interactions in the oceanic cycling of neodymium (Nd) isotopes is essential for its reliable use as a modern and palaeoceanographic tracer of ocean circulation. However, the exact processes that control Nd cycling in the ocean are poorly defined and require an up-to-date knowledge of the sources, sinks and transformation of this tracer to and within the ocean (e.g. as per the GEOTRACES core mission). We propose a considerable improvement of Nd-source identification by providing an extensive and up-to-date compilation of published terrestrial and marine sedimentary Nd isotopic measurements. From this database, we construct high resolution, gridded, global maps that characterise the Nd-isotopic signature of the continental margins and seafloor sediment. Here, we present the database, interpolation methods, and final data products. Consistent with the previous studies that inform our compilation, our global results show unradiogenic detrital Nd isotopic values (εNd ≈ -20) in the North Atlantic, εNd values of ≈ -12 to -7 in the Indian and Southern Ocean, and radiogenic values (εNd ≈ -3 to +4) in the Pacific. The new, high-resolution interpolation is useful for improving conceptual knowledge of Nd sources and sinks and enables the application of isotope-enabled ocean models to understand targeted Nd behaviour in the oceans. Such applications may include: examining the strength and distribution of a possible benthic flux required to reconcile global Nd budgets, establishing the potential use of Nd isotopes as a kinematic tracer of ocean circulation, and a general quantification of the non-conservative sedimentary processes that may contribute to marine Nd cycling.