4.7 Article

Effective use of cerium anomalies as a redox proxy in carbonate-dominated marine settings

Journal

CHEMICAL GEOLOGY
Volume 438, Issue -, Pages 146-162

Publisher

ELSEVIER
DOI: 10.1016/j.chemgeo.2016.06.027

Keywords

Rare earth elements; Ce anomalies; Acid leaching; Method development; Redox proxies; Fe-speciation; Carbonate geochemistry

Funding

  1. NERC's Life and the Planet project [NE/1005978/1]
  2. NERC [NE/I00596X/1, NE/I005935/1] Funding Source: UKRI
  3. Natural Environment Research Council [NE/I005935/1, 1220713, NE/I00596X/1] Funding Source: researchfish

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Rare earth elements and yttrium (REY) have a distinct distribution pattern in seawater, and this pattern may be faithfully preserved in carbonate sediments and rocks. Anomalous concentrations of redox-sensitive cerium (Ce) compared with neighbouring REY originate in oxic water column conditions, and as such, Ce anomalies can provide a potentially useful redox proxy in carbonate-dominated marine settings. The methods used to extract REY from carbonates vary widely, and may suffer from widespread leaching of REY from accessory non-carbonate minerals and organic matter, limiting the application of Ce anomalies for palaeo-redox reconstruction. We have systematically compared different methods on 195 carbonate samples with varying purity (% carbonate) from both modern and ancient environments. We used sequential leaching experiments in nitric add to identify the most 'seawater-like' portion of the carbonate sample where contributions from non-carbonate minerals and organic matter are minimised. We also compared the results of sample dissolution in different types and strengths of acid. Our results confirm that REY concentrations can be inadvertently contaminated by partial leaching of days and Fe (oxyhydr)oxides during a singlestep digestion, and we suggest a pre-leach of 20% of the sample, followed by a partial leach of 40% of the sample to selectively dissolve carbonate. We suggest that REY studies are optimised in carbonates with >85% CaCO3, and show that dolomites behave differently during the leaching process and must be treated separately. We present REY patterns for modern carbonate-rich sediments from a range of environments, and show that seawater REY are faithfully preserved in some non-skeletal carbonate, but modified leaching procedures are necessary for impure, unlithified or organic rich carbonate sediments. We combine REY with Fe-spedation data to identify how Fe oxides and clays contribute to the REY signal and explore how the two proxies can be used together to provide a complex and high-resolution redox reconstruction in carbonate-dominated marine environments. (C) 2016 The Authors. Published by Elsevier B.V.

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