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Neodymium isotope constraints from global carbonatites on the possible presence of a long-lived enriched mantle reservoir

Polák, Ladislav, Ackerman, Lukáš, Magna, Tomáš, Rapprich, Vladislav, Bizimis, Michael, Giebel, Robert Johannes, Dahlgren, Sven, Čejková, Bohuslava and Béguelin, Paul 2026. Neodymium isotope constraints from global carbonatites on the possible presence of a long-lived enriched mantle reservoir. Lithos: Journal of Petrology, Mineralogy and Geochemistry 538-53 , 108599. 10.1016/j.lithos.2026.108599

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Abstract

The occurrence of mantle-derived carbonatites in the geologic record since ∼3 billion years ago (Ga) allows to track the evolution of carbon-bearing mantle sources throughout much of the Earth's history. There appears to be continuing evidence for a significant proportion of subducted marine sedimentary material into the mantle sources of many carbonatites, attested by large ranges in εSr(i) from 7 to 73 and in εNd(i) from −10 to +0.5 which is different to conventional carbonatites originating from asthenospheric mantle with a limited contribution from enriched mantle sources; yet, neither sedimentary recycling via subduction nor common mantle metasomatism can explain highly unradiogenic and correlated initial 143Nd/144Nd ratios with εNd(i) values as low as −18.3, observed in many worldwide carbonatites with emplacement ages ranging from ∼2.0 Ga to 30 Ma. Here, we argue that these carbonatites require derivation from a long-lived mantle reservoir characterized by low-Sm/Nd (<0.17). These signatures can be best explained by admixture of an ancient, low-Sm/Nd slab-derived component that must have been incorporated into the mantle source parental to these low-143Nd/144Nd carbonatites at least 2.7 billion years ago.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Schools > Earth and Environmental Sciences
Additional Information: RRS policy applied
Publisher: Elsevier
ISSN: 0024-4937
Date of First Compliant Deposit: 9 June 2026
Date of Acceptance: 7 May 2026
Last Modified: 02 Aug 2026 07:45
URI: https://orca.cardiff.ac.uk/id/eprint/187062

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