A benthic flux from calcareous sediments results in non-conservative neodymium behavior during lateral transport: A study from the Tasman Sea
Author:
Affiliation:
1. Department of Earth and Planetary Sciences, and Macquarie University Marine Research Centre, Macquarie University, Macquarie Park, New South Wales 2109, Australia
Publisher
Geological Society of America
Subject
Geology
Link
https://pubs.geoscienceworld.org/gsa/geology/article-pdf/47/4/363/4659261/363.pdf
Reference39 articles.
1. The sedimentary flux of dissolved rare earth elements to the ocean;Abbott;Geochimica et Cosmochimica Acta,2015
2. Bottoms up: Sedimentary control of the deep North Pacific Ocean’s εNd signature;Abbott;Geology,2015
3. The impact of sedimentary coatings on the diagenetic Nd flux;Abbott;Earth and Planetary Science Letters,2016
4. Reconstructing the Nd oceanic cycling using a coupled dynamical-biogeochemical model;Arsouze;Biogeosciences,2009
5. Neodymium isotopic characterization of Ross Sea Bottom Water and its advection through the Southern Pacific;Basak;Earth and Planetary Science Letters,2015
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3. Simulating marine neodymium isotope distributions using Nd v1.0 coupled to the ocean component of the FAMOUS–MOSES1 climate model: sensitivities to reversible scavenging efficiency and benthic source distributions;Geoscientific Model Development;2023-02-22
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