Sedimentary Fe–Mn oxyhydroxides as paleoceanographic archives and the role of aeolian flux in regulating oceanic dissolved REE

Author:

Bayon Germain,German Christopher R.,Burton Kevin W.,Nesbitt Robert W.,Rogers Nick

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference59 articles.

1. Reduced North Atlantic Deep Water flux to the glacial Southern Ocean inferred from neodymium isotope ratios;Rutberg;Nature,2000

2. Sr and Nd isotope analyses in paleoceanography: the separation of both detrital and Fe–Mn fractions from marine sediments by sequential leaching;Bayon;Chem. Geol.,2002

3. North Atlantic Deep Water strength during the last deglaciation from Nd isotopes;Piotrowski;Geochim. Cosmochim. Acta,2002

4. S.L. Goldstein, S.R. Hemming, A.M. Piotrowski, R.L. Rutberg. Tracing glacial–interglacial thermohaline circulation with Nd isotopes: progress and precautions. Eos Trans. AGU 83, Fall Meet (2002). Abs. OS22E-06.

5. Radiogenic isotopes: tracers of past ocean circulation and erosional inputs;Frank;Rev. Geophys.,2002

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